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  <front>
    <journal-meta><journal-id journal-id-type="publisher">ANGEO</journal-id><journal-title-group>
    <journal-title>Annales Geophysicae</journal-title>
    <abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Ann. Geophys.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1432-0576</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/angeo-42-313-2024</article-id><title-group><article-title>Low-frequency solar radio type II bursts and their association with space weather events during the ascending phase of solar cycle 25</article-title><alt-title>Low-frequency solar radio type II bursts and space weather</alt-title>
      </title-group><?xmltex \runningtitle{Low-frequency solar radio type II bursts and space weather}?><?xmltex \runningauthor{T. Ndacyayisenga et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1 aff2">
          <name><surname>Ndacyayisenga</surname><given-names>Theogene</given-names></name>
          <email>ndacyatheogene@gmail.com</email>
        <ext-link>https://orcid.org/0000-0002-3836-1907</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Uwamahoro</surname><given-names>Jean</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Uwamahoro</surname><given-names>Jean Claude</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff4">
          <name><surname>Okoh</surname><given-names>Daniel Izuikedinachi</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff5">
          <name><surname>Sasikumar Raja</surname><given-names>Kantepalli</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-1192-1804</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Rabiu</surname><given-names>Akeem Babatunde</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-2734-5389</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Kwisanga</surname><given-names>Christian</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff6">
          <name><surname>Monstein</surname><given-names>Christian</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-3178-363X</ext-link></contrib>
        <aff id="aff1"><label>1</label><institution>College of Science and Technology, University of Rwanda, P.O. Box 3900, Kigali, Rwanda</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>United Nations African Regional Centre for Space Science and Technology Education – English (UN-ARCSSTE-E), Obafemi Awolowo University, Ile-Ife, Nigeria</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>College of Education, University of Rwanda, P.O. Box 55, Rwamagana, Rwanda</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>National Institute for Geophysics and Volcanology (INGV), 00143 Rome, Italy</institution>
        </aff>
        <aff id="aff5"><label>5</label><institution>Indian Institute of Astrophysics, II Block, Koramangala, Bengaluru 560 034, India</institution>
        </aff>
        <aff id="aff6"><label>6</label><institution>IRSOL, Istituto Ricerche Solari “Aldo e Cele Daccò”, Università della Svizzera italiana, Locarno, Switzerland</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Theogene Ndacyayisenga (ndacyatheogene@gmail.com)</corresp></author-notes><pub-date><day>8</day><month>July</month><year>2024</year></pub-date>
      
      <volume>42</volume>
      <issue>2</issue>
      <fpage>313</fpage><lpage>329</lpage>
      <history>
        <date date-type="received"><day>8</day><month>February</month><year>2023</year></date>
           <date date-type="rev-request"><day>16</day><month>February</month><year>2023</year></date>
           <date date-type="rev-recd"><day>13</day><month>May</month><year>2024</year></date>
           <date date-type="accepted"><day>23</day><month>May</month><year>2024</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2024 Theogene Ndacyayisenga et al.</copyright-statement>
        <copyright-year>2024</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://angeo.copernicus.org/articles/angeo-42-313-2024.html">This article is available from https://angeo.copernicus.org/articles/angeo-42-313-2024.html</self-uri><self-uri xlink:href="https://angeo.copernicus.org/articles/angeo-42-313-2024.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/angeo-42-313-2024.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d1e179">Type II solar radio bursts are signatures of the coronal shocks and, therefore, particle acceleration events in the solar atmosphere and interplanetary space. Type II bursts can serve as a proxy to provide early warnings of incoming solar storm disturbances, such as geomagnetic storms and radiation storms, which may further lead to ionospheric effects. In this article, we report the first observation of 32 type II bursts by measuring various plasma parameters that occurred between May 2021 and December 2022 in solar cycle 25. We further evaluated their accompanying space weather events in terms of ionospheric total electron content (TEC) enhancement using the rate of TEC index (ROTI). In this study, we find that at heliocentric distance <inline-formula><mml:math id="M1" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:mrow></mml:math></inline-formula>, the shock and the Alfvén speeds are in the range 504–1282 and 368–826 km<inline-formula><mml:math id="M3" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, respectively. The Alfvén Mach number is of the order of <inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.2</mml:mn><mml:mo>≤</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">1.8</mml:mn></mml:mrow></mml:math></inline-formula> at the above-mentioned heliocentric distance. In addition, the measured magnetic field strength is consistent with the earlier reports and follows a single power law <inline-formula><mml:math id="M5" display="inline"><mml:mrow><mml:mi>B</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">6.07</mml:mn><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3.96</mml:mn></mml:mrow></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula>. Based on the current analysis, it is found that 19 out of 32 type II bursts are associated with immediate space weather events in terms of radio blackouts and polar cap absorption events, making them strong indications of space weather disruption. The ROTI enhancements, which indicate ionospheric irregularities, strongly correlate with GOES X-ray flares, which are associated with the type II radio bursts recorded. The diurnal variability in ROTI is proportional to the strength of the associated flare class, and the corresponding longitudinal variation is attributed to the difference in longitude. This article demonstrates that since type II bursts are connected to space weather hazards, understanding various physical parameters of type II bursts helps to predict and forecast the space weather.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <?pagebreak page315?><p id="d1e274">The interaction of coronal mass ejections (CMEs) and their shocks with the magnetosphere is the major cause of the strongest space weather events in the magnetosphere. Shocks can be observed at extreme ultraviolet, visible and radio wavelengths <xref ref-type="bibr" rid="bib1.bibx57 bib1.bibx13" id="paren.1"/>. CMEs trigger space weather hazards by compressing the Earth's magnetosphere upon their arrival at the Earth, which results in channelling the particles into the Earth's atmosphere to produce auroras. CMEs are also responsible for geomagnetic storms, power grid disruptions, accelerating solar energetic particles (SEPs) events, etc. The energy released by explosive flares produces disruptions in the Earth's atmosphere within 8 min of the initial emission time <xref ref-type="bibr" rid="bib1.bibx81 bib1.bibx104" id="paren.2"/>. Solar flare radiations interact with ionosphere constituents, causing an immediate rise in total electron density of the ionosphere. The extent of the ionospheric total electron content (TEC) enhancements appears to be determined by the category of solar flares <xref ref-type="bibr" rid="bib1.bibx53 bib1.bibx54 bib1.bibx45 bib1.bibx3" id="paren.3"/>. During the peak of X-ray solar flares, ionospheric TEC abnormalities are frequently suppressed due to accelerated solar energetic particles <xref ref-type="bibr" rid="bib1.bibx70" id="paren.4"/>. The rate at which TEC varies temporally is related to the effective flare radiation flux <xref ref-type="bibr" rid="bib1.bibx107" id="paren.5"/>. Enhanced TEC in the ionospheric D layer causes the absorption and blocking of high-frequency radio signals, resulting in significant radio blackouts (R3) <xref ref-type="bibr" rid="bib1.bibx3" id="paren.6"/>. Radio blackouts are disruptions in wireless communication and global positioning satellite (GPS) systems that use radio waves to communicate through the ionosphere. The National Oceanic and Atmospheric Administration (NOAA) classifies radio blackouts into five levels, which occur when radio signals carried through the ionosphere are reduced or absorbed <xref ref-type="bibr" rid="bib1.bibx45" id="paren.7"/>. In addition to global navigation satellite system (GNSS) signals, ionospheric disturbances have a significant impact on high-frequency communications. <xref ref-type="bibr" rid="bib1.bibx74" id="text.8"/> developed an index known as the rate of change in TEC (ROT) that is based on the time rate of various phase changes in dual-frequency GNSS signals crossing the same ionospheric parcel and is expressed in TECU min<inline-formula><mml:math id="M6" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (1 TECU <inline-formula><mml:math id="M7" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">16</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> electrons m<inline-formula><mml:math id="M8" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>). Depending on the dual-frequency GPS signals, ROT explains the irregularities on various length scales. The standard deviation of the ROT is used to construct the rate of TEC index (ROTI), which has the same unit as ROT <xref ref-type="bibr" rid="bib1.bibx74 bib1.bibx14 bib1.bibx56" id="paren.9"><named-content content-type="pre">e.g.</named-content></xref>. ROTI describes the small-scale irregularity of the line-of-sight electron content resulting from the ionosphere <xref ref-type="bibr" rid="bib1.bibx74 bib1.bibx56" id="paren.10"/>. During the solar minimum, the corotating interaction regions (CIRs) are the principal source of energetic particles in the heliosphere <xref ref-type="bibr" rid="bib1.bibx60 bib1.bibx100 bib1.bibx79" id="paren.11"><named-content content-type="pre">e.g.</named-content></xref>. CIRs develop when a stream of rapid solar wind emerges from a coronal hole that reaches to low latitudes and overtakes a parcel of slow solar wind generated by the Sun at earlier times. The solar rotation causes these plasmas of different speeds to become radially aligned and interact <xref ref-type="bibr" rid="bib1.bibx31" id="paren.12"><named-content content-type="pre">e.g.</named-content></xref>. This interaction generates a compression area that revolves with the Sun and can amplify to produce shocks that accelerate particles. The radio emissions that occur in the solar atmosphere to interplanetary space arise from a broad range of physical phenomena with space weather implications <xref ref-type="bibr" rid="bib1.bibx24 bib1.bibx67 bib1.bibx104" id="paren.13"><named-content content-type="pre">e.g. flares, solar energetic particles, CMEs and shocks,</named-content></xref>. Solar radio bursts (SRBs) originate from different altitudes in the solar atmosphere, and they are observed over a wide range of wavelengths from millimetres to decametres. Plasma density, electron beam density, injected electron beam speed, local turbulence levels, etc., all have a significant impact on the generation of various solar radio bursts <xref ref-type="bibr" rid="bib1.bibx86" id="paren.14"/>. Furthermore, electron density, magnetic field and turbulence levels change with the solar cycle phase <xref ref-type="bibr" rid="bib1.bibx84 bib1.bibx85 bib1.bibx64" id="paren.15"/>. Moreover, it is obvious that the phase of solar activity affects the multiple coronal features outlined above, which in turn influences the formation of SRBs. <xref ref-type="bibr" rid="bib1.bibx109" id="text.16"/> classified SRBs into five types according to their  morphologies of their dynamic spectra and their origin. Of the five types, type II, III and IV bursts are relevant to space weather study because they are associated  with space weather drivers, such as shock waves <xref ref-type="bibr" rid="bib1.bibx10 bib1.bibx11 bib1.bibx15" id="paren.17"><named-content content-type="pre">type II bursts;</named-content></xref>, streams of electrons propagating along open magnetic field lines <xref ref-type="bibr" rid="bib1.bibx78" id="paren.18"><named-content content-type="pre">type III bursts;</named-content><named-content content-type="post">for a review</named-content></xref> and CMEs or post-flare loops <xref ref-type="bibr" rid="bib1.bibx68 bib1.bibx48" id="paren.19"><named-content content-type="pre">type IV bursts;</named-content></xref>. In the present paper, metric type II radio bursts observed from the ground by extended Compound Astronomical Low frequency Low cost Instrument for Spectroscopy and Transportable Observatory (herein <inline-formula><mml:math id="M9" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO) <xref ref-type="bibr" rid="bib1.bibx6 bib1.bibx7" id="paren.20"/> are studied. First discovered by <xref ref-type="bibr" rid="bib1.bibx72" id="text.21"/>, type II radio bursts are among the most powerful events in the solar radio emission observed at metric wavelengths <xref ref-type="bibr" rid="bib1.bibx108" id="paren.22"><named-content content-type="pre">e.g.</named-content></xref>. At present, it is generally accepted that type II radio emissions are excited by magnetohydrodynamic (MHD) shock waves driven by solar flares, CMEs and fast plasma flow in the magnetic reconnection regions  <xref ref-type="bibr" rid="bib1.bibx58 bib1.bibx75 bib1.bibx96 bib1.bibx32 bib1.bibx101 bib1.bibx46 bib1.bibx30 bib1.bibx110 bib1.bibx15 bib1.bibx44" id="paren.23"/>. Physical properties of metric type II radio bursts, including but not limited to drift rate, starting frequency and duration, are used to study the dynamics of the middle and upper solar corona. For example, the Alfvén Mach number, <inline-formula><mml:math id="M10" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">S</mml:mi></mml:msub><mml:mo>/</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">S</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M12" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are shock and Alfvén speeds, respectively), is calculated using three different methods: (i) from shock geometry in extreme ultraviolet (EUV) images, (ii) from the ratio of the CME speed to the  Alfvén speed and (iii) using shock parameters derived from type II radio-band-splitting phenomena <xref ref-type="bibr" rid="bib1.bibx106 bib1.bibx57 bib1.bibx44" id="paren.24"/>. A recent study by <xref ref-type="bibr" rid="bib1.bibx57" id="text.25"/> showed that these three methods give consistent results after their comparative analysis. By analysing one or two events, many authors <xref ref-type="bibr" rid="bib1.bibx17 bib1.bibx18 bib1.bibx46 bib1.bibx57 bib1.bibx49 bib1.bibx43 bib1.bibx59" id="paren.26"><named-content content-type="pre">e.g.</named-content></xref> have determined the magnetic field strengths and examined the spatial and temporal evolution of shock properties, as well as the conditions responsible for type II radio emissions during the high solar activity of solar cycle 24. There have been few works completed during the rise and fall phases of solar cycle 24 <xref ref-type="bibr" rid="bib1.bibx26 bib1.bibx102" id="paren.27"><named-content content-type="pre">e.g.</named-content></xref>. <xref ref-type="bibr" rid="bib1.bibx40" id="text.28"/>, on the other hand, covered the entire solar cycle 23. In the current study, a number of events are analysed during the ascending phase of solar cycle 25 which started in December 2019 <xref ref-type="bibr" rid="bib1.bibx37 bib1.bibx2 bib1.bibx8" id="paren.29"/>. In this article, we apply the Rankine–Hugoniot density jump relation and parameters of type II radio bursts to estimate the parameter of shock waves (shock and the Alfvén speed and the Alfvén Mach number) of metric type II radio bursts observed by <inline-formula><mml:math id="M13" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO and then analyse their space weather implication in terms of the ionospheric TEC enhancements using ROTI variability on daily basis.</p>
</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Observation</title>
<sec id="Ch1.S2.SS1">
  <label>2.1</label><title>Type II radio burst observation</title>
      <p id="d1e505">The radio data presented in the current work were observed by <inline-formula><mml:math id="M14" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO from May 2021 to December 2022 in solar cycle 25. First, we selected a number of radio events from the observations made by the instrument (<uri>https://e-callisto.org</uri>, last access: 19 February 2024) and selected 32 well-separated type II radio bursts whose morphologies are clear. We then examined their association with the current solar phenomena to give insights into the status of the ascending phase of the solar cycle 25. In order to investigate the implications of space weather in terms of TEC, each selected type II radio burst was associated with a coronal mass ejection (CME) and an onset of a solar flare. The flare records were checked from the solar monitor (<uri>https://solarmonitor.org/</uri>, last access: 19 February 2024). The CME parameters were taken from the Large Angle and Spectrometric COronagraph (LASCO C2) on board the Solar and Heliospheric Observatory  <xref ref-type="bibr" rid="bib1.bibx9" id="paren.30"><named-content content-type="pre">SOHO;</named-content></xref> catalogue updated to 30 December 2022.</p>
</sec>
<sec id="Ch1.S2.SS2">
  <label>2.2</label><title>Derivation of shock characteristic parameters</title>
      <p id="d1e534">In this study, first we measured the bandwidth (BDW) of each type II radio burst. Because all of the type II bursts do not show a band-splitting feature, the BDW of the fundamental band is linked to the ambient density jump to ensure consistency in computation.
            <disp-formula id="Ch1.E1" content-type="numbered"><label>1</label><mml:math id="M15" display="block"><mml:mrow><mml:mi mathvariant="normal">BDW</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">u</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">u</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M17" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> denote the upper and lower frequencies, respectively, of the fundamental emission band. Figure <xref ref-type="fig" rid="Ch1.F1"/> shows an example of type II radio burst from 03:28:25 to 03:32:30 UT on 17 April 2022 for which <inline-formula><mml:math id="M18" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">u</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M19" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are indicated. This burst is associated with an X1.1 flare that started at 03:17 UT and stopped at 03:51 UT in NOAA active region 12994.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><?xmltex \currentcnt{1}?><?xmltex \def\figurename{Figure}?><label>Figure 1</label><caption><p id="d1e619">Type II radio burst from 03:28:25 to 03:32:30 UT observed by the South Korean Astronomy and Space science Institute (KASI) on 17 April 2022. <inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mi mathvariant="normal">u</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> denote the upper and lower frequencies of the fundamental band of the type II radio emission.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f01.png"/>

