Articles | Volume 39, issue 4
https://doi.org/10.5194/angeo-39-641-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/angeo-39-641-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Regular paper
| 
12 Jul 2021
Regular paper |
| 12 Jul 2021
| 12 Jul 2021
Role of eddy diffusion in the delayed ionospheric response to solar flux changes
Rajesh Vaishnav
CORRESPONDING AUTHOR
Leipzig Institute for Meteorology, Universität Leipzig, Stephanstr. 3, 04103 Leipzig, Germany
Christoph Jacobi
Leipzig Institute for Meteorology, Universität Leipzig, Stephanstr. 3, 04103 Leipzig, Germany
Jens Berdermann
German Aerospace Center, Kalkhorstweg 53, 17235 Neustrelitz, Germany
Mihail Codrescu
Space Weather Prediction Centre, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA
Erik Schmölter
German Aerospace Center, Kalkhorstweg 53, 17235 Neustrelitz, Germany
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Rajesh Vaishnav, Erik Schmölter, Christoph Jacobi, Jens Berdermann, and Mihail Codrescu
Ann. Geophys., 39, 341–355, https://doi.org/10.5194/angeo-39-341-2021, https://doi.org/10.5194/angeo-39-341-2021, 2021
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We investigate the delayed ionospheric response using the observed and CTIPe-model-simulated TEC against the solar EUV flux. The ionospheric delay estimated using model-simulated TEC is in good agreement with the delay estimated for observed TEC. The study confirms the model's capabilities to reproduce the delayed ionospheric response against the solar EUV flux. Results also indicate that the average delay is higher in the Northern Hemisphere as compared to the Southern Hemisphere.
Rajesh Vaishnav, Christoph Jacobi, and Jens Berdermann
Ann. Geophys., 37, 1141–1159, https://doi.org/10.5194/angeo-37-1141-2019, https://doi.org/10.5194/angeo-37-1141-2019, 2019
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We investigate the ionospheric response to the temporal and spatial dynamics of the solar activity using total electron content (TEC) maps and multiple solar proxies. The maximum correlation at a 16–32-d timescale is observed between the He-II, Mg-II, and F30 with respect to global mean TEC, with an effective time delay of about 1 d. The most suitable proxy to represent the solar activity at the timescales of 16–32 d and 32–64 d is He-II.
Erik Schmölter, Jens Berdermann, Norbert Jakowski, Christoph Jacobi, and Rajesh Vaishnav
Adv. Radio Sci., 16, 149–155, https://doi.org/10.5194/ars-16-149-2018, https://doi.org/10.5194/ars-16-149-2018, 2018
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Physical and chemical processes in the ionosphere are driven by complex interactions with the solar radiation. The ionospheric plasma is in particular sensitive to solar variations with a time delay between one and two days.
Here we present preliminary results of the ionospheric delay based on a comprehensive and reliable database consisting of GNSS TEC Maps and EUV spectral flux data.
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Adv. Radio Sci., 16, 157–165, https://doi.org/10.5194/ars-16-157-2018, https://doi.org/10.5194/ars-16-157-2018, 2018
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We investigate the ionospheric response to solar Extreme Ultraviolet (EUV) variations using different solar proxies and IGS TEC maps. An ionospheric delay in GTEC is observed at the 27 days solar rotation period with the time scale of about ~ 1–2 days. Here we present preliminary results from the CTIPe model simulations which qualitatively reproduce the observed ~1-2 days delay in GTEC, which is might be due to vertical transport processes.
Sina Mehrdad, Dörthe Handorf, Ines Höschel, Khalil Karami, Johannes Quaas, Sudhakar Dipu, and Christoph Jacobi
Weather Clim. Dynam., 5, 1223–1268, https://doi.org/10.5194/wcd-5-1223-2024, https://doi.org/10.5194/wcd-5-1223-2024, 2024
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This study introduces a novel deep learning (DL) approach to analyze how regional radiative forcing in Europe impacts the Arctic climate. By integrating atmospheric poleward energy transport with DL-based clustering of atmospheric patterns and attributing anomalies to specific clusters, our method reveals crucial, nuanced interactions within the climate system, enhancing our understanding of intricate climate dynamics.
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Ann. Geophys. Discuss., https://doi.org/10.5194/angeo-2024-13, https://doi.org/10.5194/angeo-2024-13, 2024
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Ales Kuchar, Maurice Öhlert, Roland Eichinger, and Christoph Jacobi
Weather Clim. Dynam., 5, 895–912, https://doi.org/10.5194/wcd-5-895-2024, https://doi.org/10.5194/wcd-5-895-2024, 2024
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Gunter Stober, Sharon L. Vadas, Erich Becker, Alan Liu, Alexander Kozlovsky, Diego Janches, Zishun Qiao, Witali Krochin, Guochun Shi, Wen Yi, Jie Zeng, Peter Brown, Denis Vida, Neil Hindley, Christoph Jacobi, Damian Murphy, Ricardo Buriti, Vania Andrioli, Paulo Batista, John Marino, Scott Palo, Denise Thorsen, Masaki Tsutsumi, Njål Gulbrandsen, Satonori Nozawa, Mark Lester, Kathrin Baumgarten, Johan Kero, Evgenia Belova, Nicholas Mitchell, Tracy Moffat-Griffin, and Na Li
Atmos. Chem. Phys., 24, 4851–4873, https://doi.org/10.5194/acp-24-4851-2024, https://doi.org/10.5194/acp-24-4851-2024, 2024
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On 15 January 2022, the Hunga Tonga-Hunga Ha‘apai volcano exploded in a vigorous eruption, causing many atmospheric phenomena reaching from the surface up to space. In this study, we investigate how the mesospheric winds were affected by the volcanogenic gravity waves and estimated their propagation direction and speed. The interplay between model and observations permits us to gain new insights into the vertical coupling through atmospheric gravity waves.
