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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

VHF radar observed characteristics of convectively generated gravity waves during wet<br />

<strong>an</strong>d dry spells of Indi<strong>an</strong> summer monsoon<br />

Uma K. N 1 , Kar<strong>an</strong>am Kishore Kumar 2 , Rao T. Naray<strong>an</strong>a 3<br />

1 Space Physics Laboratory, Triv<strong>an</strong>drum, India, 2 Space Physics Laboratory, Triv<strong>an</strong>drum, India, 3<br />

National Atmospheric Research Laboratory, Tirupati, India<br />

A powerful VHF radar observed characteristics of convectively generated gravity<br />

waves (CGW) excited during the wet <strong>an</strong>d dry spells of Indi<strong>an</strong> summer monsoon over a<br />

tropical station Gad<strong>an</strong>ki (13.5 0 N, 79.2 0 E) are discussed. The characteristics of gravity waves<br />

in the lower stratosphere during these two spells are discussed in terms their wavelet spectra<br />

along with height-time sections of vertical velocities. In most of the cases, the lower<br />

stratospheric gravity wave amplitudes were found to be relatively more in dry spell compared<br />

to wet spell. The wavelet <strong>an</strong>alysis of lower stratospheric vertical velocities showed a<br />

domin<strong>an</strong>t periodicity of about ~20- 40 min in wet spell <strong>an</strong>d ~15-20 min in dry spell. The<br />

<strong>an</strong>alyses also showed clearly that wet spell is found to be more conducive for the generation<br />

of gravity waves. However, the propagation of these waves to the stratosphere is found to be<br />

more efficient during dry spell of monsoon. The strengthening/weakening of the tropical<br />

easterly jet during wet/dry spell of monsoon is found to be the main reason for the<br />

inhibited/enh<strong>an</strong>ced wave activity in the lower stratosphere during wet/dry spell. The present<br />

<strong>an</strong>alysis also suggests that the static stability of the mid <strong>an</strong>d upper troposphere during dry <strong>an</strong>d<br />

wet spell have implications in the observed frequency of the CGW. Thus, the present <strong>an</strong>alyses<br />

brought out for the first time the features of CGW during two distinctive regimes of<br />

convective systems <strong>an</strong>d emphasized the import<strong>an</strong>ce of prevailing background conditions in<br />

exciting them.

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