        </fig>

      <?pagebreak page316?><p id="d1e650">The values of BDW were used to estimate the density jump across the shock <xref ref-type="bibr" rid="bib1.bibx105 bib1.bibx106 bib1.bibx16 bib1.bibx65" id="paren.31"/> <inline-formula><mml:math id="M22" display="inline"><mml:mi mathvariant="italic">χ</mml:mi></mml:math></inline-formula> via the relation
            <disp-formula id="Ch1.E2" content-type="numbered"><label>2</label><mml:math id="M23" display="block"><mml:mrow><mml:mi mathvariant="italic">χ</mml:mi><mml:mo>=</mml:mo><mml:mo>(</mml:mo><mml:mi mathvariant="normal">BDW</mml:mi><mml:mo>+</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:msup><mml:mo>)</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula>
          By assuming low plasma ratio (<inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:mi mathvariant="italic">β</mml:mi><mml:mo>→</mml:mo><mml:mn mathvariant="normal">0</mml:mn></mml:mrow></mml:math></inline-formula>) for a perpendicular shock in the corona <xref ref-type="bibr" rid="bib1.bibx105 bib1.bibx106" id="paren.32"/>, the density jump allows one to compute the Alfvén Mach number (<inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) using the Rankine–Hugoniot approximation as follows:
            <disp-formula id="Ch1.E3" content-type="numbered"><label>3</label><mml:math id="M26" display="block"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:msqrt><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi mathvariant="italic">χ</mml:mi><mml:mo>(</mml:mo><mml:mi mathvariant="italic">χ</mml:mi><mml:mo>+</mml:mo><mml:mn mathvariant="normal">5</mml:mn><mml:mo>)</mml:mo></mml:mrow><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mo>(</mml:mo><mml:mn mathvariant="normal">4</mml:mn><mml:mo>-</mml:mo><mml:mi mathvariant="italic">χ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mfrac></mml:mstyle></mml:msqrt><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula>
          It has been shown that the rate of change in the frequency of metric type II radio bursts is related to the shock speed and the electron density gradient in the solar corona <xref ref-type="bibr" rid="bib1.bibx25 bib1.bibx103" id="paren.33"><named-content content-type="pre">e.g.</named-content></xref> via the following:
            <disp-formula id="Ch1.E4" content-type="numbered"><label>4</label><mml:math id="M27" display="block"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mo>-</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mi>r</mml:mi></mml:mrow><mml:mi mathvariant="italic">α</mml:mi></mml:mfrac></mml:mstyle><mml:mfenced open="(" close=")"><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mn mathvariant="normal">1</mml:mn><mml:mi>f</mml:mi></mml:mfrac></mml:mstyle></mml:mfenced><mml:mfenced open="(" close=")"><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>f</mml:mi></mml:mrow><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:mfrac></mml:mstyle></mml:mfenced><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M28" display="inline"><mml:mi>r</mml:mi></mml:math></inline-formula> is the shock formation height, <inline-formula><mml:math id="M29" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula> is a fitted empirical index of density variation over the heliocentric distance, <inline-formula><mml:math id="M30" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula> is the starting frequency, and <inline-formula><mml:math id="M31" display="inline"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>f</mml:mi></mml:mrow><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:mfrac></mml:mstyle></mml:math></inline-formula> is the frequency drift rate. The electron density decreases with heliocentric distance from the Sun, according to the power law <inline-formula><mml:math id="M32" display="inline"><mml:mrow><mml:msub><mml:mi>n</mml:mi><mml:mi mathvariant="normal">e</mml:mi></mml:msub><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>∝</mml:mo><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mi mathvariant="italic">α</mml:mi></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. Three different density models by <xref ref-type="bibr" rid="bib1.bibx66" id="text.34"/>, <xref ref-type="bibr" rid="bib1.bibx80" id="text.35"/> and <xref ref-type="bibr" rid="bib1.bibx50" id="text.36"/> describe the variation in the electron density in the corona and interplanetary medium. With these models, it has been observed that within one to three solar radii <inline-formula><mml:math id="M33" display="inline"><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, the electron density is directly proportional to <inline-formula><mml:math id="M34" display="inline"><mml:mrow><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">6</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> in the corona and directly proportional to <inline-formula><mml:math id="M35" display="inline"><mml:mrow><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> beyond few tens of solar radii. Because the type II radio observed has all occurred in the range of <inline-formula><mml:math id="M36" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M37" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula> is chosen to be 6.13 <xref ref-type="bibr" rid="bib1.bibx25" id="paren.37"/>. The Alfvén velocity is directly related to the shock speed as
            <disp-formula id="Ch1.E5" content-type="numbered"><label>5</label><mml:math id="M38" display="block"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula>
          In the region surrounding a CME, the ambient magnetic field strength (<inline-formula><mml:math id="M39" display="inline"><mml:mi>B</mml:mi></mml:math></inline-formula>)  of the plasma can be estimated using the following relation <xref ref-type="bibr" rid="bib1.bibx106 bib1.bibx16 bib1.bibx49" id="paren.38"/>:
            <disp-formula id="Ch1.E6" content-type="numbered"><label>6</label><mml:math id="M40" display="block"><mml:mrow><mml:mi>B</mml:mi><mml:mo>[</mml:mo><mml:mi>G</mml:mi><mml:mo>]</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">5.1</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:msup><mml:mo>×</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub><mml:mo>[</mml:mo><mml:mi mathvariant="normal">MHz</mml:mi><mml:mo>]</mml:mo><mml:mo>×</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>[</mml:mo><mml:msup><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">s</mml:mi></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mo>]</mml:mo><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M41" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">l</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the lower frequency of the fundamental frequency band.</p>
</sec>
<sec id="Ch1.S2.SS3">
  <label>2.3</label><title>Ionospheric data and solar energetic particles</title>
      <p id="d1e1085">Data from ground-based GPS receiver stations around the world were used to analyse the ionospheric TEC for disturbed days identified by type II radio burst observations in this study. These include the African Geodetic Reference Frame (AFREF) database (<uri>http://afrefdata.org/</uri>, last access: 12 February 2024) and UNAVCO Archive of GNSS Data (<uri>https://www.unavco.org/</uri>, last access: 12 February 2024). Figure <xref ref-type="fig" rid="Ch1.F2"/> maps the geographic locations of some GNSS stations used in the current study for reference.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><?xmltex \currentcnt{2}?><?xmltex \def\figurename{Figure}?><label>Figure 2</label><caption><p id="d1e1098">Geographic locations of some GNSS station codes used for this study (FALK is the Falkland Islands (Islas Malvinas), British Overseas Territories; ABPO is in Madagascar; MBAR is in Uganda; SEY2 is the Seychelles; IISC is for India; YKRO is for Côte d'Ivoire; BOGT is in Colombia; BAKE is in Canada; and INVK is in Canada).</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f02.png"/>