Christoph Jacobi, Ales Kuchar, Toralf Renkwitz, and Juliana Jaen
Adv. Radio Sci., 21, 111–121, https://doi.org/10.5194/ars-21-111-2023, https://doi.org/10.5194/ars-21-111-2023, 2023
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Middle atmosphere long-term changes show the signature of climate change. We analyse 43 years of mesopause region horizontal winds obtained at two sites in Germany. We observe mainly positive trends of the zonal prevailing wind throughout the year, while the meridional winds tend to decrease in magnitude in both summer and winter. Furthermore, there is a change in long-term trends around the late 1990s, which is most clearly visible in summer winds.
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Atmos. Chem. Phys., 23, 14871–14887, https://doi.org/10.5194/acp-23-14871-2023, https://doi.org/10.5194/acp-23-14871-2023, 2023
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Investigation of winds is important to understand atmospheric dynamics. In the summer mesosphere and lower thermosphere, there are three main wind flows: the mesospheric westward, the mesopause southward (equatorward), and the lower-thermospheric eastward wind. Combining almost 2 decades of measurements from different radars, we study the trend, their interannual oscillations, and the effects of the geomagnetic activity over these wind maxima.
Olivia Linke, Johannes Quaas, Finja Baumer, Sebastian Becker, Jan Chylik, Sandro Dahlke, André Ehrlich, Dörthe Handorf, Christoph Jacobi, Heike Kalesse-Los, Luca Lelli, Sina Mehrdad, Roel A. J. Neggers, Johannes Riebold, Pablo Saavedra Garfias, Niklas Schnierstein, Matthew D. Shupe, Chris Smith, Gunnar Spreen, Baptiste Verneuil, Kameswara S. Vinjamuri, Marco Vountas, and Manfred Wendisch
Atmos. Chem. Phys., 23, 9963–9992, https://doi.org/10.5194/acp-23-9963-2023, https://doi.org/10.5194/acp-23-9963-2023, 2023
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Lapse rate feedback (LRF) is a major driver of the Arctic amplification (AA) of climate change. It arises because the warming is stronger at the surface than aloft. Several processes can affect the LRF in the Arctic, such as the omnipresent temperature inversion. Here, we compare multimodel climate simulations to Arctic-based observations from a large research consortium to broaden our understanding of these processes, find synergy among them, and constrain the Arctic LRF and AA.
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Adv. Radio Sci., 20, 85–92, https://doi.org/10.5194/ars-20-85-2023, https://doi.org/10.5194/ars-20-85-2023, 2023
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Sporadic E (Es) layers are thin regions of accumulated ions in the lower ionosphere. They can be observed by disturbances of GNSS links between low-Earth orbiting satellites and GNSS satellites. Es layers are influenced by neutral atmospheric tides and show the coupling between the neutral atmosphere and the ionosphere. Here we analyse migrating (sun-synchronous) and non-migrating tidal components in Es. The main signatures are migrating Es, but nonmigrating components are found as well.
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The instrument records annual changes in Spectral Outgoing Radiation from 200–1100 nm, with 60 photomultiplier tubes simultaneously providing spectrometer and photometer data. Using Total Solar Irradiance data with a stability of 0.01 Wm-2 per year to recalibrate the established instruments, stable data of ~0.1 Wm-2 over a solar cycle period is expected. Determination of the changes in the global green Earth coverage and mapping will also assess the impact of climate engineering actions.
Gunter Stober, Alan Liu, Alexander Kozlovsky, Zishun Qiao, Ales Kuchar, Christoph Jacobi, Chris Meek, Diego Janches, Guiping Liu, Masaki Tsutsumi, Njål Gulbrandsen, Satonori Nozawa, Mark Lester, Evgenia Belova, Johan Kero, and Nicholas Mitchell
Atmos. Meas. Tech., 15, 5769–5792, https://doi.org/10.5194/amt-15-5769-2022, https://doi.org/10.5194/amt-15-5769-2022, 2022
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Precise and accurate measurements of vertical winds at the mesosphere and lower thermosphere are rare. Although meteor radars have been used for decades to observe horizontal winds, their ability to derive reliable vertical wind measurements was always questioned. In this article, we provide mathematical concepts to retrieve mathematically and physically consistent solutions, which are compared to the state-of-the-art non-hydrostatic model UA-ICON.
Ales Kuchar, Petr Sacha, Roland Eichinger, Christoph Jacobi, Petr Pisoft, and Harald Rieder
EGUsphere, https://doi.org/10.5194/egusphere-2022-474, https://doi.org/10.5194/egusphere-2022-474, 2022
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We focus on the impact of small-scale orographic gravity waves (OGWs) above the Himalayas. The interaction of GWs with the large-scale circulation in the stratosphere is not still well understood and can have implications on climate projections. We use a chemistry-climate model to show that these strong OGW events are associated with anomalously increased upward planetary-scale waves and in turn affect the circumpolar circulation and have the potential to alter ozone variability as well.
Sumanta Sarkhel, Gunter Stober, Jorge L. Chau, Steven M. Smith, Christoph Jacobi, Subarna Mondal, Martin G. Mlynczak, and James M. Russell III
Ann. Geophys., 40, 179–190, https://doi.org/10.5194/angeo-40-179-2022, https://doi.org/10.5194/angeo-40-179-2022, 2022
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A rare gravity wave event was observed on the night of 25 April 2017 over northern Germany. An all-sky airglow imager recorded an upward-propagating wave at different altitudes in mesosphere with a prominent wave front above 91 km and faintly observed below. Based on wind and satellite-borne temperature profiles close to the event location, we have found the presence of a leaky thermal duct layer in 85–91 km. The appearance of this duct layer caused the wave amplitudes to diminish below 91 km.
Juliana Jaen, Toralf Renkwitz, Jorge L. Chau, Maosheng He, Peter Hoffmann, Yosuke Yamazaki, Christoph Jacobi, Masaki Tsutsumi, Vivien Matthias, and Chris Hall
Ann. Geophys., 40, 23–35, https://doi.org/10.5194/angeo-40-23-2022, https://doi.org/10.5194/angeo-40-23-2022, 2022
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To study long-term trends in the mesosphere and lower thermosphere (70–100 km), we established two summer length definitions and analyzed the variability over the years (2004–2020). After the analysis, we found significant trends in the summer beginning of one definition. Furthermore, we were able to extend one of the time series up to 31 years and obtained evidence of non-uniform trends and periodicities similar to those known for the quasi-biennial oscillation and El Niño–Southern Oscillation.
