Dominant Modes of Interannual Variability in Eurasian Surface Air Temperature during Boreal Spring
Author(s) -
Shangfeng Chen,
Renguang Wu,
Yong Liu
Publication year - 2015
Publication title -
journal of climate
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.315
H-Index - 287
eISSN - 1520-0442
pISSN - 0894-8755
DOI - 10.1175/jcli-d-15-0524.1
Subject(s) - climatology , anticyclone , anomaly (physics) , arctic oscillation , geology , sea surface temperature , atmospheric circulation , advection , north atlantic oscillation , extratropical cyclone , boreal , middle latitudes , latitude , northern hemisphere , atmospheric sciences , paleontology , physics , geodesy , thermodynamics , condensed matter physics
This study investigates interannual variations of surface air temperature (SAT) over mid- and high latitudes of Eurasia during boreal spring and their association with snow, atmospheric circulation, and sea surface temperature (SST) changes. The leading mode of spring SAT variations is featured by same-sign anomalies over most regions. The second mode features a tripole anomaly pattern with anomalies over the central part opposite to those over the eastern and western parts of Eurasia. A diagnosis of surface heat flux anomalies suggests that snow change contributes partly to SAT anomalies in several regions mainly by modulating surface shortwave radiation but cannot explain SAT changes in other regions. Atmospheric circulation anomalies play an important role in spring SAT variability via wind-induced heat advection and cloud-induced surface radiation changes. Positive SAT anomalies are associated with anomalous westerly winds from the North Atlantic Ocean or with anomalous anticyclone and souther...
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