        </fig>

      <p id="d1e1107">As GPS data are usually provided in a Receiver Independent EXchange (RINEX) format, TEC were derived from RINEX files using the GPS TEC software developed at Boston College, assuming a thin-shell ionosphere at the altitude of 350 km. Details on the software used to derive TEC are provided in <xref ref-type="bibr" rid="bib1.bibx88" id="text.39"/> and <xref ref-type="bibr" rid="bib1.bibx99" id="text.40"/> and references therein. To reduce the multipath effects on slant TEC (STEC), the elevation angle was fixed to <inline-formula><mml:math id="M42" display="inline"><mml:mrow><mml:mn mathvariant="normal">30</mml:mn><mml:mi mathvariant="italic">°</mml:mi></mml:mrow></mml:math></inline-formula>. The ROT was calculated using Eq. (<xref ref-type="disp-formula" rid="Ch1.E7"/>) proposed by <xref ref-type="bibr" rid="bib1.bibx74" id="text.41"/> and has been utilized by several researchers to explore ionospheric irregularities <xref ref-type="bibr" rid="bib1.bibx5 bib1.bibx55 bib1.bibx56 bib1.bibx21 bib1.bibx34" id="paren.42"/>.
            <disp-formula id="Ch1.E7" content-type="numbered"><label>7</label><mml:math id="M43" display="block"><mml:mrow><mml:mi mathvariant="normal">ROT</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi mathvariant="normal">STEC</mml:mi><mml:mrow><mml:mi>k</mml:mi><mml:mo>+</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi mathvariant="normal">STEC</mml:mi><mml:mi>k</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:msub><mml:mi>t</mml:mi><mml:mi>k</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where STEC<inline-formula><mml:math id="M44" display="inline"><mml:msub><mml:mi/><mml:mrow><mml:mi>k</mml:mi><mml:mo>+</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msub></mml:math></inline-formula> and STEC<inline-formula><mml:math id="M45" display="inline"><mml:msub><mml:mi/><mml:mi>k</mml:mi></mml:msub></mml:math></inline-formula> are the STEC values at two successive epochs, and <inline-formula><mml:math id="M46" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:msub><mml:mi>t</mml:mi><mml:mi>k</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the time difference between them equivalent to 30 s for the International GNSS Service (IGS) given in Fig. <xref ref-type="fig" rid="Ch1.F2"/>. Equation (<xref ref-type="disp-formula" rid="Ch1.E8"/>) was used to calculate the ROTI, which was defined as the standard deviation of ROT over 5 min.
            <disp-formula id="Ch1.E8" content-type="numbered"><label>8</label><mml:math id="M47" display="block"><mml:mrow><mml:mi mathvariant="normal">ROTI</mml:mi><mml:mo>=</mml:mo><mml:msqrt><mml:mrow><mml:mo>&lt;</mml:mo><mml:msup><mml:mi mathvariant="normal">ROT</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>&gt;</mml:mo><mml:mo>-</mml:mo><mml:mo>&lt;</mml:mo><mml:mi mathvariant="normal">ROT</mml:mi><mml:msup><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:msqrt><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where the <inline-formula><mml:math id="M48" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mo>&gt;</mml:mo></mml:mrow></mml:math></inline-formula> stands for the time-averaged value. The solar energetic particles were taken from the database at <uri>https://cdaweb.gsfc.nasa.gov/</uri> (last access: 19 February 2024).</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <label>3</label><title>Results and discussion</title>
<sec id="Ch1.S3.SS1">
  <label>3.1</label><title>Comparison and analysis</title>
      <p id="d1e1279">During the ascending phase of the solar cycle 25, the <inline-formula><mml:math id="M49" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO network observed a series of solar radio bursts in the range from 5 to 870 MHz. With the interest of space weather diagnostics, 32 well-separated type II radio bursts observed are presented in this study. Table <xref ref-type="table" rid="Ch1.T1"/> lists the spectrometers used in this study, as well as their geographic locations, frequency range of observation and number of radio bursts taken at each station. All spectrometers are observing in a narrow frequency range of few tens of megahertz.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><?xmltex \currentcnt{1}?><label>Table 1</label><caption><p id="d1e1294"><inline-formula><mml:math id="M50" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO Spectrometers, their geographical locations and their frequency ranges.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="7">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="right"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">No.</oasis:entry>
         <oasis:entry colname="col2">File ID</oasis:entry>
         <oasis:entry colname="col3">Country</oasis:entry>
         <oasis:entry colname="col4">Lat (°)</oasis:entry>
         <oasis:entry colname="col5">Long (°)</oasis:entry>
         <oasis:entry colname="col6">Obs. frequency range (MHz)</oasis:entry>
         <oasis:entry colname="col7">No. of events</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">1</oasis:entry>
         <oasis:entry colname="col2">Australia-ASSA</oasis:entry>
         <oasis:entry colname="col3">Australia</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M51" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">34.66</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">139.64</oasis:entry>
         <oasis:entry colname="col6">15–87</oasis:entry>
         <oasis:entry colname="col7">11</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2</oasis:entry>
         <oasis:entry colname="col2">Arecibo Observatory</oasis:entry>
         <oasis:entry colname="col3">Puerto Rico, USA</oasis:entry>
         <oasis:entry colname="col4">18.22</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M52" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">66.59</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6">15–87</oasis:entry>
         <oasis:entry colname="col7">9</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">3</oasis:entry>
         <oasis:entry colname="col2">GREENLAND</oasis:entry>
         <oasis:entry colname="col3">Greenland</oasis:entry>
         <oasis:entry colname="col4">67.00</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M53" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">50.72</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6">10–110</oasis:entry>
         <oasis:entry colname="col7">3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">4</oasis:entry>
         <oasis:entry colname="col2">ALASKA-HAARP</oasis:entry>
         <oasis:entry colname="col3">USA</oasis:entry>
         <oasis:entry colname="col4">62.40</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M54" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">150.20</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6">5–87</oasis:entry>
         <oasis:entry colname="col7">2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">5</oasis:entry>
         <oasis:entry colname="col2">ALMATY</oasis:entry>
         <oasis:entry colname="col3">Kazakhstan</oasis:entry>
         <oasis:entry colname="col4">43.22</oasis:entry>
         <oasis:entry colname="col5">76.83</oasis:entry>
         <oasis:entry colname="col6">45–165</oasis:entry>
         <oasis:entry colname="col7">1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">6</oasis:entry>
         <oasis:entry colname="col2">BIR</oasis:entry>
         <oasis:entry colname="col3">Ireland</oasis:entry>
         <oasis:entry colname="col4">16.61</oasis:entry>
         <oasis:entry colname="col5">77.51</oasis:entry>
         <oasis:entry colname="col6">10–100</oasis:entry>
         <oasis:entry colname="col7">2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">7</oasis:entry>
         <oasis:entry colname="col2">INDIAN-OOTY</oasis:entry>
         <oasis:entry colname="col3">India</oasis:entry>
         <oasis:entry colname="col4">11.41</oasis:entry>
         <oasis:entry colname="col5">76.69</oasis:entry>
         <oasis:entry colname="col6">45–165</oasis:entry>
         <oasis:entry colname="col7">1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">8</oasis:entry>
         <oasis:entry colname="col2">KASI</oasis:entry>
         <oasis:entry colname="col3">South Korea</oasis:entry>
         <oasis:entry colname="col4">36.35</oasis:entry>
         <oasis:entry colname="col5">127.38</oasis:entry>
         <oasis:entry colname="col6">150–400</oasis:entry>
         <oasis:entry colname="col7">1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">9</oasis:entry>
         <oasis:entry colname="col2">MEXICO-LANCE</oasis:entry>
         <oasis:entry colname="col3">Mexico</oasis:entry>
         <oasis:entry colname="col4">19.81</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M55" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">101.69</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6">50–90</oasis:entry>
         <oasis:entry colname="col7">1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">10</oasis:entry>
         <oasis:entry colname="col2">SWISS-Landschlacht</oasis:entry>
         <oasis:entry colname="col3">Switzerland</oasis:entry>
         <oasis:entry colname="col4">47.63</oasis:entry>
         <oasis:entry colname="col5">9.25</oasis:entry>
         <oasis:entry colname="col6">15–87</oasis:entry>
         <oasis:entry colname="col7">1</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><?xmltex \gdef\@currentlabel{1}?></table-wrap>