Christoph Jacobi, Friederike Lilienthal, Dmitry Korotyshkin, Evgeny Merzlyakov, and Gunter Stober
Adv. Radio Sci., 19, 185–193, https://doi.org/10.5194/ars-19-185-2021, https://doi.org/10.5194/ars-19-185-2021, 2021
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We compare winds and tidal amplitudes in the upper mesosphere/lower thermosphere region for cases with disturbed and undisturbed geomagnetic conditions. The zonal winds in both the mesosphere and lower thermosphere tend to be weaker during disturbed conditions. The summer equatorward meridional wind jet is weaker for disturbed geomagnetic conditions. The effect of geomagnetic variability on tidal amplitudes, except for the semidiurnal tide, is relatively small.
Gunter Stober, Ales Kuchar, Dimitry Pokhotelov, Huixin Liu, Han-Li Liu, Hauke Schmidt, Christoph Jacobi, Kathrin Baumgarten, Peter Brown, Diego Janches, Damian Murphy, Alexander Kozlovsky, Mark Lester, Evgenia Belova, Johan Kero, and Nicholas Mitchell
Atmos. Chem. Phys., 21, 13855–13902, https://doi.org/10.5194/acp-21-13855-2021, https://doi.org/10.5194/acp-21-13855-2021, 2021
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Little is known about the climate change of wind systems in the mesosphere and lower thermosphere at the edge of space at altitudes from 70–110 km. Meteor radars represent a well-accepted remote sensing technique to measure winds at these altitudes. Here we present a state-of-the-art climatological interhemispheric comparison using continuous and long-lasting observations from worldwide distributed meteor radars from the Arctic to the Antarctic and sophisticated general circulation models.
Rajesh Vaishnav, Erik Schmölter, Christoph Jacobi, Jens Berdermann, and Mihail Codrescu
Ann. Geophys., 39, 341–355, https://doi.org/10.5194/angeo-39-341-2021, https://doi.org/10.5194/angeo-39-341-2021, 2021
Short summary
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We investigate the delayed ionospheric response using the observed and CTIPe-model-simulated TEC against the solar EUV flux. The ionospheric delay estimated using model-simulated TEC is in good agreement with the delay estimated for observed TEC. The study confirms the model's capabilities to reproduce the delayed ionospheric response against the solar EUV flux. Results also indicate that the average delay is higher in the Northern Hemisphere as compared to the Southern Hemisphere.
Harikrishnan Charuvil Asokan, Jorge L. Chau, Raffaele Marino, Juha Vierinen, Fabio Vargas, Juan Miguel Urco, Matthias Clahsen, and Christoph Jacobi
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2020-974, https://doi.org/10.5194/acp-2020-974, 2020
Preprint withdrawn
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This paper explores the dynamics of gravity waves and turbulence present in the mesosphere and lower thermosphere (MLT) region. We utilized two different techniques on meteor radar observations and simulations to obtain power spectra at different horizontal scales. The techniques are applied to a special campaign conducted in northern Germany in November 2018. The study revealed the dominance of large-scale structures with horizontal scales larger than 500 km during the campaign period.
Ales Kuchar, Petr Sacha, Roland Eichinger, Christoph Jacobi, Petr Pisoft, and Harald E. Rieder
Weather Clim. Dynam., 1, 481–495, https://doi.org/10.5194/wcd-1-481-2020, https://doi.org/10.5194/wcd-1-481-2020, 2020
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Our study focuses on the impact of topographic structures such as the Himalayas and Rocky Mountains, so-called orographic gravity-wave hotspots. These hotspots play an important role in the dynamics of the middle atmosphere, in particular in the lower stratosphere. We study intermittency and zonally asymmetric character of these hotspots and their effects on the upper stratosphere and mesosphere using a new detection method in various modeling and observational datasets.
Christoph Geißler, Christoph Jacobi, and Friederike Lilienthal
Ann. Geophys., 38, 527–544, https://doi.org/10.5194/angeo-38-527-2020, https://doi.org/10.5194/angeo-38-527-2020, 2020
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This is an extensive model study to analyze the migrating quarterdiurnal solar tide (QDT) and its forcing mechanisms in the middle atmosphere. We first show a climatology of the QDT amplitudes and examine the contribution of the different forcing mechanisms, including direct solar, nonlinear and gravity wave forcing, on the QDT amplitude. We then investigate the destructive interference between the individual forcing mechanisms.
Friederike Lilienthal, Erdal Yiğit, Nadja Samtleben, and Christoph Jacobi
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2019-339, https://doi.org/10.5194/gmd-2019-339, 2020
Preprint withdrawn
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Gravity waves are a small-scale but prominent dynamical feature in the Earth's atmosphere. Here, we use a mechanistic nonlinear general circulation model and implement a modern whole atmosphere gravity wave parameterization. We study the response of the atmosphere on several phase speed spectra. We find a large influence of fast travelling waves on the background dynamics in the thermosphere and also a strong dependence of the amplitude of the terdiurnal solar tide, indicating wave interactions.
Erik Schmölter, Jens Berdermann, Norbert Jakowski, and Christoph Jacobi
Ann. Geophys., 38, 149–162, https://doi.org/10.5194/angeo-38-149-2020, https://doi.org/10.5194/angeo-38-149-2020, 2020
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This study correlates ionospheric parameters with the integrated solar radiation for an analysis of the delayed ionospheric response in order to confirm previous studies on the delay and to further specify variations of the delay (seasonal and spatial). Results also indicate the dependence on the geomagnetic activity as well as on the 11-year solar cycle. The results are important for the understanding of ionospheric processes and could be used for the validation of ionospheric models.
Nadja Samtleben, Aleš Kuchař, Petr Šácha, Petr Pišoft, and Christoph Jacobi
Ann. Geophys., 38, 95–108, https://doi.org/10.5194/angeo-38-95-2020, https://doi.org/10.5194/angeo-38-95-2020, 2020
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The additional transfer of momentum and energy induced by locally breaking gravity wave hotspots in the lower stratosphere may lead to a destabilization of the polar vortex, which is strongly dependent on the position of the hotspot. The simulations with a global circulation model show that hotspots located above Eurasia cause a total decrease in the stationary planetary wave (SPW) activity, while the impact of hotspots located in North America mostly increase the SPW activity.
