DYNAMIC CONTRIBUTION TO HEMISPHERIC MEAN TEMPERATURE TRENDS

被引:149
作者
WALLACE, JM
ZHANG, Y
RENWICK, JA
机构
[1] Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195-1640
关键词
D O I
10.1126/science.270.5237.780
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
On the basis of land station data from the Northern Hemisphere, it was determined that roughly half of the temporal variance of monthly mean hemispheric mean anomalies in surface air temperature during the period from 1900 through 1990 were linearly related to the amplitude of a distinctive spatial pattern in which the oceans are anomalously cold and the continents are anomalously warm poleward of 40 degrees north when the hemisphere is warm. Apart from an upward trend since 1975, to which El Nino has contributed, the amplitude time series associated with this pattern resembles seasonally dependent white noise. It is argued that the variability associated with this pattern is dynamically induced and is not necessarily an integral part of the fingerprint of global warming.
引用
收藏
页码:780 / 783
页数:4
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