      <p id="d1e1645">Using the radio parameters such as bandwidth, drift rate and starting frequency, the shock characteristics from each radio event have been estimated. Table <xref ref-type="table" rid="Ch1.T2"/> illustrates each type II radio burst selected and the associated CME, GOES soft X-ray flares and shock characteristics. The first column of this table is the numbering index of the events, the next four columns are the date of the radio events in the format dd/mm/yyyy and hh:mm, their starting frequencies, <inline-formula><mml:math id="M56" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula> (MHz), their drift rates (MHz s<inline-formula><mml:math id="M57" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) and their shock formation heights (<inline-formula><mml:math id="M58" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>) estimated using the relation <inline-formula><mml:math id="M59" display="inline"><mml:mrow><mml:mi>f</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">307.87</mml:mn><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3.78</mml:mn></mml:mrow></mml:msup><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.14</mml:mn></mml:mrow></mml:math></inline-formula> <xref ref-type="bibr" rid="bib1.bibx29" id="paren.43"/>. Columns 6 to 9 are the GOES soft X-ray flare parameters (start, class, NOAA region and location), followed by two columns that present the CME onset and speed, respectively. Columns 12 to 15 present the shock characteristics (density jumps, Mach numbers, shock and Alfvén velocities, respectively), while the last column of this table presents the estimated ambient magnetic field strength B (Gauss).</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T2" specific-use="star"><?xmltex \currentcnt{2}?><label>Table 2</label><caption><p id="d1e1718">Type II radio bursts observed by <inline-formula><mml:math id="M60" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO during the ascending phase of solar cycle 25 and their associated CMEs, GOES soft X-ray flares and estimated shock characteristics.</p></caption><oasis:table frame="topbot"><?xmltex \begin{scaleboxenv}{.82}[.82]?><oasis:tgroup cols="16">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="center"/>
     <oasis:colspec colnum="5" colname="col5" align="center" colsep="1"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="left"/>
     <oasis:colspec colnum="8" colname="col8" align="left"/>
     <oasis:colspec colnum="9" colname="col9" align="left" colsep="1"/>
     <oasis:colspec colnum="10" colname="col10" align="right"/>
     <oasis:colspec colnum="11" colname="col11" align="right" colsep="1"/>
     <oasis:colspec colnum="12" colname="col12" align="center"/>
     <oasis:colspec colnum="13" colname="col13" align="center"/>
     <oasis:colspec colnum="14" colname="col14" align="right"/>
     <oasis:colspec colnum="15" colname="col15" align="center"/>
     <oasis:colspec colnum="16" colname="col16" align="center"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry rowsep="1" namest="col2" nameend="col5" align="center" colsep="1">Type II burst event </oasis:entry>
         <oasis:entry rowsep="1" namest="col6" nameend="col9" align="center" colsep="1">Soft X-ray flare </oasis:entry>
         <oasis:entry rowsep="1" namest="col10" nameend="col11" align="center" colsep="1">CME </oasis:entry>
         <oasis:entry rowsep="1" namest="col12" nameend="col15">Shock characteristics </oasis:entry>
         <oasis:entry colname="col16"/>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">No.</oasis:entry>
         <oasis:entry colname="col2">Date</oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M61" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4">Drift rate</oasis:entry>
         <oasis:entry colname="col5">Height</oasis:entry>
         <oasis:entry colname="col6">Start</oasis:entry>
         <oasis:entry colname="col7">Class</oasis:entry>
         <oasis:entry colname="col8">NOAA</oasis:entry>
         <oasis:entry colname="col9">Location</oasis:entry>
         <oasis:entry colname="col10">Onset</oasis:entry>
         <oasis:entry colname="col11">Speed</oasis:entry>
         <oasis:entry colname="col12"><inline-formula><mml:math id="M62" display="inline"><mml:mi mathvariant="italic">χ</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col13"><inline-formula><mml:math id="M63" display="inline"><mml:mi>M</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col14"><inline-formula><mml:math id="M64" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col15"><inline-formula><mml:math id="M65" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col16">B field</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">(UT)</oasis:entry>
         <oasis:entry colname="col3">(MHz)</oasis:entry>
         <oasis:entry colname="col4">(MHz<inline-formula><mml:math id="M66" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M67" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6">(UT)</oasis:entry>
         <oasis:entry colname="col7"/>
         <oasis:entry colname="col8"/>
         <oasis:entry colname="col9"/>
         <oasis:entry colname="col10">(UT)</oasis:entry>
         <oasis:entry colname="col11">(km<inline-formula><mml:math id="M68" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col12"/>
         <oasis:entry colname="col13"/>
         <oasis:entry colname="col14">(km<inline-formula><mml:math id="M69" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col15">(km<inline-formula><mml:math id="M70" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col16"><inline-formula><mml:math id="M71" display="inline"><mml:mi>G</mml:mi></mml:math></inline-formula></oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">1</oasis:entry>
         <oasis:entry colname="col2">22/05/2021 02:57</oasis:entry>
         <oasis:entry colname="col3">86</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M72" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">02:47</oasis:entry>
         <oasis:entry colname="col7">C6.1</oasis:entry>
         <oasis:entry colname="col8">12824</oasis:entry>
         <oasis:entry colname="col9">N18E25</oasis:entry>
         <oasis:entry colname="col10">…</oasis:entry>
         <oasis:entry colname="col11">…</oasis:entry>
         <oasis:entry colname="col12">1.6</oasis:entry>
         <oasis:entry colname="col13">1.5</oasis:entry>
         <oasis:entry colname="col14">752</oasis:entry>
         <oasis:entry colname="col15">504</oasis:entry>
         <oasis:entry colname="col16">1.5</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2</oasis:entry>
         <oasis:entry colname="col2">23/06/2021 07:05</oasis:entry>
         <oasis:entry colname="col3">73</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M73" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.10</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">06:43</oasis:entry>
         <oasis:entry colname="col7">C3.4</oasis:entry>
         <oasis:entry colname="col8">12833</oasis:entry>
         <oasis:entry colname="col9">N14E89</oasis:entry>
         <oasis:entry colname="col10">07:24</oasis:entry>
         <oasis:entry colname="col11">390</oasis:entry>
         <oasis:entry colname="col12">1.5</oasis:entry>
         <oasis:entry colname="col13">1.4</oasis:entry>
         <oasis:entry colname="col14">668</oasis:entry>
         <oasis:entry colname="col15">464</oasis:entry>
         <oasis:entry colname="col16">1.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">3</oasis:entry>
         <oasis:entry colname="col2">25/07/2021 04:54</oasis:entry>
         <oasis:entry colname="col3">64</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M74" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">…</oasis:entry>
         <oasis:entry colname="col7">…</oasis:entry>
         <oasis:entry colname="col8">F. S.</oasis:entry>
         <oasis:entry colname="col9">…</oasis:entry>
         <oasis:entry colname="col10">05:48</oasis:entry>
         <oasis:entry colname="col11">237</oasis:entry>
         <oasis:entry colname="col12">1.3</oasis:entry>
         <oasis:entry colname="col13">1.2</oasis:entry>
         <oasis:entry colname="col14">785</oasis:entry>
         <oasis:entry colname="col15">637</oasis:entry>
         <oasis:entry colname="col16">1.6</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">4</oasis:entry>
         <oasis:entry colname="col2">28/08/2021 05:10</oasis:entry>
         <oasis:entry colname="col3">64</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M75" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">05:01</oasis:entry>
         <oasis:entry colname="col7">C7.0</oasis:entry>
         <oasis:entry colname="col8">12860</oasis:entry>
         <oasis:entry colname="col9">S31E06</oasis:entry>
         <oasis:entry colname="col10">…</oasis:entry>
         <oasis:entry colname="col11">…</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">894</oasis:entry>
         <oasis:entry colname="col15">556</oasis:entry>
         <oasis:entry colname="col16">1.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">5</oasis:entry>
         <oasis:entry colname="col2">09/10/2021 06:34</oasis:entry>
         <oasis:entry colname="col3">75</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M76" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">06:19</oasis:entry>
         <oasis:entry colname="col7">M1.6</oasis:entry>
         <oasis:entry colname="col8">12882</oasis:entry>
         <oasis:entry colname="col9">N18E06</oasis:entry>
         <oasis:entry colname="col10">07:00</oasis:entry>
         <oasis:entry colname="col11">712</oasis:entry>
         <oasis:entry colname="col12">1.6</oasis:entry>
         <oasis:entry colname="col13">1.5</oasis:entry>
         <oasis:entry colname="col14">735</oasis:entry>
         <oasis:entry colname="col15">496</oasis:entry>
         <oasis:entry colname="col16">1.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">6</oasis:entry>
         <oasis:entry colname="col2">09/10/2021 06:49</oasis:entry>
         <oasis:entry colname="col3">31</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M77" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.04</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.9</oasis:entry>
         <oasis:entry colname="col6">06:19</oasis:entry>
         <oasis:entry colname="col7">M1.6</oasis:entry>
         <oasis:entry colname="col8">12882</oasis:entry>
         <oasis:entry colname="col9">N18E06</oasis:entry>
         <oasis:entry colname="col10">07:00</oasis:entry>
         <oasis:entry colname="col11">712</oasis:entry>
         <oasis:entry colname="col12">1.3</oasis:entry>
         <oasis:entry colname="col13">1.3</oasis:entry>
         <oasis:entry colname="col14">706</oasis:entry>
         <oasis:entry colname="col15">561</oasis:entry>
         <oasis:entry colname="col16">0.7</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">7</oasis:entry>
         <oasis:entry colname="col2">28/10/2021  15:28</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M78" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.18</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">15:17</oasis:entry>
         <oasis:entry colname="col7">X1.0</oasis:entry>
         <oasis:entry colname="col8">12887</oasis:entry>
         <oasis:entry colname="col9">S26W07</oasis:entry>
         <oasis:entry colname="col10">15:48</oasis:entry>
         <oasis:entry colname="col11">1519</oasis:entry>
         <oasis:entry colname="col12">2.0</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">1273</oasis:entry>
         <oasis:entry colname="col15">697</oasis:entry>
         <oasis:entry colname="col16">1.6</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">8</oasis:entry>
         <oasis:entry colname="col2">20/12/2021 11:27</oasis:entry>
         <oasis:entry colname="col3">87</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M79" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.14</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">11:12</oasis:entry>
         <oasis:entry colname="col7">M1.8</oasis:entry>
         <oasis:entry colname="col8">12908</oasis:entry>
         <oasis:entry colname="col9">S20W01</oasis:entry>
         <oasis:entry colname="col10">12:36</oasis:entry>
         <oasis:entry colname="col11">386</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">750</oasis:entry>
         <oasis:entry colname="col15">479</oasis:entry>
         <oasis:entry colname="col16">1.5</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">9</oasis:entry>
         <oasis:entry colname="col2">12/01/2022 04:28</oasis:entry>
         <oasis:entry colname="col3">69</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M80" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">…</oasis:entry>
         <oasis:entry colname="col7">…</oasis:entry>
         <oasis:entry colname="col8">F. S.</oasis:entry>
         <oasis:entry colname="col9">…</oasis:entry>
         <oasis:entry colname="col10">03:12</oasis:entry>
         <oasis:entry colname="col11">433</oasis:entry>
         <oasis:entry colname="col12">1.8</oasis:entry>
         <oasis:entry colname="col13">1.7</oasis:entry>
         <oasis:entry colname="col14">816</oasis:entry>
         <oasis:entry colname="col15">479</oasis:entry>
         <oasis:entry colname="col16">1.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">10</oasis:entry>
         <oasis:entry colname="col2">12/02/2022 08:33</oasis:entry>
         <oasis:entry colname="col3">173</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M81" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.36</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.2</oasis:entry>
         <oasis:entry colname="col6">08:25</oasis:entry>
         <oasis:entry colname="col7">M1.4</oasis:entry>
         <oasis:entry colname="col8">12939</oasis:entry>
         <oasis:entry colname="col9">S17W82</oasis:entry>
         <oasis:entry colname="col10">08:12</oasis:entry>
         <oasis:entry colname="col11">785</oasis:entry>
         <oasis:entry colname="col12">1.3</oasis:entry>
         <oasis:entry colname="col13">1.2</oasis:entry>
         <oasis:entry colname="col14">792</oasis:entry>
         <oasis:entry colname="col15">659</oasis:entry>
         <oasis:entry colname="col16">4.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">11</oasis:entry>
         <oasis:entry colname="col2">02/03/2022 17:42</oasis:entry>
         <oasis:entry colname="col3">67</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M82" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">17:31</oasis:entry>
         <oasis:entry colname="col7">M2.0</oasis:entry>
         <oasis:entry colname="col8">12958</oasis:entry>
         <oasis:entry colname="col9">N15E29</oasis:entry>
         <oasis:entry colname="col10">18:24</oasis:entry>
         <oasis:entry colname="col11">248</oasis:entry>
         <oasis:entry colname="col12">1.9</oasis:entry>
         <oasis:entry colname="col13">1.7</oasis:entry>
         <oasis:entry colname="col14">924</oasis:entry>
         <oasis:entry colname="col15">532</oasis:entry>
         <oasis:entry colname="col16">1.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">12</oasis:entry>
         <oasis:entry colname="col2">14/03/2022 17:20</oasis:entry>
         <oasis:entry colname="col3">98</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M83" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">17:13</oasis:entry>
         <oasis:entry colname="col7">B8.5</oasis:entry>
         <oasis:entry colname="col8">12964</oasis:entry>
         <oasis:entry colname="col9">S30W86</oasis:entry>
         <oasis:entry colname="col10">17:48</oasis:entry>
         <oasis:entry colname="col11">534</oasis:entry>
         <oasis:entry colname="col12">1.9</oasis:entry>
         <oasis:entry colname="col13">1.7</oasis:entry>
         <oasis:entry colname="col14">883</oasis:entry>
         <oasis:entry colname="col15">506</oasis:entry>
         <oasis:entry colname="col16">1.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">13</oasis:entry>
         <oasis:entry colname="col2">25/03/2022 05:15</oasis:entry>
         <oasis:entry colname="col3">66</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M84" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.12</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">05:02</oasis:entry>
         <oasis:entry colname="col7">M1.4</oasis:entry>
         <oasis:entry colname="col8">12974</oasis:entry>
         <oasis:entry colname="col9">S18E37</oasis:entry>
         <oasis:entry colname="col10">06:12</oasis:entry>
         <oasis:entry colname="col11">433</oasis:entry>
         <oasis:entry colname="col12">1.5</oasis:entry>
         <oasis:entry colname="col13">1.4</oasis:entry>
         <oasis:entry colname="col14">801</oasis:entry>
         <oasis:entry colname="col15">590</oasis:entry>
         <oasis:entry colname="col16">1.6</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">14</oasis:entry>
         <oasis:entry colname="col2">28/03/2022 11:23</oasis:entry>
         <oasis:entry colname="col3">87</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M85" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.15</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">10:58</oasis:entry>
         <oasis:entry colname="col7">M4.0</oasis:entry>
         <oasis:entry colname="col8">12975</oasis:entry>
         <oasis:entry colname="col9">N18W04</oasis:entry>
         <oasis:entry colname="col10">12:12</oasis:entry>
         <oasis:entry colname="col11">335</oasis:entry>
         <oasis:entry colname="col12">1.8</oasis:entry>
         <oasis:entry colname="col13">1.7</oasis:entry>
         <oasis:entry colname="col14">951</oasis:entry>
         <oasis:entry colname="col15">554</oasis:entry>
         <oasis:entry colname="col16">1.4</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">15</oasis:entry>
         <oasis:entry colname="col2">30/03/2022 17:33</oasis:entry>
         <oasis:entry colname="col3">72</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M86" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">17:21</oasis:entry>
         <oasis:entry colname="col7">X1.3</oasis:entry>
         <oasis:entry colname="col8">12975</oasis:entry>
         <oasis:entry colname="col9">N13W31</oasis:entry>
         <oasis:entry colname="col10">18:00</oasis:entry>
         <oasis:entry colname="col11">493</oasis:entry>
         <oasis:entry colname="col12">1.9</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">1128</oasis:entry>
         <oasis:entry colname="col15">654</oasis:entry>
         <oasis:entry colname="col16">1.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">16</oasis:entry>
         <oasis:entry colname="col2">31/03/2022 18:34</oasis:entry>
         <oasis:entry colname="col3">67</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M87" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">18:17</oasis:entry>
         <oasis:entry colname="col7">M9.6</oasis:entry>
         <oasis:entry colname="col8">12975</oasis:entry>
         <oasis:entry colname="col9">N12W47</oasis:entry>
         <oasis:entry colname="col10">19:12</oasis:entry>
         <oasis:entry colname="col11">489</oasis:entry>
         <oasis:entry colname="col12">2.0</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">1081</oasis:entry>
         <oasis:entry colname="col15">594</oasis:entry>
         <oasis:entry colname="col16">1.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">17</oasis:entry>
         <oasis:entry colname="col2">02/04/2022  13:24</oasis:entry>
         <oasis:entry colname="col3">71</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M88" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.15</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">12:56.</oasis:entry>
         <oasis:entry colname="col7">M3.9</oasis:entry>
         <oasis:entry colname="col8">12975</oasis:entry>
         <oasis:entry colname="col9">N12W68</oasis:entry>
         <oasis:entry colname="col10">13:36</oasis:entry>
         <oasis:entry colname="col11">686</oasis:entry>
         <oasis:entry colname="col12">1.8</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">1038</oasis:entry>
         <oasis:entry colname="col15">631</oasis:entry>
         <oasis:entry colname="col16">1.5</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">18</oasis:entry>
         <oasis:entry colname="col2">17/04/2022  03:28</oasis:entry>
         <oasis:entry colname="col3">382</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M89" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.83</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">0.9</oasis:entry>
         <oasis:entry colname="col6">03:17</oasis:entry>
         <oasis:entry colname="col7">X1.1</oasis:entry>
         <oasis:entry colname="col8">12994</oasis:entry>
         <oasis:entry colname="col9">N12E88</oasis:entry>
         <oasis:entry colname="col10">03:48</oasis:entry>
         <oasis:entry colname="col11">728</oasis:entry>
         <oasis:entry colname="col12">1.2</oasis:entry>
         <oasis:entry colname="col13">1.2</oasis:entry>
         <oasis:entry colname="col14">828</oasis:entry>
         <oasis:entry colname="col15">711</oasis:entry>
         <oasis:entry colname="col16">7.8</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">19</oasis:entry>
         <oasis:entry colname="col2">21/04/2022  02:00</oasis:entry>
         <oasis:entry colname="col3">85</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M90" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.15</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">01:47</oasis:entry>
         <oasis:entry colname="col7">M9.6</oasis:entry>
         <oasis:entry colname="col8">12993</oasis:entry>
         <oasis:entry colname="col9">N22E23</oasis:entry>
         <oasis:entry colname="col10">02:36</oasis:entry>
         <oasis:entry colname="col11">828</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.5</oasis:entry>
         <oasis:entry colname="col14">1070</oasis:entry>
         <oasis:entry colname="col15">696</oasis:entry>
         <oasis:entry colname="col16">1.6</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">20</oasis:entry>
         <oasis:entry colname="col2">21/04/2022 22:47</oasis:entry>
         <oasis:entry colname="col3">69</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M91" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">22:39</oasis:entry>
         <oasis:entry colname="col7">C1.6</oasis:entry>
         <oasis:entry colname="col8">12993</oasis:entry>
         <oasis:entry colname="col9">N12E25</oasis:entry>
         <oasis:entry colname="col10">23:12</oasis:entry>
         <oasis:entry colname="col11">389</oasis:entry>
         <oasis:entry colname="col12">1.4</oasis:entry>
         <oasis:entry colname="col13">1.3</oasis:entry>
         <oasis:entry colname="col14">791</oasis:entry>
         <oasis:entry colname="col15">591</oasis:entry>
         <oasis:entry colname="col16">1.4</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">21</oasis:entry>
         <oasis:entry colname="col2">30/04/2022 13:46</oasis:entry>
         <oasis:entry colname="col3">83</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M92" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">13:37</oasis:entry>
         <oasis:entry colname="col7">X1.1</oasis:entry>
         <oasis:entry colname="col8">12994</oasis:entry>
         <oasis:entry colname="col9">N16W88</oasis:entry>
         <oasis:entry colname="col10">14:00</oasis:entry>
         <oasis:entry colname="col11">535</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.5</oasis:entry>
         <oasis:entry colname="col14">936</oasis:entry>
         <oasis:entry colname="col15">610</oasis:entry>
         <oasis:entry colname="col16">1.4</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">22</oasis:entry>
         <oasis:entry colname="col2">30/04/2022 19:50</oasis:entry>
         <oasis:entry colname="col3">80</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M93" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.12</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">19:42</oasis:entry>
         <oasis:entry colname="col7">M1.9</oasis:entry>
         <oasis:entry colname="col8">12994</oasis:entry>
         <oasis:entry colname="col9">N16W88</oasis:entry>
         <oasis:entry colname="col10">20:12</oasis:entry>
         <oasis:entry colname="col11">793</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">855</oasis:entry>
         <oasis:entry colname="col15">543</oasis:entry>
         <oasis:entry colname="col16">1.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">23</oasis:entry>
         <oasis:entry colname="col2">04/07/2022 13:35</oasis:entry>
         <oasis:entry colname="col3">69</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M94" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">12:23</oasis:entry>
         <oasis:entry colname="col7">C5.1</oasis:entry>
         <oasis:entry colname="col8">13050</oasis:entry>
         <oasis:entry colname="col9">N17E36</oasis:entry>
         <oasis:entry colname="col10">11:36</oasis:entry>
         <oasis:entry colname="col11">256</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">918</oasis:entry>
         <oasis:entry colname="col15">581</oasis:entry>
         <oasis:entry colname="col16">1.4</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">24</oasis:entry>
         <oasis:entry colname="col2">05/07/2022 04:16</oasis:entry>
         <oasis:entry colname="col3">69</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M95" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.10</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">03:59</oasis:entry>
         <oasis:entry colname="col7">C9.8</oasis:entry>
         <oasis:entry colname="col8">13045</oasis:entry>
         <oasis:entry colname="col9">S20W18</oasis:entry>
         <oasis:entry colname="col10">05:00</oasis:entry>
         <oasis:entry colname="col11">515</oasis:entry>
         <oasis:entry colname="col12">1.6</oasis:entry>
         <oasis:entry colname="col13">1.5</oasis:entry>
         <oasis:entry colname="col14">761</oasis:entry>
         <oasis:entry colname="col15">512</oasis:entry>
         <oasis:entry colname="col16">1.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">25</oasis:entry>
         <oasis:entry colname="col2">14/08/2022 12:05</oasis:entry>
         <oasis:entry colname="col3">70</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M96" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.08</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">11:50</oasis:entry>
         <oasis:entry colname="col7">C2.4</oasis:entry>
         <oasis:entry colname="col8">13076</oasis:entry>
         <oasis:entry colname="col9">N21W14</oasis:entry>
         <oasis:entry colname="col10">13:25</oasis:entry>
         <oasis:entry colname="col11">411</oasis:entry>
         <oasis:entry colname="col12">1.4</oasis:entry>
         <oasis:entry colname="col13">1.3</oasis:entry>
         <oasis:entry colname="col14">512</oasis:entry>
         <oasis:entry colname="col15">402</oasis:entry>
         <oasis:entry colname="col16">1.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">26</oasis:entry>
         <oasis:entry colname="col2">18/08/2022 12:12</oasis:entry>
         <oasis:entry colname="col3">62</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M97" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.16</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.6</oasis:entry>
         <oasis:entry colname="col6">…</oasis:entry>
         <oasis:entry colname="col7">…</oasis:entry>
         <oasis:entry colname="col8">F. S.</oasis:entry>
         <oasis:entry colname="col9">…</oasis:entry>
         <oasis:entry colname="col10">11:00</oasis:entry>
         <oasis:entry colname="col11">1131</oasis:entry>
         <oasis:entry colname="col12">1.7</oasis:entry>
         <oasis:entry colname="col13">1.6</oasis:entry>
         <oasis:entry colname="col14">1282</oasis:entry>
         <oasis:entry colname="col15">826</oasis:entry>
         <oasis:entry colname="col16">1.9</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">27</oasis:entry>
         <oasis:entry colname="col2">19/08/2022 04:35</oasis:entry>
         <oasis:entry colname="col3">81</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M98" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.10</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">04:14</oasis:entry>
         <oasis:entry colname="col7">M1.6</oasis:entry>
         <oasis:entry colname="col8">13078</oasis:entry>
         <oasis:entry colname="col9">S27W48</oasis:entry>
         <oasis:entry colname="col10">04:49</oasis:entry>
         <oasis:entry colname="col11">695</oasis:entry>
         <oasis:entry colname="col12">1.3</oasis:entry>
         <oasis:entry colname="col13">1.2</oasis:entry>
         <oasis:entry colname="col14">504</oasis:entry>
         <oasis:entry colname="col15">420</oasis:entry>
         <oasis:entry colname="col16">1.4</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">28</oasis:entry>
         <oasis:entry colname="col2">23/09/2022 18:02</oasis:entry>
         <oasis:entry colname="col3">67</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M99" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.12</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.5</oasis:entry>
         <oasis:entry colname="col6">17:48</oasis:entry>
         <oasis:entry colname="col7">M1.7</oasis:entry>
         <oasis:entry colname="col8">13110</oasis:entry>
         <oasis:entry colname="col9">N16E84</oasis:entry>
         <oasis:entry colname="col10">18:12</oasis:entry>
         <oasis:entry colname="col11">687</oasis:entry>
         <oasis:entry colname="col12">2.0</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">1010</oasis:entry>
         <oasis:entry colname="col15">548</oasis:entry>
         <oasis:entry colname="col16">1.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">29</oasis:entry>
         <oasis:entry colname="col2">29/09/2022 12:06</oasis:entry>
         <oasis:entry colname="col3">80</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M100" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.10</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">11:50</oasis:entry>
         <oasis:entry colname="col7">C5.7</oasis:entry>
         <oasis:entry colname="col8">…</oasis:entry>
         <oasis:entry colname="col9">N26E86</oasis:entry>
         <oasis:entry colname="col10">12:24</oasis:entry>
         <oasis:entry colname="col11">321</oasis:entry>
         <oasis:entry colname="col12">1.5</oasis:entry>
         <oasis:entry colname="col13">1.4</oasis:entry>
         <oasis:entry colname="col14">672</oasis:entry>
         <oasis:entry colname="col15">473</oasis:entry>
         <oasis:entry colname="col16">1.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">30</oasis:entry>
         <oasis:entry colname="col2">09/11/2022  20:03</oasis:entry>
         <oasis:entry colname="col3">89</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M101" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.11</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">…</oasis:entry>
         <oasis:entry colname="col7">…</oasis:entry>
         <oasis:entry colname="col8">F. S.</oasis:entry>
         <oasis:entry colname="col9">…</oasis:entry>
         <oasis:entry colname="col10">20:36</oasis:entry>
         <oasis:entry colname="col11">371</oasis:entry>
         <oasis:entry colname="col12">1.5</oasis:entry>
         <oasis:entry colname="col13">1.4</oasis:entry>
         <oasis:entry colname="col14">618</oasis:entry>
         <oasis:entry colname="col15">435</oasis:entry>
         <oasis:entry colname="col16">1.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">31</oasis:entry>
         <oasis:entry colname="col2">03/12/2022 17:44</oasis:entry>
         <oasis:entry colname="col3">84</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M102" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.13</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.4</oasis:entry>
         <oasis:entry colname="col6">17:36</oasis:entry>
         <oasis:entry colname="col7">M1.2</oasis:entry>
         <oasis:entry colname="col8">13157</oasis:entry>
         <oasis:entry colname="col9">N14E89</oasis:entry>
         <oasis:entry colname="col10">…</oasis:entry>
         <oasis:entry colname="col11">…</oasis:entry>
         <oasis:entry colname="col12">1.8</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">857</oasis:entry>
         <oasis:entry colname="col15">518</oasis:entry>
         <oasis:entry colname="col16">1.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">32</oasis:entry>
         <oasis:entry colname="col2">14/12/2022 08:30</oasis:entry>
         <oasis:entry colname="col3">160</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M103" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.22</mml:mn></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5">1.2</oasis:entry>
         <oasis:entry colname="col6">08:24</oasis:entry>
         <oasis:entry colname="col7">M1.1</oasis:entry>
         <oasis:entry colname="col8">13162</oasis:entry>
         <oasis:entry colname="col9">S16W89</oasis:entry>
         <oasis:entry colname="col10">08:48</oasis:entry>
         <oasis:entry colname="col11">402</oasis:entry>
         <oasis:entry colname="col12">1.9</oasis:entry>
         <oasis:entry colname="col13">1.8</oasis:entry>
         <oasis:entry colname="col14">657</oasis:entry>
         <oasis:entry colname="col15">368</oasis:entry>
         <oasis:entry colname="col16">1.7</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup><?xmltex \end{scaleboxenv}?></oasis:table><?xmltex \gdef\@currentlabel{2}?></table-wrap>