Rajesh Vaishnav, Christoph Jacobi, and Jens Berdermann
Ann. Geophys., 37, 1141–1159, https://doi.org/10.5194/angeo-37-1141-2019, https://doi.org/10.5194/angeo-37-1141-2019, 2019
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We investigate the ionospheric response to the temporal and spatial dynamics of the solar activity using total electron content (TEC) maps and multiple solar proxies. The maximum correlation at a 16–32-d timescale is observed between the He-II, Mg-II, and F30 with respect to global mean TEC, with an effective time delay of about 1 d. The most suitable proxy to represent the solar activity at the timescales of 16–32 d and 32–64 d is He-II.
Friederike Lilienthal and Christoph Jacobi
Ann. Geophys., 37, 943–953, https://doi.org/10.5194/angeo-37-943-2019, https://doi.org/10.5194/angeo-37-943-2019, 2019
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We analyzed the forcing mechanisms of the migrating terdiurnal solar tide in the middle atmosphere, focusing the impact on the zonal mean circulation. We show that the primary solar forcing is the most dominant one but secondary wave–wave interactions also contribute in the lower thermosphere region. We further demonstrate that small-scale gravity waves can strongly and irregularly influence the amplitude of the terdiurnal tide as well as the background circulation in the thermosphere.
Christoph Jacobi and Christina Arras
Adv. Radio Sci., 17, 213–224, https://doi.org/10.5194/ars-17-213-2019, https://doi.org/10.5194/ars-17-213-2019, 2019
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We analyze tidal phases and related wind shear in the mesosphere and
lower thermosphere as observed by a meteor radar. The wind shear phases are compared with those of sporadic E occurrence rates, which were derived from GPS radio occultation observations. We find good correspondence between radar derived wind shear and sporadic E phases for the semidiurnal, terdiurnal, and quarterdiurnal tidal components, but not for the diurnal tide.
Nadja Samtleben, Christoph Jacobi, Petr Pišoft, Petr Šácha, and Aleš Kuchař
Ann. Geophys., 37, 507–523, https://doi.org/10.5194/angeo-37-507-2019, https://doi.org/10.5194/angeo-37-507-2019, 2019
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Simulations of locally breaking gravity wave hot spots in the stratosphere show a suppression of wave propagation at midlatitudes, which is partly compensated for by additional wave propagation through the polar region. This leads to a displacement of the polar vortex towards lower latitudes. The effect is highly dependent on the position of the artificial gravity wave forcing. It is strongest (weakest) for hot spots at lower to middle latitudes (higher latitudes).
Christoph Jacobi, Christina Arras, Christoph Geißler, and Friederike Lilienthal
Ann. Geophys., 37, 273–288, https://doi.org/10.5194/angeo-37-273-2019, https://doi.org/10.5194/angeo-37-273-2019, 2019
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Sporadic E (Es) layers in the Earth's ionosphere are produced by ion convergence due to vertical wind shear in the presence of a horizontal component of the Earth's magnetic field. We present analyses of the 6 h tidal signatures in ES occurrence rates derived from GPS radio observations. Times of maxima in ES agree well with those of negative wind shear obtained from radar observation. The global distribution of ES amplitudes agrees with wind shear amplitudes from numerical modeling.
Daniel Mewes and Christoph Jacobi
Atmos. Chem. Phys., 19, 3927–3937, https://doi.org/10.5194/acp-19-3927-2019, https://doi.org/10.5194/acp-19-3927-2019, 2019
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Horizontal moist static energy (MSE) transport patterns were extracted from reanalysis data using an artificial neuronal network for the winter months. The results show that during the last 30 years transport pathways that favour MSE transport through the North Atlantic are getting more frequent. This North Atlantic pathway is connected to positive temperature anomalies over the central Arctic, which implies a connection between Arctic amplification and the change in horizontal heat transport.
Sven Wilhelm, Gunter Stober, Vivien Matthias, Christoph Jacobi, and Damian J. Murphy
Ann. Geophys., 37, 1–14, https://doi.org/10.5194/angeo-37-1-2019, https://doi.org/10.5194/angeo-37-1-2019, 2019
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This study shows that the mesospheric winds are affected by an expansion–shrinking of the mesosphere and lower thermosphere that takes place due to changes in the intensity of the solar radiation, which affects the density within the atmosphere. On seasonal timescales, an increase in the neutral density occurs together with a decrease in the eastward-directed zonal wind. Further, even after removing the seasonal and the 11-year solar cycle variations, we show a connection between them.
Friederike Lilienthal, Christoph Jacobi, and Christoph Geißler
Atmos. Chem. Phys., 18, 15725–15742, https://doi.org/10.5194/acp-18-15725-2018, https://doi.org/10.5194/acp-18-15725-2018, 2018
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The terdiurnal solar tide is an atmospheric wave, owing to the daily variation of solar heating with a period of 8 h. Here, we present model simulations of this tide and investigate the relative importance of possible forcing mechanisms because they are still under debate. These are, besides direct solar heating, nonlinear interactions between other tides and gravity wave–tide interactions. As a result, solar heating is most important and nonlinear effects partly counteract this forcing.
Christoph Jacobi, Christoph Geißler, Friederike Lilienthal, and Amelie Krug
Adv. Radio Sci., 16, 141–147, https://doi.org/10.5194/ars-16-141-2018, https://doi.org/10.5194/ars-16-141-2018, 2018
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The possible sources of the quarterdiurnal tide (QDT) in the middle atmosphere are still under discussion. Therefore, meteor radar winds were analyzed with respect to non-linear interaction, which probably plays a role in winter, but to a lesser degree in summer. Numerical model experiments lead to the conclusion that, although non-linear tidal interaction is indeed one source of the QDT, the major source is direct solar forcing of the 6-hr tidal components.
