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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-20-107-2002</article-id>
<title-group>
<article-title>A study of the relationship between cloud-to-ground lightning and precipitation in the convective weather system in China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhou</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Qie</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Soula</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratoire d’Aerologie, UMR 5560 UPS/CNRS, OMP, 14 av. E. Belin 31400 Toulouse, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Correspondence to: X. Qie (qiex@ns.lzb.ac.cn)</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>01</month>
<year>2002</year>
</pub-date>
<volume>20</volume>
<issue>1</issue>
<fpage>107</fpage>
<lpage>113</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2002 Y. Zhou et al.</copyright-statement>
<copyright-year>2002</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://angeo.copernicus.org/articles/20/107/2002/angeo-20-107-2002.html">This article is available from https://angeo.copernicus.org/articles/20/107/2002/angeo-20-107-2002.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/20/107/2002/angeo-20-107-2002.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/20/107/2002/angeo-20-107-2002.pdf</self-uri>
<abstract>
<p>In this paper, the
 correlation between cloud-to-ground (CG) lightning and precipitation has been
 studied by making use of the data from weather radar, meteorological soundings,
 and a lightning location system that includes three direction finders about 40
 km apart from each other in the Pingliang area of east Gansu province in P. R.
 China. We have studied the convective systems that developed during two cold
 front processes passing over the observation area, and found that the CG
 lightning can be an important factor in the precipitation estimation. The
 regression equation between the average precipitation intensity (&lt;i&gt;R&lt;/i&gt;) and
 the number of CG lightning flashes (&lt;i&gt;L&lt;/i&gt;) in the main precipitation period
 is &lt;i&gt;R&lt;/i&gt; = 1.69 ln (&lt;i&gt;L&lt;/i&gt;) - 0.27, and the correlation coefficient &lt;i&gt;r&lt;/i&gt;
 is 0.86. The CG lightning flash rate can be used as an indicator of the
 formation and development of the convective weather system. Another more
 exhaustive precipitation estimation method has been developed by analyzing the
 temporal and spatial distributions of the precipitation relative to the
 location of the CG lightning flashes. Precipitation calculated from the CG
 lightning flashes is very useful, especially in regions with inadequate radar
 cover.&lt;br&gt;&lt;br&gt;&lt;b&gt;Key words. &lt;/b&gt;Meteorology and
 atmospheric dynamics (atmospheric electricity; lightning; precipitation)</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
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