      <?pagebreak page317?><p id="d1e3946">There is a strong correlation (CC <inline-formula><mml:math id="M104" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.98</mml:mn></mml:mrow></mml:math></inline-formula>) between the drift rates and starting frequencies of the type II radio bursts (Fig. <xref ref-type="fig" rid="Ch1.F3"/>), which are the key parameters to estimate the shock speeds from the dynamic spectra. Higher starting frequency have higher drift rates <xref ref-type="bibr" rid="bib1.bibx98" id="paren.44"/>. Such a correlation agrees well with the previous studies, giving slopes of <inline-formula><mml:math id="M105" display="inline"><mml:mrow><mml:mi mathvariant="italic">ϵ</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1.89</mml:mn></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M106" display="inline"><mml:mrow><mml:mi mathvariant="italic">ϵ</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1.33</mml:mn></mml:mrow></mml:math></inline-formula>, respectively <xref ref-type="bibr" rid="bib1.bibx106 bib1.bibx98" id="paren.45"><named-content content-type="pre">e.g.</named-content></xref>.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3"><?xmltex \currentcnt{3}?><?xmltex \def\figurename{Figure}?><label>Figure 3</label><caption><p id="d1e3996">Scatterplot between the absolute drift rates <inline-formula><mml:math id="M107" display="inline"><mml:mrow><mml:mfenced open="(" close=")"><mml:mrow><mml:mo>|</mml:mo><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>f</mml:mi></mml:mrow><mml:mrow><mml:mi mathvariant="normal">d</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>|</mml:mo></mml:mrow></mml:mfenced></mml:mrow></mml:math></inline-formula> and the starting frequency (<inline-formula><mml:math id="M108" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) for all 32 metric type II radio bursts. The power law least squares fits and the corresponding correlation coefficient (CC) are shown.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f03.png"/>

