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dc.contributor.authorKakade, S.B.-
dc.contributor.authorDugam, S.S.-
dc.date.accessioned2008-06-18T09:33:33Z-
dc.date.available2008-06-18T09:33:33Z-
dc.date.issued2006-09-
dc.identifier.issn0379-5136-
dc.identifier.urihttp://hdl.handle.net/123456789/1517-
dc.description205-209en_US
dc.description.abstractIn this paper, the effect of Winter-NAO on northern hemispheric temperature and snow-cover is studied because North Atlantic Oscillation (NAO) fluctuations are strongest in the winter season. The correlation analysis, for the period 1973-2003, suggests that winter-NAO is inversely associated with Northern hemispheric snow-cover from winter through summer and the correlation coefficients are significant at 5% level. Moreover, NAO is showing direct relationship with northern hemispheric temperature during winter season. This relationship is also significant at 5% level. The stability of this relationship is tested and found to be stable. The correlation analysis further suggests that winter-NAO and global temperature difference between land and ocean have direct association, which is significant at 5% level. The effect of rising trend in winter-NAO may have resulted in decreasing northern hemispheric snow-cover, which ultimately results in warming of northern hemispheric temperature. The study suggests that NAO plays an important role in warming of northern hemisphere through decreasing northern hemispheric snow-cover extent.en_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.sourceIJMS Vol.35(3) [September 2006]en_US
dc.subjectNAOen_US
dc.subjectSnow-coveren_US
dc.subjectNorthern hemisphere temperatureen_US
dc.subjectSSTen_US
dc.subjectWarmingen_US
dc.subjectLand-ocean temperatureen_US
dc.subjectThermal contrasten_US
dc.titleNorth Atlantic Oscillation and northern hemispheric warmingen_US
dc.typeArticleen_US
Appears in Collections: IJMS Vol.35(3) [September 2006]

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