Geomagnetic-induced tropopause temperature and wind variation over low latitude

dc.contributor.authorLal, M.
dc.contributor.authorSubramanian, M.V.
dc.date.accessioned2015-09-15T09:21:59Z
dc.date.accessioned2021-02-12T09:27:33Z
dc.date.available2015-09-15T09:21:59Z
dc.date.available2021-02-12T09:27:33Z
dc.date.issued2008
dc.description.abstractThe present study reports the effect of geomagnetic storm on 200 mb altitude temperature and wind at a low latitude (8.7°N, 77.8°N) Indian region. The severe and strong geomagnetic storm (Dst < – 100 nT) between 2000 and 2005 has been studied. The impact of the geomagnetic activity on temperature and wind variation is affected by the QBO (Quasi-Biennial Oscillation) phase. The tropopause temperature increases by ~ 2.5 K during W-phase of QBO and decreases by ~ 1.5 K during E-phase of QBO. The time lag between the onset of the event and the maximum change in temperature becomes a minimum during the transition phase of QBO. The horizontal wind velocity shows a pronounced effect over the east coast of India. The effect has not been observed during the onset of the south-west monsoon. The vertical wind velocity at 200 mb shows increase (or decrease) during W- (or E-) phase of the event.en_US
dc.identifier.accession090914
dc.identifier.citationIndian Journal of Radio & Space Physics, v.37, p.258-263, 2008en_US
dc.identifier.urihttp://library.iigm.res.in:4000/handle/123456789/416
dc.language.isoenen_US
dc.subjectTropical meteorologyen_US
dc.subjectStorms and substormsen_US
dc.subjectWind variationen_US
dc.subjectTropopause temperatureen_US
dc.subjectLow latitudeen_US
dc.titleGeomagnetic-induced tropopause temperature and wind variation over low latitudeen_US
dc.typeArticleen_US

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