        </fig>

      <?pagebreak page318?><p id="d1e4040">From Table <xref ref-type="table" rid="Ch1.T2"/>, it is clearly observed that 4 out of 32 radio events are not associated with any solar flare because they originate from the far side on the solar surface, but the shocks generating these bursts were excited by associated CMEs. It is also noticed that 19 out of 28 are connected with intense GOES X-ray flares (M and X classes), which is compatible with their speeds, as well as estimated shock speeds. We derived the shock and Alfvén speeds of these type II radio bursts of the order of 504–1282 and 368–826 km<inline-formula><mml:math id="M109" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, respectively, at heliocentric distance <inline-formula><mml:math id="M110" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M111" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace linebreak="nobreak" width="0.25em"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. Comparatively, values are consistent with the measurements reported by <xref ref-type="bibr" rid="bib1.bibx18 bib1.bibx61" id="text.46"/> about 590–810  and 250–550 km<inline-formula><mml:math id="M112" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, respectively, at <inline-formula><mml:math id="M113" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.2</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M114" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.8</mml:mn><mml:mspace linebreak="nobreak" width="0.25em"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. The Alfvén speeds from the current work are also in agreement with the range of the Alfvén speeds of 140–460 km<inline-formula><mml:math id="M115" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> over 1.2–1.5 <inline-formula><mml:math id="M116" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> and 259–982 km<inline-formula><mml:math id="M117" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> over  3–15 <inline-formula><mml:math id="M118" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> given in <xref ref-type="bibr" rid="bib1.bibx26" id="text.47"/> and in <xref ref-type="bibr" rid="bib1.bibx40" id="text.48"/>, respectively. Figure <xref ref-type="fig" rid="Ch1.F4"/> presents the correlation between the speeds from the LASCO field of view (FOV) and the speeds derived from the dynamic spectra.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4"><?xmltex \currentcnt{4}?><?xmltex \def\figurename{Figure}?><label>Figure 4</label><caption><p id="d1e4178">Scatterplot showing the correlation between the speeds from LASCO FOV and speeds derived from dynamic spectra. Higher values of speeds obtained from dynamic spectra are attributed to the radio source, which propagates at faster speeds due to the interaction of slow CMEs with background magnetized coronal plasma <xref ref-type="bibr" rid="bib1.bibx95" id="paren.49"/>.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f04.png"/>

        </fig>

      <p id="d1e4191">The Table <xref ref-type="table" rid="Ch1.T2"/> observations and Fig. <xref ref-type="fig" rid="Ch1.F4"/> show that there are estimated shock speeds that are faster than CME speeds from LASCO FOV, and vice versa. The difference in CME speed between dynamic spectra and LASCO is attributed to the CME's central position angle as observed by LASCO, implying that the shock may be weakened and dissipated before entering LASCO FOV <xref ref-type="bibr" rid="bib1.bibx28" id="paren.50"/>. On the other hand, the shock decelerates in the case of a decline in its intensity or when it breaks. The type II burst only serves as a time marker for when the shock occurs. It should be noted that type II radio emission can come from anywhere on the shock front, namely the nose or the flanks, depending on which location is best for electron acceleration <xref ref-type="bibr" rid="bib1.bibx29" id="paren.51"/>. Solar radio type II bursts associated with slow CMEs are thought to be generated from non-thermal electrons accelerated by a moving magnetic reconnection when slow CMEs interact with the background magnetized coronal plasma <xref ref-type="bibr" rid="bib1.bibx95" id="paren.52"/>. Furthermore, a recent study confirmed that observing a type II radio burst is evidence of shock acceleration in the solar corona <xref ref-type="bibr" rid="bib1.bibx15" id="paren.53"/>. The Alfvén Mach numbers in the range <inline-formula><mml:math id="M119" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.2</mml:mn></mml:mrow></mml:math></inline-formula>–1.8 at <inline-formula><mml:math id="M120" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M121" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> are consistent with the measurements of about 1.1–1.9 at <inline-formula><mml:math id="M122" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M123" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.5</mml:mn><mml:mspace linebreak="nobreak" width="0.25em"/><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:mrow></mml:math></inline-formula> reported by <xref ref-type="bibr" rid="bib1.bibx106" id="text.54"/> and that of <xref ref-type="bibr" rid="bib1.bibx18" id="text.55"/> of the order of 1.4 to 1.7 at <inline-formula><mml:math id="M124" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.2</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M125" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.8</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. The magnetic field strength is an important parameter that influences the dynamical eruption of CMEs in the solar atmosphere <xref ref-type="bibr" rid="bib1.bibx83 bib1.bibx12" id="paren.56"/>. High-starting type II radio bursts are associated with coronal shocks that are closer to the solar surface. As a result, high magnetic field values are expected. Figure <xref ref-type="fig" rid="Ch1.F5"/> demonstrates the variation in the magnetic field strength estimated in this study (Eq. <xref ref-type="disp-formula" rid="Ch1.E6"/>) relative to the quiet Sun magnetic field model <inline-formula><mml:math id="M126" display="inline"><mml:mrow><mml:mi>B</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mi>a</mml:mi><mml:mrow><mml:msup><mml:mi>r</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:mfrac></mml:mstyle></mml:mrow></mml:math></inline-formula> with <inline-formula><mml:math id="M127" display="inline"><mml:mrow><mml:mi>a</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">2.2</mml:mn></mml:mrow></mml:math></inline-formula> <xref ref-type="bibr" rid="bib1.bibx27" id="paren.57"/> and <xref ref-type="bibr" rid="bib1.bibx22" id="text.58"/> empirical model for the magnetic field above active region <inline-formula><mml:math id="M128" display="inline"><mml:mrow><mml:mi>B</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mfenced close=")" open="("><mml:mrow><mml:mi>r</mml:mi><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:mfenced><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1.5</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The magnetic field has been calculated in the range <inline-formula><mml:math id="M129" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:mo>&lt;</mml:mo><mml:mi>B</mml:mi><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">8</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula> at <inline-formula><mml:math id="M130" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M131" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>, which shows  excellent consistency with earlier research and is fitted with a single power law distribution of the type <inline-formula><mml:math id="M132" display="inline"><mml:mrow><mml:mi>B</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">6.07</mml:mn><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3.96</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula>, as represented by the dotted black curve in Fig. <xref ref-type="fig" rid="Ch1.F5"/>.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5"><?xmltex \currentcnt{5}?><?xmltex \def\figurename{Figure}?><label>Figure 5</label><caption><p id="d1e4460">Comparison of the magnetic field strength from the current study, the quiet Sun magnetic field model <xref ref-type="bibr" rid="bib1.bibx27" id="paren.59"/> and the empirical magnetic field relation <xref ref-type="bibr" rid="bib1.bibx22" id="paren.60"/>. The magnetic values estimated are all above the quiet Sun magnetic model, and the pattern is close to the empirical model, which confirms that the Sun was awake.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f05.png"/>

        </fig>

      <p id="d1e4475">However, Rankine–Hugoniot jump relation has been used by a number of researchers to derive shock parameters. For example, with this technique, <xref ref-type="bibr" rid="bib1.bibx90 bib1.bibx91" id="text.61"/> found <inline-formula><mml:math id="M133" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.2</mml:mn><mml:mo>≤</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">1.7</mml:mn></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M134" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.3</mml:mn><mml:mo>≤</mml:mo><mml:mi>B</mml:mi><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">4</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula>. The same technique was applied by <xref ref-type="bibr" rid="bib1.bibx106" id="text.62"/>, who  reported a magnetic field strength in the range 1–8 <inline-formula><mml:math id="M135" display="inline"><mml:mi>G</mml:mi></mml:math></inline-formula> at heliocentric distance of <inline-formula><mml:math id="M136" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.6</mml:mn><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. A field strength of 6–5 <inline-formula><mml:math id="M137" display="inline"><mml:mi>G</mml:mi></mml:math></inline-formula> at <inline-formula><mml:math id="M138" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.5</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M139" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.77</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> is reported by <xref ref-type="bibr" rid="bib1.bibx76" id="text.63"/>.  <xref ref-type="bibr" rid="bib1.bibx22" id="text.64"/> and <xref ref-type="bibr" rid="bib1.bibx87" id="text.65"/> have given a detailed review on solar coronal magnetic fields measured using different techniques and at different wavelengths of the electromagnetic spectrum. A recent work has reported that two necessary conditions for type II radio emissions, (i) relatively intense shock waves (the Mach number should exceed a certain value <inline-formula><mml:math id="M140" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">cr</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) and (ii) perpendicular shock waves, are required <xref ref-type="bibr" rid="bib1.bibx15" id="paren.66"/>. Our values of Mach numbers <inline-formula><mml:math id="M141" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.2</mml:mn><mml:mo>≤</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">1.8</mml:mn></mml:mrow></mml:math></inline-formula> agree well with these conditions. In Table <xref ref-type="table" rid="Ch1.T3"/>, the statistical findings from this study and<?pagebreak page319?> earlier research that examined more than two radio events are summarized and compared.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T3" specific-use="star"><?xmltex \currentcnt{3}?><label>Table 3</label><caption><p id="d1e4624">Comparison of the statistical findings of this study and previous studies that analysed more than two radio events.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="7">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="center"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="left"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Epoch</oasis:entry>
         <oasis:entry colname="col2">No. of events</oasis:entry>
         <oasis:entry colname="col3">Mean shock</oasis:entry>
         <oasis:entry colname="col4">Mean Alfvén</oasis:entry>
         <oasis:entry colname="col5">B-field range</oasis:entry>
         <oasis:entry colname="col6">Height range</oasis:entry>
         <oasis:entry colname="col7">Citation</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">(<inline-formula><mml:math id="M142" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">Citation</oasis:entry>
         <oasis:entry colname="col3"/>
         <oasis:entry colname="col4"/>
         <oasis:entry colname="col5"/>
         <oasis:entry colname="col6"/>
         <oasis:entry colname="col7"/>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">2021–2022</oasis:entry>
         <oasis:entry colname="col2">32</oasis:entry>
         <oasis:entry colname="col3">860</oasis:entry>
         <oasis:entry colname="col4">566</oasis:entry>
         <oasis:entry colname="col5">8–0.5</oasis:entry>
         <oasis:entry colname="col6">1.0–2.0</oasis:entry>
         <oasis:entry colname="col7">This work</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2013–2014</oasis:entry>
         <oasis:entry colname="col2">4</oasis:entry>
         <oasis:entry colname="col3">739</oasis:entry>
         <oasis:entry colname="col4">579</oasis:entry>
         <oasis:entry colname="col5">1.8–1.3</oasis:entry>
         <oasis:entry colname="col6">1.7–1.9</oasis:entry>
         <oasis:entry colname="col7">
                    <xref ref-type="bibr" rid="bib1.bibx41" id="text.67"/>
                  </oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">1996–2007</oasis:entry>
         <oasis:entry colname="col2">10</oasis:entry>
         <oasis:entry colname="col3">1288</oasis:entry>
         <oasis:entry colname="col4">555</oasis:entry>
         <oasis:entry colname="col5">0.105–0.006</oasis:entry>
         <oasis:entry colname="col6">3–15</oasis:entry>
         <oasis:entry colname="col7">
                    <xref ref-type="bibr" rid="bib1.bibx40" id="text.68"/>
                  </oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><?xmltex \gdef\@currentlabel{3}?></table-wrap>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6"><?xmltex \currentcnt{6}?><?xmltex \def\figurename{Figure}?><label>Figure 6</label><caption><p id="d1e4793">Type II radio emissions observed on 28 October 2021 overlapped by a type IV radio emission from 15:32 to 15:43 UT.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f06.png"/>