Erik Schmölter, Jens Berdermann, Norbert Jakowski, Christoph Jacobi, and Rajesh Vaishnav
Adv. Radio Sci., 16, 149–155, https://doi.org/10.5194/ars-16-149-2018, https://doi.org/10.5194/ars-16-149-2018, 2018
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Physical and chemical processes in the ionosphere are driven by complex interactions with the solar radiation. The ionospheric plasma is in particular sensitive to solar variations with a time delay between one and two days.
Here we present preliminary results of the ionospheric delay based on a comprehensive and reliable database consisting of GNSS TEC Maps and EUV spectral flux data.
Rajesh Vaishnav, Christoph Jacobi, Jens Berdermann, Erik Schmölter, and Mihail Codrescu
Adv. Radio Sci., 16, 157–165, https://doi.org/10.5194/ars-16-157-2018, https://doi.org/10.5194/ars-16-157-2018, 2018
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We investigate the ionospheric response to solar Extreme Ultraviolet (EUV) variations using different solar proxies and IGS TEC maps. An ionospheric delay in GTEC is observed at the 27 days solar rotation period with the time scale of about ~ 1–2 days. Here we present preliminary results from the CTIPe model simulations which qualitatively reproduce the observed ~1-2 days delay in GTEC, which is might be due to vertical transport processes.
Gunter Stober, Jorge L. Chau, Juha Vierinen, Christoph Jacobi, and Sven Wilhelm
Atmos. Meas. Tech., 11, 4891–4907, https://doi.org/10.5194/amt-11-4891-2018, https://doi.org/10.5194/amt-11-4891-2018, 2018
Sabine Wüst, Thomas Offenwanger, Carsten Schmidt, Michael Bittner, Christoph Jacobi, Gunter Stober, Jeng-Hwa Yee, Martin G. Mlynczak, and James M. Russell III
Atmos. Meas. Tech., 11, 2937–2947, https://doi.org/10.5194/amt-11-2937-2018, https://doi.org/10.5194/amt-11-2937-2018, 2018
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OH*-spectrometer measurements allow the analysis of gravity wave ground-based periods, but spatial information cannot necessarily be deduced. We combine the approach of Wachter at al. (2015) in order to derive horizontal wavelengths (but based on only one OH* spectrometer) with additional information about wind and temperature and compute vertical wavelengths. Knowledge of these parameters is a precondition for the calculation of further information such as the wave group velocity.
Christoph Jacobi, Tatiana Ermakova, Daniel Mewes, and Alexander I. Pogoreltsev
Adv. Radio Sci., 15, 199–206, https://doi.org/10.5194/ars-15-199-2017, https://doi.org/10.5194/ars-15-199-2017, 2017
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There is continuous interest in coupling processes between the lower and middle atmosphere. Here we analyse midlatitude winds measured by radar at 82–97 km and find that especially in February they are positively correlated with El Niño. The signal is strong for the upper altitudes accessible to the radar, but weakens below. The observations can be qualitatively reproduced by numerical experiments using a mechanistic global circulation model.
Friederike Lilienthal, Christoph Jacobi, Torsten Schmidt, Alejandro de la Torre, and Peter Alexander
Ann. Geophys., 35, 785–798, https://doi.org/10.5194/angeo-35-785-2017, https://doi.org/10.5194/angeo-35-785-2017, 2017
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Gravity waves (GWs) are one of the most important dynamical features of the middle atmosphere that extends from the tropopause to the lower thermosphere. They originate from the troposphere and propagate upward. Here, we show the impact of the horizontal GW distribution in the lower atmosphere on the dynamics of the middle atmosphere using a global circulation model. As a result, we find that non-zonal GW structures can force additional stationary planetary waves.
Gunter Stober, Vivien Matthias, Christoph Jacobi, Sven Wilhelm, Josef Höffner, and Jorge L. Chau
Ann. Geophys., 35, 711–720, https://doi.org/10.5194/angeo-35-711-2017, https://doi.org/10.5194/angeo-35-711-2017, 2017
Martin Kriegel, Norbert Jakowski, Jens Berdermann, Hiroatsu Sato, and Mogese Wassaie Mersha
Ann. Geophys., 35, 97–106, https://doi.org/10.5194/angeo-35-97-2017, https://doi.org/10.5194/angeo-35-97-2017, 2017
Petr Šácha, Friederike Lilienthal, Christoph Jacobi, and Petr Pišoft
Atmos. Chem. Phys., 16, 15755–15775, https://doi.org/10.5194/acp-16-15755-2016, https://doi.org/10.5194/acp-16-15755-2016, 2016
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With a mechanistic model for the middle and upper atmosphere we performed sensitivity simulations to study a possible impact of a localized GW breaking hotspot in the eastern Asia–northern Pacific region and also the possible influence of the spatial distribution of gravity wave activity on the middle atmospheric circulation and transport. We show implications for polar vortex stability, in situ PW generation and longitudinal variability and strength of the Brewer–Dobson circulation.
Ch. Jacobi, N. Samtleben, and G. Stober
Adv. Radio Sci., 14, 169–174, https://doi.org/10.5194/ars-14-169-2016, https://doi.org/10.5194/ars-14-169-2016, 2016
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VHF meteor radar observations of mesosphere/lower thermosphere daily temperatures have been performed at Collm, Germany. The data have been analyzed with respect to long-period oscillations at time scales of 2 to 30 days. The results reveal that oscillations with periods of up to 6 days are more frequently observed during summer, while those with longer periods have larger amplitudes during winter. The results are comparable with analyses from radar wind measurements.
Christoph Jacobi, Norbert Jakowski, Gerhard Schmidtke, and Thomas N. Woods
Adv. Radio Sci., 14, 175–180, https://doi.org/10.5194/ars-14-175-2016, https://doi.org/10.5194/ars-14-175-2016, 2016
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The ionospheric response to solar extreme ultraviolet variability is shown by simple proxies based on Solar Dynamics Observatory/Extreme Ultraviolet Variability Experiment solar spectra. The daily proxies are compared with global mean total electron content. At time scales of the solar rotation up to about 40 days there is a time lag between EUV and TEC variability of about one day, with a tendency to increase for longer time scales.
