Resmi, E A; Dr.Mohanakumar,K(Cochin University Of Science And Technology, September , 2012)
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Abstract:
The stratospheric warming events are categorized into major and minor
warming depending on the temperature increase in the polar stratosphere.
The warming is called a ‘major’, when the polar temperature increases
poleward from 60 degree latitude and followed by a reversal in the zonal
wind at 10 hPa (~32 Km). Usually major warming events are associated
with the displacement of polar vortex from high to mid latitudes or the
splitting of vortices in to two. The warming is called a "Minor", when the
polar temperature increases more than 25 degree in a period of a week or
less, at any stratospheric level with less intensified easterly wind anomalies. The stratospheric warmings generated during the transition
period of winter to spring are called final warmings. The warming events
observed in the early winter period (November to early December) over
Canadian region are called Canadian warmings. There is strong
interaction between stratosphere and troposphere during SSW period over
high and low latitudes regions.
The thesis consists of 7 chapters
Description:
Department of Atmospheric Sciences, Cochin
University of Science and Technology