        </fig>

</sec>
<sec id="Ch1.S3.SS2">
  <label>3.2</label><title>Associated space weather implication</title>
      <p id="d1e4810">The ascending phase of solar cycle 25 is characterized by more intense solar activity than expected <xref ref-type="bibr" rid="bib1.bibx19 bib1.bibx35 bib1.bibx38" id="paren.69"><named-content content-type="pre">e.g.</named-content></xref>. <xref ref-type="bibr" rid="bib1.bibx94" id="text.70"/> and <xref ref-type="bibr" rid="bib1.bibx82" id="text.71"/> show that solar cycle 25 is more active than the previous cycle and is more consistent with actual observations as predicted. Furthermore, <xref ref-type="bibr" rid="bib1.bibx20" id="text.72"/> estimated that the maximum peak of cycle 25 would be 30 % stronger than that of cycle 24. These indicate that the activity would be high, and we use this advantage to track the intensity of early space weather events in the current cycle. To account for ionospheric irregularities caused by concurrent GOES X-ray flares, type II solar radio bursts were utilized as selection criteria for disturbed days due to their association with solar phenomena such as radio blackouts. The ROTI were examined on 25 type II radio bursts, which are linked to both solar flares and CMEs, by selecting GNSS stations in either equatorial, mid-latitude or high-latitude regions. Furthermore, the ROTI classifies the irregularities of the ionospheric TEC as no TEC irregularity (ROTI <inline-formula><mml:math id="M143" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">0.25</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M144" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>), weak (<inline-formula><mml:math id="M145" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.25</mml:mn><mml:mo>≤</mml:mo></mml:mrow></mml:math></inline-formula> ROTI <inline-formula><mml:math id="M146" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M147" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>), moderate (<inline-formula><mml:math id="M148" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:mo>≤</mml:mo></mml:mrow></mml:math></inline-formula> ROTI <inline-formula><mml:math id="M149" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">1.0</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M150" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) and strong (ROTI <inline-formula><mml:math id="M151" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">1.0</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M152" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) <xref ref-type="bibr" rid="bib1.bibx55" id="paren.73"/>. It is worth noting that four major solar energetic particles (<inline-formula><mml:math id="M153" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> MeV; SEPs) occurred on days when type II radio bursts are observed, and these dates are used as illustrative examples in this study.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7" specific-use="star"><?xmltex \currentcnt{7}?><?xmltex \def\figurename{Figure}?><label>Figure 7</label><caption><p id="d1e4952">Variability in the ROTI in the <bold>(a)</bold> equatorial region (SEY2), <bold>(b)</bold> mid-latitude region (IISC), <bold>(c)</bold> high-latitude region (BOGT) and <bold>(d)</bold> associated GOES soft X-ray X1.0 flare intensity profile.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f07.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><?xmltex \currentcnt{8}?><?xmltex \def\figurename{Figure}?><label>Figure 8</label><caption><p id="d1e4975">Profile of the particle intensity of the SEP on 28 October 2021 in five energy levels, with the onset at 17:00 UT and peak at 18:26 UT.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f08.png"/>

        </fig>

<sec id="Ch1.S3.SS2.SSS1">
  <label>3.2.1</label><title>28 October 2021 event</title>
      <p id="d1e4992">Type II radio bursts on 28 October 2021 were recorded by the CALLISTO spectrometer, Birr Castle, Ireland. This type II burst is recorded in the time range from 15:28 to 15:38 UT, which overlapped by a type IV radio burst from 15:32 to 15:43 UT as indicated in Fig. <xref ref-type="fig" rid="Ch1.F6"/>. This radio event is associated with the GOES soft X-ray flare of X1.0 class that started at 15:17 UT, peaked at 15:35 UT and stopped at 15:38 UT from the NOAA active region (AR) 12 887 explosion.</p>
      <p id="d1e4997">It is also associated with energetic halo CME observed by LASCO C2 coronagraph with onset at 15:48 UT with a speed of 1519 km<inline-formula><mml:math id="M154" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>. This CME did not reach near the Earth, and therefore, no geomagnetic storm was recorded in next 5 d. It is observed that a few minutes after the type II had started, an enhancement of protons took place as an effect of radio blackout (R3; major, <uri>https://spaceweather.com/images2021/28oct21/blackout_x1.jpg</uri>, last access: 15 February 2024) which affected the whole South America and Atlantic Ocean. Figure <xref ref-type="fig" rid="Ch1.F7"/> depicts the ionospheric irregularities in terms of ROTI observed in different region of the globe.</p>
      <?pagebreak page320?><p id="d1e5017">It is noted that the flare has no direct interaction with the magnetosphere, but its radiation agents (X-rays, UV and EUV) perturb the ionosphere by increasing the ionization which in turn causes the signal delay in global navigation satellite systems (GNSSs) <xref ref-type="bibr" rid="bib1.bibx4" id="paren.74"><named-content content-type="pre">e.g.</named-content></xref>. Figure <xref ref-type="fig" rid="Ch1.F7"/> clearly shows that there is no ionospheric perturbation associated with the X1.0 flare in the equatorial region over Seychelles (Fig. <xref ref-type="fig" rid="Ch1.F7"/>a), whereas ROTI is strongly suppressed in the mid-latitude zone over India (Fig. <xref ref-type="fig" rid="Ch1.F7"/>b). The ROTI profile in high-latitude region over Colombia (Fig. <xref ref-type="fig" rid="Ch1.F7"/>c) is consistent with the X1.0 flare flux profile (Fig. <xref ref-type="fig" rid="Ch1.F7"/>d). According to <xref ref-type="bibr" rid="bib1.bibx33" id="text.75"/>, the F2 layer was unaffected by the X1.0 flare on 28 October 2021. However, ROTI is strongly suppressed in equatorial region (SEY2) when substantial SEP arrives at 17:00 UT. On this day, a major SEP (<inline-formula><mml:math id="M155" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> MeV) is observed with an onset time of roughly 17:00 UT on the high-energy detector (HED) on board the Solar and Heliospheric Observatory (SOHO) Energetic and Relativistic Nuclei and Electron (ERNE) experiment, as shown in Fig. <xref ref-type="fig" rid="Ch1.F8"/>.</p>
      <p id="d1e5051">However, the neutron monitor (<uri>https://gle.oulu.fi/</uri>, last access: 16 February 2024) recorded the SEP on 28 October 2021 as a ground-level event (GLE) that started at 15:46 UT <xref ref-type="bibr" rid="bib1.bibx42" id="paren.76"/>.</p>
</sec>
<sec id="Ch1.S3.SS2.SSS2">
  <label>3.2.2</label><title>28 March  2022 event</title>
      <p id="d1e5068">The solar activity is seen to be high during March 2022. This is due to a number of solar events observed and recorded during this month where seven type II radio events were recorded in March 2022. Figure <xref ref-type="fig" rid="Ch1.F9"/> presents a type II radio burst observed by the <inline-formula><mml:math id="M156" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO network at Arecibo Observatory in Puerto Rico, USA, from 11:23:12 to 11:28:37 UT on 28 March 2022 within the 87–32 MHz frequency range. This burst is overlapped by a type IV radio burst that occurred from 11:26 to 11:36 UT. These bursts are associated with a GOES soft X-ray flare M4.0 that started at 10:58 UT, peaked at 11:29 UT and stopped at 11:45 UT from NOAA 12 975. This eruption also produced a tsunami in the solar atmosphere (see <uri>https://sdo.gsfc.nasa.gov/data/dailymov/movie.php?q=20220328_1024_0193</uri>, last access: 15 February 2024).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F9"><?xmltex \currentcnt{9}?><?xmltex \def\figurename{Figure}?><label>Figure 9</label><caption><p id="d1e5085">The type II radio emissions that are observed on 28 March 2022 from 11:23:12 to 11:28:37 UT followed by a type IV radio bursts from 11:26 to 11:36 UT.</p></caption>
            <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f09.png"/>

          </fig>

      <?pagebreak page321?><p id="d1e5094">The bursts are also associated with a partial halo CME with speed of 335 km<inline-formula><mml:math id="M157" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, and the CME was off the Sun–Earth line because no geomagnetic storm is linked to it. However, the flare and the tsunami accelerated protons that hit the Earth's magnetosphere and caused a minor radiation storm. The enhancement of proton events is revealed by the radio blackout that cover the whole African continent (<uri>https://spaceweather.com/images2022/28mar22/blackout.jpg</uri>, last access: 15 February 2024) and the polar cap absorption event (PCAE) that occurred after about 02:40 UT from the burst onset (<uri>https://spaceweather.com/images2022/28mar22/pca.jpg</uri>, last access: 15 February 2024). This event is a signature of the solar proton enhancement where the high frequency (HF) and very high frequency (VHF) are absorbed while low and very low frequencies are reflected at a low altitude. Previous works showed that solar flares that cause solar energetic particles (SEPs) are usually accompanied by radio bursts and noise storms that disturb the ionospheric TEC <xref ref-type="bibr" rid="bib1.bibx77" id="paren.77"/> and mostly observed 20 min to 20 h after the solar flare <xref ref-type="bibr" rid="bib1.bibx62 bib1.bibx39 bib1.bibx73" id="paren.78"/>. They also showed that SEPs and PCAEs are frequently close to the maximum solar cycle <xref ref-type="bibr" rid="bib1.bibx89" id="paren.79"/>, but the solar cycle 25 is far from its maximum. Thus, these observations are the evidence of high solar activity during the ascending phase of the current sunspot cycle. It is important to note that the association of type II radio bursts with space weather drivers such as solar flares, SEPs and coronal mass ejections make them special for space weather <xref ref-type="bibr" rid="bib1.bibx47 bib1.bibx64" id="paren.80"/>. Figure <xref ref-type="fig" rid="Ch1.F10"/> presents the ionospheric irregularities using ROTI in response to the solar flare of 28 March 2022.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F10" specific-use="star"><?xmltex \currentcnt{10}?><?xmltex \def\figurename{Figure}?><label>Figure 10</label><caption><p id="d1e5133">ROTI variability in the <bold>(a)</bold> high-latitude region, <bold>(b)</bold> mid-latitude region, <bold>(c)</bold> equatorial region and <bold>(d)</bold> associated GOES soft X-ray M4.0 flare.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f10.png"/>

          </fig>

      <p id="d1e5154">Figure <xref ref-type="fig" rid="Ch1.F10"/>a reveals strong TEC abnormalities (ROTI <inline-formula><mml:math id="M158" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M159" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) at the M4.0 flare intensity peak. In response to the M4.0 flare, no TEC anomalies are seen in the mid-latitude and equatorial regions (Fig. <xref ref-type="fig" rid="Ch1.F10"/>b–c). Furthermore, the suppression of ROTI in the mid-latitude zone is related to the significant SEP, which began about 13:00 UT, as shown in Fig. <xref ref-type="fig" rid="Ch1.F11"/>.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F11" specific-use="star"><?xmltex \currentcnt{11}?><?xmltex \def\figurename{Figure}?><label>Figure 11</label><caption><p id="d1e5187">Major SEPs in five energy levels that occurred on 28 March 2022.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f11.png"/>

          </fig>

      <p id="d1e5196">This figure shows two peaks in particle intensities at 15:50 and 17:11 UT, respectively. It also indicates a decline in the minimum particle intensity at 16:55 UT. The mid-latitude region above India has an ionospheric irregularity as a result of SEP. As ROTI <inline-formula><mml:math id="M160" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn></mml:mrow></mml:math></inline-formula> TECU min<inline-formula><mml:math id="M161" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> indicates, the equatorial region (Mbarara station) was impacted by the intensification of the SEP during the ascent towards the second peak.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F12" specific-use="star"><?xmltex \currentcnt{12}?><?xmltex \def\figurename{Figure}?><label>Figure 12</label><caption><p id="d1e5223">Daily variation in the ionospheric TEC in terms of ROTI <bold>(a)</bold> in the high-latitude zone <bold>(b)</bold>, in the mid-latitude region and <bold>(c)</bold> in equatorial region with the <bold>(d)</bold> associated GOES soft X-ray flare.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f12.png"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F13" specific-use="star"><?xmltex \currentcnt{13}?><?xmltex \def\figurename{Figure}?><label>Figure 13</label><caption><p id="d1e5247">Daily variation in the ionospheric TEC in terms of ROTI <bold>(a)</bold> in the high-latitude zone, <bold>(b)</bold> in the mid-latitude region, <bold>(c)</bold> in the equatorial region and <bold>(d)</bold> accompanying GOES soft X-ray flare.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://angeo.copernicus.org/articles/42/313/2024/angeo-42-313-2024-f13.png"/>

