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dc.contributor.authorMuraleedharan, P.M.
dc.contributor.authorNisha, P.G.
dc.contributor.authorMohankumar, K.
dc.date.accessioned2011-08-23T09:37:07Z
dc.date.available2011-08-23T09:37:07Z
dc.date.issued2011
dc.identifier.citationJournal of Atmospheric and Solar-Terrestrial Physics, vol.73; 2011; 1988-1998
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/3903
dc.description.abstractAtmospheric perturbations due to the annular solar eclipse were monitored to understand its influence on the meteorological parameters from surface to the lower stratosphere. A strong inversion at 13 km and an abnormal warming in the upper troposphere were noticed on the eclipse day. A decrease in tropopause height associated with increase in temperature caused anomalous warming. Considerable attenuation of incoming solar radiation resulted in abrupt increase of air temperature during the next 24 h followed by sharp decrease in relative humidity. The time lag is attributed to the distance from the totality and the response time between tropopause and surface layer
dc.language.isoen
dc.publisherElsevier
dc.rightsAn edited version of this paper was published by Elsevier. Copyright [2011] Elsevier
dc.subjectsolar eclipse
dc.subjecthumidity
dc.subjectVaisala radiosonde
dc.subjectTropopause
dc.titleEffect of January 15, 2010 annular solar eclipse on meteorological parameters over Goa, India
dc.typeJournal Article


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