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Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456789/609
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dc.contributor.authorSridharan, S.
dc.contributor.authorRaghunath, K.
dc.contributor.authorSathishkumar, S.
dc.contributor.authorNath, D.
dc.date.accessioned2015-10-15T09:12:06Z
dc.date.accessioned2021-02-12T09:34:48Z-
dc.date.available2015-10-15T09:12:06Z
dc.date.available2021-02-12T09:34:48Z-
dc.date.issued2010
dc.identifier.citationJASTP, v.72/14-15, p.1139-1146, 2010, doi10.1016/j.jastp.2010.06.003en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/609-
dc.description.abstractRayleigh lidar observations at Gadanki (13.5°N, 79.2°E) show an enhancement of the nightly mean temperature by 10–15 K at altitudes 70–80 km and of gravity wave potential energy at 60–70 km during the 2009 major stratospheric warming event. An enhanced quasi-16-day wave activity is observed at 50–70 km in the wavelet spectrum of TIMED–SABER temperatures, possibly due to the absence of a critical level in the low-latitude stratosphere because of less westward winds caused by this warming event. The observed low-latitude mesospheric warming could be due to wave breaking, as waves are damped at 80 km.en_US
dc.language.isoenen_US
dc.subjectMajor sudden stratospheric warmingen_US
dc.subjectGravity wavesen_US
dc.subjectPlanetary wavesen_US
dc.subjectMeridional circulationen_US
dc.titleFirst results of warm mesospheric temperature over Gadanki (13.5°N, 79.2°E) during the sudden stratospheric warming of 2009en_US
dc.typeArticleen_US
dc.identifier.accession091132
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