P. Šácha, A. Kuchař, C. Jacobi, and P. Pišoft
Atmos. Chem. Phys., 15, 13097–13112, https://doi.org/10.5194/acp-15-13097-2015, https://doi.org/10.5194/acp-15-13097-2015, 2015
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In this study, we present a discovery of an internal gravity wave activity and breaking hotspot collocated with an area of anomalously low annual cycle amplitude and specific dynamics in the stratosphere over the Northeastern Pacific/Eastern Asia coastal region. The reasons why this particular IGW activity hotspot was not discovered before nor the specific dynamics of this region pointed out are discussed together with possible consequences on the middle atmospheric dynamics and transport.
F. Lilienthal and Ch. Jacobi
Atmos. Chem. Phys., 15, 9917–9927, https://doi.org/10.5194/acp-15-9917-2015, https://doi.org/10.5194/acp-15-9917-2015, 2015
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The quasi 2-day wave (QTDW), one of the most striking features in the mesosphere/lower thermosphere, is analyzed using meteor radar measurements at Collm (51°N, 13°E) during 2004-2014. The QTDW has periods lasting between 43 and 52h during strong summer bursts, and weaker enhancements are found during winter. A correlation between QTDW amplitudes and wind shear suggests baroclinic instability to be a likely forcing mechanism.
G. Schmidtke, Ch. Jacobi, B. Nikutowski, and Ch. Erhardt
Adv. Radio Sci., 12, 251–260, https://doi.org/10.5194/ars-12-251-2014, https://doi.org/10.5194/ars-12-251-2014, 2014
F. Lilienthal and Ch. Jacobi
Adv. Radio Sci., 12, 205–210, https://doi.org/10.5194/ars-12-205-2014, https://doi.org/10.5194/ars-12-205-2014, 2014
Ch. Jacobi
Adv. Radio Sci., 12, 161–165, https://doi.org/10.5194/ars-12-161-2014, https://doi.org/10.5194/ars-12-161-2014, 2014
Related subject area
Subject: Earth's ionosphere & aeronomy | Keywords: Solar-induced atmospheric variability
Ionospheric response to solar extreme ultraviolet radiation variations: comparison based on CTIPe model simulations and satellite measurements
Rajesh Vaishnav, Erik Schmölter, Christoph Jacobi, Jens Berdermann, and Mihail Codrescu
Ann. Geophys., 39, 341–355, https://doi.org/10.5194/angeo-39-341-2021, https://doi.org/10.5194/angeo-39-341-2021, 2021
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We investigate the delayed ionospheric response using the observed and CTIPe-model-simulated TEC against the solar EUV flux. The ionospheric delay estimated using model-simulated TEC is in good agreement with the delay estimated for observed TEC. The study confirms the model's capabilities to reproduce the delayed ionospheric response against the solar EUV flux. Results also indicate that the average delay is higher in the Northern Hemisphere as compared to the Southern Hemisphere.
Cited articles
Afraimovich, E. L., Astafyeva, E. I., Oinats, A. V., Yasukevich, Y. V., and
Zhivetiev, I. V.: Global electron content: a new conception to track solar
activity, Ann. Geophys., 26, 335–344, https://doi.org/10.5194/angeo-26-335-2008,
2008. a
Anderson, P. C. and Hawkins, J. M.: Topside ionospheric response to solar EUV
variability, J. Geophys. Res.-Space, 121, 1518–1529,
https://doi.org/10.1002/2015ja021202, 2016. a
Brasseur, G. P. and Solomon, S.: Aeronomy of the middle atmosphere: Chemistry
and physics of the stratosphere and mesosphere, Vol. 32, 3rd Edn., 646 pp., Springer, Dordrecht, the Netherlands, 2005. a
Chandra, S. and Sinha, A. K.: The role of eddy turbulence in the development of
self-consistent models of the lower and upper thermospheres, J.
Geophys. Res., 79, 1916–1922, https://doi.org/10.1029/ja079i013p01916, 1974. a, b
Codrescu, M. V., Fuller-Rowell, T. J., Munteanu, V., Minter, C. F., and
Millward, G. H.: Validation of the Coupled Thermosphere Ionosphere
Plasmasphere Electrodynamics model: CTIPE-Mass Spectrometer Incoherent
Scatter temperature comparison, Space Weather, 6, S09005, https://doi.org/10.1029/2007sw000364,
2008. a
Codrescu, M. V., Negrea, C., Fedrizzi, M., Fuller-Rowell, T. J., Dobin, A.,
Jakowsky, N., Khalsa, H., Matsuo, T., and Maruyama, N.: A real-time run of
the Coupled Thermosphere Ionosphere Plasmasphere Electrodynamics (CTIPe)
model, Space Weather, 10, S02001, https://doi.org/10.1029/2011sw000736, 2012. a, b
Colegrove, F. D., Hanson, W. B., and Johnson, F. S.: Eddy diffusion and oxygen
transport in the lower thermosphere, J. Geophys. Res., 70,
4931–4941, https://doi.org/10.1029/jz070i019p04931, 1965. a
Danilov, A. D. and Konstantinova, A. V.: Reduction of the atomic oxygen content
in the upper atmosphere, Geomagn. Aeronomy, 54, 224–229,
https://doi.org/10.1134/s0016793214020066, 2014. a
Fuller-Rowell, T. J.: A two-dimensional, high-resolution, nested-grid model
of the thermosphere: 1. Neutral response to an electric field
“spike”, J. Geophys.
Res., 89, 2971, https://doi.org/10.1029/ja089ia05p02971, 1984. a
Fuller-Rowell, T. J. and Rees, D.: A Three-Dimensional Time-Dependent Global
Model of the Thermosphere, J. Atmos. Sci., 37,
2545–2567, https://doi.org/10.1175/1520-0469(1980)037<2545:atdtdg>2.0.co;2, 1980. a, b, c
Fuller-Rowell, T. J. and Rees, D.: Derivation of a conservation equation for
mean molecular weight for a two-constituent gas within a three-dimensional,
time-dependent model of the thermosphere, Planet. Space Sci., 31,
1209–1222, https://doi.org/10.1016/0032-0633(83)90112-5, 1983. a, b
Fuller-Rowell, T. J. and Rees, D.: Turbulent diffusion variability and
implications for the upper thermosphere, Adv. Space Res., 12,
45–56, https://doi.org/10.1016/0273-1177(92)90443-2, 1992. a, b, c
Fuller-Rowell, T. J., Rees, D., Quegan, S., Moffett, R., and Bailey, G.:
Interactions between neutral thermospheric composition and the polar
ionosphere using a coupled ionosphere-thermosphere model, J.
