Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century

Details Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century

Jun 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004georl..3112204y&link_type=abstract

Geophysical Research Letters, Volume 31, Issue 12, CiteID L12204

Physics

29

Global Change: Climate Dynamics (3309), Global Change: Atmosphere (0315, 0325), Atmospheric Composition And Structure: Evolution Of The Atmosphere

Scientific paper

At odds with global warming trends, surface air temperature over large subtropical Eurasia continent in spring March exhibits unique strong cooling over the last half century. The cause for this cooling is shown to be related to Winter (DJF) North Atlantic Oscillation (W-NAO). Positive values of W-NAO provoke cooling signals in northern Africa continent simultaneously from surface to tropopause. The W-NAO generated signals barotropically extend eastward over most of subtropical Eurasia and reaches eastern China in March.

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