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dc.contributor.authorLal, M.
dc.contributor.authorSubramanian, M.V.
dc.date.accessioned2015-09-15T06:36:04Z
dc.date.accessioned2021-02-12T09:29:20Z-
dc.date.available2015-09-15T06:36:04Z
dc.date.available2021-02-12T09:29:20Z-
dc.date.issued2007
dc.identifier.citationCP23, International Symposium on Rainfall Rate and Radio Wave Propagation (ISRR'07) ed. by R.S.Jaiswal and S.Uma, p.289-295, 2007, doi: 10.1063/1.2767049en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/410-
dc.description.abstractWe have made an attempt to study the influence of geomagnetic storm on the equatorial upper troposphere temperature and wind variability. The NCEP — Re analysis data has been taken as an input for the present study. The Dst index has been taken as an indicator of the onset of magnetic storm and its strength. The change in the upper tropospheric temperature and wind variation over equatorial latitude is found to be sensitive to the onset of geomagnetic storm. The superpose epoch analysis shows the changes in temperature and wind velocity after 3 days of the onset of the event. The influence of QBO phase has been found to be effective on the temperature as well as vertical wind velocity variation. The change in the magnitude is also sensitive to the solar activity condition. The increase in the temperature during W‐phase of QBO and vice versa has been observed after the onset of the event. The horizontal wind velocity shows the influence of magnetic storm on the continent as well as over the Ocean. One of the possible mechanism is the geomagnetic activity influences equatorial tropospheric meteorological parameters via the stratosphere.en_US
dc.language.isoenen_US
dc.subjectGeomagnetic stormsen_US
dc.subjectStorms and substormsen_US
dc.subjectDensityen_US
dc.subjectAtmospheric temperatureen_US
dc.subjectTroposphereen_US
dc.subjectSolar activityen_US
dc.subjectMeteorologicalen_US
dc.titleMeteorological characteristics changes in equatorial latitude associated with solar activityen_US
dc.typeArticleen_US
dc.identifier.accession090907
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