Geophys. Res., 92, 7744, https://doi.org/10.1029/ja092ia07p07744, 1987. a
Jacobi, C., Jakowski, N., Schmidtke, G., and Woods, T. N.: Delayed response of
the global total electron content to solar EUV variations, Adv.
Radio Sci., 14, 175–180, https://doi.org/10.5194/ars-14-175-2016, 2016. a, b
Jones, M., Forbes, J. M., and Hagan, M. E.: Tidal-induced net transport effects
on the oxygen distribution in the thermosphere, Geophys. Res. Lett.,
41, 5272–5279, https://doi.org/10.1002/2014gl060698, 2014a. a
Jones, M., Forbes, J. M., Hagan, M. E., and Maute, A.: Impacts of vertically
propagating tides on the mean state of the ionosphere-thermosphere system,
J. Geophys. Res.-Space, 119, 2197–2213,
https://doi.org/10.1002/2013ja019744, 2014b. a
Jones, M., Emmert, J. T., Drob, D. P., Picone, J. M., and Meier, R. R.: Origins
of the Thermosphere-Ionosphere Semiannual Oscillation: Reformulating the
“Thermospheric Spoon” Mechanism, J. Geophys. Res.-Space, 123, 931–954,
https://doi.org/10.1002/2017ja024861, 2018. a
Keneshea, T. J. and Zimmerman, S. P.: The Effect of Mixing Upon Atomic and
Molecular Oxygen in the 70–170 km Region of the Atmosphere,
J. Atmos. Sci., 27, 831–840,
https://doi.org/10.1175/1520-0469(1970)027<0831:teomua>2.0.co;2, 1970. a
Kirchhoff, V. W. J. H. and Clemesha, B. R.: Eddy diffusion coefficients in the
lower thermosphere, J. Geophys. Res., 88, 5765,
https://doi.org/10.1029/ja088ia07p05765, 1983. a, b, c
Lee, C.-K., Han, S.-C., Bilitza, D., and Seo, K.-W.: Global characteristics of
the correlation and time lag between solar and ionospheric parameters in the
27-day period, J. Atmos. Sol.-Terr. Phys., 77,
219–224, https://doi.org/10.1016/j.jastp.2012.01.010, 2012. a
Li, F., Liu, A. Z., and Swenson, G. R.: Characteristics of instabilities in the
mesopause region over Maui, Hawaii, J. Geophys. Res., 110, D09S12,
https://doi.org/10.1029/2004jd005097, 2005. a
Liu, L., Wan, W., Ning, B., Pirog, O. M., and Kurkin, V. I.: Solar activity
variations of the ionospheric peak electron density, J. Geophys.
Res., 111, A08304, https://doi.org/10.1029/2006ja011598, 2006. a
Meraner, K. and Schmidt, H.: Transport of nitrogen oxides through the winter
mesopause in HAMMONIA, J. Geophys. Res.-Atmos., 121,
2556–2570, https://doi.org/10.1002/2015jd024136, 2016. a
Millward, G., Moffett, R., Quegan, S., and Fuller-Rowell, T.: A coupled
thermosphere-ionosphere-plasmasphere model (CTIP), STEP handbook on
ionospheric models, 239–279, 1996. a
Pilinski, M. D. and Crowley, G.: Seasonal variability in global eddy diffusion
and the effect on neutral density, J. Geophys. Res.-Space, 120, 3097–3117, https://doi.org/10.1002/2015ja021084, 2015. a
Qian, L., Solomon, S. C., and Kane, T. J.: Seasonal variation of thermospheric
density and composition, J. Geophys. Res.-Space, 114, A01312,
https://doi.org/10.1029/2008ja013643, 2009. a
Qian, L., Burns, A. G., Solomon, S. C., and Wang, W.: Annual/semiannual
variation of the ionosphere, Geophys. Res. Lett., 40, 1928–1933,
https://doi.org/10.1002/grl.50448, 2013. a
Quegan, S., Bailey, G., Moffett, R., Heelis, R., Fuller-Rowell, T., Rees, D.,
and Spiro, R.: A theoretical study of the distribution of ionization in the
high-latitude ionosphere and the plasmasphere: first results on the
mid-latitude trough and the light-ion trough, J. Atmos.
Terr. Phys., 44, 619–640, https://doi.org/10.1016/0021-9169(82)90073-3, 1982. a, b
Rees, D. and Fuller-Rowell, T.: Understanding the transport of atomic oxygen
within the thermosphere, using a numerical global thermospheric model,
Planet. Space Sci., 36, 935–948,
https://doi.org/10.1016/0032-0633(88)90101-8, 1988. a, b, c
Ren, D., Lei, J., Wang, W., Burns, A., Luan, X., and Dou, X.: Does the Peak
Response of the Ionospheric F2 Region Plasma Lag the Peak of 27-Day Solar
Flux Variation by Multiple Days?, J. Geophys. Res.-Space, 123, 7906–7916, https://doi.org/10.1029/2018ja025835, 2018. a, b, c, d
Ren, D., Lei, J., Wang, W., Burns, A., Luan, X., and Dou, X.: A Simulation
Study on the Time Delay of Daytime Thermospheric Temperature Response to the
27-Day Solar EUV Flux Variation, J. Geophys. Res.-Space, 124, 9184–9193, https://doi.org/10.1029/2019ja027000, 2019. a
Ren, D., Lei, J., Wang, W., Burns, A., Luan, X., and Dou, X.: Different Peak
Response Time of Daytime Thermospheric Neutral Species to the 27-Day Solar
EUV Flux Variations, J. Geophys. Res.-Space, 125, e2020JA027840,
https://doi.org/10.1029/2020ja027840, 2020. a, b
Ren, D., Lei, J., Wang, W., Burns, A., and Luan, X.: Observations and
simulations of the peak response time of thermospheric mass density to the
27-day solar EUV flux variation, J. Geophys. Res.-Space, 126, e2020JA028756, https://doi.org/10.1029/2020JA028756, 2021. a
Richards, P. G., Fennelly, J. A., and Torr, D. G.: EUVAC: A solar EUV Flux
Model for aeronomic calculations, J. Geophys. Res., 99, 8981,
https://doi.org/10.1029/94ja00518, 1994. a
Richmond, A. D., Ridley, E. C., and Roble, R. G.: A thermosphere/ionosphere
general circulation model with coupled electrodynamics, Geophys. Res.
