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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-28-2201-2010</article-id>
<title-group>
<article-title>A diagnostic study of monsoon energetics for two contrasting years</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ramakrishna</surname>
<given-names>S. S. V. S.</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>Brahmananda Rao</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sravani</surname>
<given-names>A.</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>Vijaya Saradhi</surname>
<given-names>N.</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>Harikishan</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Meteorology &amp; Oceanography, Andhra University, Visakhapatnam-530003, India</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Instituto Nacional de Pesquisas Espaciais, INPE. São José dos Campos, S.P, Brazil</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>12</month>
<year>2010</year>
</pub-date>
<volume>28</volume>
<issue>12</issue>
<fpage>2201</fpage>
<lpage>2212</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 S. S. V. S. Ramakrishna et al.</copyright-statement>
<copyright-year>2010</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/28/2201/2010/angeo-28-2201-2010.html">This article is available from https://angeo.copernicus.org/articles/28/2201/2010/angeo-28-2201-2010.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/28/2201/2010/angeo-28-2201-2010.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/28/2201/2010/angeo-28-2201-2010.pdf</self-uri>
<abstract>
<p>In the present study we made an attempt to explain the behavior of the
southwest monsoon for two contrasting years, from the view point of
energetics. As a test case we selected 2002 and 2003, which were weak and
strong monsoon years, respectively, based on rainfall. The energy terms &lt;I&gt;K&lt;/I&gt;&amp;psi;, &lt;I&gt;K&lt;/I&gt;&amp;chi;
and APE and the conversion terms &lt;I&gt;f&lt;/I&gt;&amp;nabla;&amp;psi;. &amp;#8711;&amp;chi;, &lt;span style=&quot;border-top: 1px solid #000; color: #000;&quot;&gt;&amp;minus;&amp;omega;&apos;&lt;I&gt;T&lt;/I&gt;&apos;&lt;/span&gt; are calculated at 850 hPa level and also
vertically integrated from 1000 hPa to 100 hPa. The results indicate that, the
year of high energy (both &lt;I&gt;K&lt;/I&gt;&lt;sub&gt;&amp;Psi;&lt;/sub&gt;, &lt;I&gt;K&lt;/I&gt;&lt;sub&gt;&amp;chi;&lt;/sub&gt;) i.e. 2002, does not give
a good amount of rainfall compared to the good year i.e. 2003. The break
period during the year 2002 has been clearly explained using the block
diagrams. Periods of highest rainfall coincide with the positive conversions
of &lt;I&gt;f&lt;/I&gt;&amp;nabla;&amp;psi;. &amp;nabla;&amp;chi; and &lt;span style=&quot;border-top: 1px solid #000; color: #000;&quot;&gt;&amp;minus;&amp;omega;&apos;&lt;I&gt;T&lt;/I&gt;&apos;&lt;/span&gt;. Vertically
integrated moisture fluxes during the break period of 2002, 2003 are also
analyzed. The main reservoirs (sources and sinks) for the monsoon energy are
also identified using block diagrams. Negative correlation between daily
rainfall and energy terms in the year 2002 indicates its unusual behavior
both in terms of energetics as well as precipitation. Positive correlations
in the year 2003 represent strong monsoonal behavior. We calculated the
climatology of the total kinetic energy at 850 hPa, vertically integrated
(1000–100 hPa) for 30 years (1980–2009) and rainfall for 103 years
(1901–2003) which clearly indicates that the monsoon is indeed a season of
high energy for the South Asian region.

&lt;br&gt;&lt;br&gt;

Also the east- west direct thermal circulations are strongly related to the
good and bad monsoon years.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>