          </fig>

</sec>
<sec id="Ch1.S3.SS2.SSS3">
  <label>3.2.3</label><title>31 March 2022 event</title>
      <p id="d1e5276">The type II radio burst observed by <inline-formula><mml:math id="M162" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO network at Arecibo Observatory in Puerto Rico, USA, from 18:33 to 18:37 UT on 31 March 2022 with the 76–34 MHz frequency range is overlapped by a type IV radio burst that occurred from 18:36 to 18:41 UT. These bursts are associated with GOES soft X-ray flare M9.6 that started at 18:17 UT, peaked at 18:35 UT and stopped at 18:45 UT from NOAA 12975. These events are associated with halo CME (19:12 UT) with speed of 489 km s<inline-formula><mml:math id="M163" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and caused a minor storm on 2 April 2022. A major SEP is also seen on this day, beginning at 03:35 UT and peaking at 04:36 UT. It is outside of the burst time range, and no other bursts were reported to correspond with the SEP (see <uri>https://cdaw.gsfc.nasa.gov/CME_list/daily_plots/sephtx/2022_03/sephtx_20220331.png</uri>, last access: 16 February 2024). This SEP is assumed to be caused by the CIRs <xref ref-type="bibr" rid="bib1.bibx60 bib1.bibx100 bib1.bibx79 bib1.bibx97" id="paren.81"/> with no GOES soft X-ray flare connected with it. Figure <xref ref-type="fig" rid="Ch1.F12"/> displays<?pagebreak page323?> the daily fluctuation in the ionospheric TEC in terms of ROTI over (Fig. <xref ref-type="fig" rid="Ch1.F12"/>a) high-latitude (INVK), (Fig. <xref ref-type="fig" rid="Ch1.F12"/>b) mid-latitude area (IISC), (Fig. <xref ref-type="fig" rid="Ch1.F12"/>c) equatorial region (MBAR), and the associated GOES soft X-ray flare flux profile (Fig. <xref ref-type="fig" rid="Ch1.F12"/>d).</p>
      <p id="d1e5315">The significant anomalies in high latitudes are thought to be caused by SEP intensification (Fig. <xref ref-type="fig" rid="Ch1.F12"/>a). However, no notable anomalies have been seen in the mid- and equatorial areas as a result of the SEP event. Furthermore, there were no anomalies in any of the locations caused by the M9.6 solar flare. This is believed to be due to electrodynamic coupling of the ionosphere–magnetosphere <xref ref-type="bibr" rid="bib1.bibx52 bib1.bibx51" id="paren.82"/>.</p>
</sec>
<?pagebreak page324?><sec id="Ch1.S3.SS2.SSS4">
  <label>3.2.4</label><title>2 April 2022 event</title>
      <p id="d1e5331">The month of April 2022 is also characterized by intense solar activity. On 2 April 2022 between 13:24 and 13:31 UT, a type II radio emission is registered within the 86–30 MHz frequency range followed by a type IV radio emission from 13:28 to 13:35 UT. They are associated with a GOES soft X-ray flare M3.9 that started at 12:56 UT, peaked at 13:55 UT and stopped at 14:44 UT from NOAA 12975. Within the time interval, the SEP takes place at 14:21 UT and peaks at 15:41 UT. Figure <xref ref-type="fig" rid="Ch1.F13"/> illustrates the variability in the ionospheric TEC in response to the GOES soft X-ray flare and SEP simultaneously over different regions of the globe (Fig. <xref ref-type="fig" rid="Ch1.F13"/>a–c).</p>
      <p id="d1e5338">Figure <xref ref-type="fig" rid="Ch1.F13"/> clearly shows no significant ionospheric TEC variation caused by the development of the M3.9 flare, as well as from the occurrence of SEP in this time frame over all regions (Fig. <xref ref-type="fig" rid="Ch1.F13"/>a–c). It should be noted that the particles that are not deflected by the magnetosphere become trapped in the Earth's magnetic field <xref ref-type="bibr" rid="bib1.bibx71" id="paren.83"/>. Another M4.3 solar flare erupted from the same active region (AR12975) at 17:34 UT, peaked at 17:44 UT, and ended at 17:51 UT. The <inline-formula><mml:math id="M164" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO has not detected any radio events and neither has been reported by the Space Weather Prediction Centre (SWPC). According to Fig. <xref ref-type="fig" rid="Ch1.F13"/>, substantial fluctuation in the ROTI in the high-latitude region (BAKE) began before the second solar flare and is thought to be manifested by the SEP interaction with the magnetosphere. However, the irregularity in ROTI began near the peak of the second flare in mid-latitude (Fig. <xref ref-type="fig" rid="Ch1.F13"/>b), and it is assumed to be a response to that flare. The equatorial region is unaffected by the three occurrences (Fig. <xref ref-type="fig" rid="Ch1.F13"/>c). Using the instance scenarios above, it is vital to note that the solar flare lasts between 15 min and 2 h, resulting in continuous ionization throughout the event <xref ref-type="bibr" rid="bib1.bibx97" id="paren.84"/>. Furthermore, the SEPs come quickly after the flare, depending on the  particle's kinetic energy, pitch angle and magnetic connectivity <xref ref-type="bibr" rid="bib1.bibx36 bib1.bibx97" id="paren.85"/>.</p>
</sec>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <label>4</label><title>Conclusions</title>
      <p id="d1e5378">In this study, we report on an analysis of 32 well-separated type II radio bursts observed by <inline-formula><mml:math id="M165" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO network from May 2021 to December 2022. The parameters of type II radio bursts, such as bandwidth, drift rates and starting frequency are used to derive the corresponding shock parameters: the shock speed, Alfvén speed, Mach number and magnetic field strength. The shock and Alfvén speeds are estimated in the range of 504–1282 and 368–826 km<inline-formula><mml:math id="M166" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, respectively, at heliocentric distance <inline-formula><mml:math id="M167" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M168" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. The range of measurements is consistent with the earlier works, including the Alfvén speed with 550–400 km<inline-formula><mml:math id="M169" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> given in <xref ref-type="bibr" rid="bib1.bibx16" id="text.86"/> at <inline-formula><mml:math id="M170" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.6</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M171" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.1</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. The Alfvén speed of the order of 140 to 460 km<inline-formula><mml:math id="M172" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> at heliocentric distance <inline-formula><mml:math id="M173" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.2</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M174" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.5</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> is reported in <xref ref-type="bibr" rid="bib1.bibx25" id="text.87"/>, while <xref ref-type="bibr" rid="bib1.bibx40" id="text.88"/> inferred Alfvén speed in the range of  259–982 km<inline-formula><mml:math id="M175" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> is over 3–15 <inline-formula><mml:math id="M176" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula>. The shock speed estimated agrees well with the works of <xref ref-type="bibr" rid="bib1.bibx18" id="text.89"/> and <xref ref-type="bibr" rid="bib1.bibx61" id="text.90"/>, who found shock speed of the order of 200 to 810 km<inline-formula><mml:math id="M177" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>. Using the Rankine–Hugoniot approximation, the Mach number of the order of  1.1 to 1.8 is obtained and the magnetic field strength in the range of <inline-formula><mml:math id="M178" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">7.8</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M179" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.7</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula>, which is fitted with a single power law <inline-formula><mml:math id="M180" display="inline"><mml:mrow><mml:mi>B</mml:mi><mml:mo>(</mml:mo><mml:mi>r</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mn mathvariant="normal">6.07</mml:mn><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3.96</mml:mn></mml:mrow></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula> at the same heliocentric distance. The range of the Mach number is in good agreement with the range of Mach number of <inline-formula><mml:math id="M181" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.59</mml:mn><mml:mo>&lt;</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">2.53</mml:mn></mml:mrow></mml:math></inline-formula> reported by <xref ref-type="bibr" rid="bib1.bibx59" id="text.91"/> and <inline-formula><mml:math id="M182" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mi mathvariant="normal">A</mml:mi></mml:msub><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">1.5</mml:mn></mml:mrow></mml:math></inline-formula> by <xref ref-type="bibr" rid="bib1.bibx93" id="text.92"/>. Our magnetic field strength estimate of the order <inline-formula><mml:math id="M183" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">7.8</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M184" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.7</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula> at <inline-formula><mml:math id="M185" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M186" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mspace linebreak="nobreak" width="0.25em"/><mml:msub><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> is well consistent with the work of <xref ref-type="bibr" rid="bib1.bibx106" id="text.93"/>, who reported the magnetic field strength of 1–8 G at <inline-formula><mml:math id="M187" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.6</mml:mn><mml:mspace linebreak="nobreak" width="0.25em"/><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:mrow></mml:math></inline-formula> and also with 6–5 G at <inline-formula><mml:math id="M188" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1.5</mml:mn></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M189" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.7</mml:mn><mml:mspace width="0.25em" linebreak="nobreak"/><mml:mi>R</mml:mi><mml:mo>⊙</mml:mo></mml:mrow></mml:math></inline-formula>, as found in <xref ref-type="bibr" rid="bib1.bibx76" id="text.94"/>. According to the current research, 19 of the 32 type II radio events are precursors for space weather because they are connected to immediate space weather phenomena like radio blackouts and polar cap absorption events, exhibit band-splitting characteristics or are followed by type III and IV bursts. The current study's findings also reveal that ionospheric disturbances are common depending on the strength of flare classes and/or SEPs, as evidenced by ROTI irregularities, and solar radio type II observations are used as indicators in this situation. This article demonstrates that because type II bursts are connected to space weather hazards, understanding various physical properties of type II bursts aids in the prediction and forecast of space weather.</p>
</sec>

      
      </body>
    <back><notes notes-type="codeavailability"><title>Code availability</title>

      <p id="d1e5735">Code for processing dynamic spectra are available on the <inline-formula><mml:math id="M190" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO website. The code for ROTI computation are accessible at <uri>https://www.mathworks.com/matlabcentral/fileexchange/129239-programs-to-compute-rot-and-roti</uri> <xref ref-type="bibr" rid="bib1.bibx69" id="paren.95"/>.</p>
  </notes><notes notes-type="dataavailability"><title>Data availability</title>

      <p id="d1e5754">The authors also thank the providers of all the data used from SOHO/LASCO, NOAA, GOES, SWPC, the African Geodetic Reference Frame (<uri>http://afrefdata.org</uri>, <xref ref-type="bibr" rid="bib1.bibx1" id="altparen.96"/>), Solar Monitor (<uri>https://solarmonitor.org/</uri>, <xref ref-type="bibr" rid="bib1.bibx92" id="altparen.97"/>), Coordinated Data Analysis Web (<uri>https://cdaweb.gsfc.nasa.gov/</uri>, <xref ref-type="bibr" rid="bib1.bibx63" id="altparen.98"/>) and the UNAVCO Archive of GNSS Data (<uri>https://www.unavco.org/</uri>, <xref ref-type="bibr" rid="bib1.bibx23" id="altparen.99"/>).</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d1e5785">TN, JU, JCU and DIO conceived the presented idea and the design of the study. TN manually gathered the data used. CM and DIO helped with the programming for the data analysis. Analysis and interpretation of the results were done by TN, who later drafted the paper. This article has been reviewed by JU, JCU, ABR, DIO, KSR and CK.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <?pagebreak page325?><p id="d1e5791">The contact author has declared that none of the authors has any competing interests.</p>
  </notes><notes notes-type="disclaimer"><title>Disclaimer</title>

      <p id="d1e5797">Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e5803">This work has been supported by International Science Programme (ISP) through Rwanda Astrophysics, Space and Climate Science Research Group (RASCSRG) and Centre for atmospheric Research through National Space Research and Development Agency, Abuja, Nigeria. The authors thank FHNW, Institute for Data Science in Brugg/Windisch, Switzerland, for hosting the <inline-formula><mml:math id="M191" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>-CALLISTO network and the individual CALLISTO operators such as the Geophysical Institute at the University of Alaska Fairbanks, Arecibo Observatory and the Astronomical Society of South Australia.  Finally, the authors would like to thank the anonymous referees for their useful comments and suggestions during the review of this paper.</p></ack><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d1e5815">This paper was edited by Margit Haberreiter and reviewed by two anonymous referees.</p>
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