Lett., 19, 601–604, https://doi.org/10.1029/92gl00401, 1992. a, b
Rishbeth, H.: How the thermospheric circulation affects the ionospheric F2
layer, J. Atmos. Sol.-Terr.l Phys., 60, 1385–1402,
https://doi.org/10.1016/s1364-6826(98)00062-5, 1998. a, b
Rishbeth, H., Fuller-Rowell, T., and Rees, D.: Diffusive equilibrium and
vertical motion in the thermosphere during a severe magnetic storm : A
computational study, Planet. Space Sci., 35, 1157–1165,
https://doi.org/10.1016/0032-0633(87)90022-5, 1987. a
Sasi, M. N. and Vijayan, L.: Turbulence characteristics in the tropical
mesosphere as obtained by MST radar at Gadanki (13.5∘ N,
79.2∘ E), Ann. Geophys., 19, 1019–1025,
https://doi.org/10.5194/angeo-19-1019-2001, 2001. a, b, c
Schmölter, E., Berdermann, J., and Codrescu, M.: The delayed ionospheric
response to the 27-day solar rotation period analyzed with GOLD and IGS TEC
data, J. Geophys. Res.-Space, 126, e2020JA028861,
https://doi.org/10.1029/2020JA028861, 2021. a
Shim, J. S., Kuznetsova, M., Rastätter, L., Hesse, M., Bilitza, D., Butala,
M., Codrescu, M., Emery, B., Foster, B., Fuller-Rowell, T., Huba, J.,
Mannucci, A. J., Pi, X., Ridley, A., Scherliess, L., Schunk, R. W., Stephens,
P., Thompson, D. C., Zhu, L., Anderson, D., Chau, J. L., Sojka, J. J., and
Rideout, B.: CEDAR Electrodynamics Thermosphere Ionosphere (ETI)
Challenge for systematic assessment of ionosphere/thermosphere models:
NmF2, hmF2, and vertical drift using ground-based observations, Space
Weather, 9, S12003, https://doi.org/10.1029/2011sw000727, 2011. a
Shimazaki, T.: Effective eddy diffusion coefficient and atmospheric composition
in the lower thermosphere, J. Atmos. Terr. Phys.,
33, 1383–1401, https://doi.org/10.1016/0021-9169(71)90011-0, 1971. a, b, c, d
Siskind, D. E., Drob, D. P., Dymond, K. F., and McCormack, J. P.: Simulations
of the effects of vertical transport on the thermosphere and ionosphere using
two coupled models, J. Geophys. Res.-Space, 119,
1172–1185, https://doi.org/10.1002/2013ja019116, 2014. a
St.-Maurice, J. P. and Torr, D. G.: Nonthermal rate coefficients in the
ionosphere: The reactions of O+ with N2, O2, and NO,
J. Geophys. Res., 83, 969–977, https://doi.org/10.1029/ja083ia03p00969,
1978. a
Su, Y. Z., Bailey, G. J., and Fukao, S.: Altitude dependencies in the solar
activity variations of the ionospheric electron density, J.
Geophys. Res.-Space, 104, 14879–14891,
https://doi.org/10.1029/1999ja900093, 1999. a, b
Swenson, G., Yee, Y., Vargas, F., and Liu, A.: Vertical diffusion transport of
atomic oxygen in the mesopause region consistent with chemical losses and
continuity: Global mean and inter-annual variability, J. Atmos. Sol.-Terr. Phys., 178, 47–57,
https://doi.org/10.1016/j.jastp.2018.05.014, 2018. a
Swenson, G. R., Salinas, C. C. J. H., Vargas, F., Zhu, Y., Kaufmann, M., Jones,
M., Drob, D. P., Liu, A., Yue, J., and Yee, J. H.: Determination of Global
Mean Eddy Diffusive Transport in the Mesosphere and Lower Thermosphere From
Atomic Oxygen and Carbon Dioxide Climatologies, J. Geophys.
Res.-Atmos., 124, 13519–13533, https://doi.org/10.1029/2019jd031329,
2019. a, b
Tapping, K. F.: Recent solar radio astronomy at centimeter wavelengths: The
temporal variability of the 10.7-cm flux, J. Geophys. Res.,
92, 829–838, https://doi.org/10.1029/jd092id01p00829, 1987. a
Vaishnav, R., Jacobi, C., Berdermann, J., Schmölter, E., and Codrescu, M.:
Ionospheric response to solar EUV variations: Preliminary results, Adv. Radio Sci., 16, 157–165, https://doi.org/10.5194/ars-16-157-2018, 2018. a, b, c
Vaishnav, R., Jacobi, C., and Berdermann, J.: Long-term trends in the
ionospheric response to solar extreme-ultraviolet variations, Ann.
Geophys., 37, 1141–1159, https://doi.org/10.5194/angeo-37-1141-2019, 2019. a
Vaishnav, R., Schmölter, E., Jacobi, C., Berdermann, J., and Codrescu, M.:
Ionospheric response to solar extreme ultraviolet radiation variations:
comparison based on CTIPe model simulations and satellite measurements,
Ann. Geophys., 39, 341–355, https://doi.org/10.5194/angeo-39-341-2021, 2021. a
Short summary
We investigate the role of eddy diffusion in the delayed ionospheric response against solar flux changes in the solar rotation period using the CTIPe model. The study confirms that eddy diffusion is an important factor affecting the delay of the total electron content. An increase in eddy diffusion leads to faster transport processes and an increased loss rate, resulting in a decrease in the ionospheric delay.
We investigate the role of eddy diffusion in the delayed ionospheric response against solar flux...
