Dynamical influences on European climate: an uncertain future

被引:119
作者
Woollings, Tim [1 ]
机构
[1] Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England
来源
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 2010年 / 368卷 / 1924期
关键词
jet stream; storm track; blocking; meridional overturning circulation; stratosphere; NORTH-ATLANTIC OSCILLATION; HEMISPHERE ATMOSPHERIC BLOCKING; WINTER STATIONARY WAVES; STORM TRACKS; OCEAN DYNAMICS; PART II; VARIABILITY; CIRCULATION; SEA; ENSEMBLE;
D O I
10.1098/rsta.2010.0040
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
Climate science is coming under increasing pressure to deliver projections of future climate change at spatial scales as small as a few kilometres for use in impacts studies. But is our understanding and modelling of the climate system advanced enough to offer such predictions? Here we focus on the Atlantic-European sector, and on the effects of greenhouse gas forcing on the atmospheric and, to a lesser extent, oceanic circulations. We review the dynamical processes which shape European climate and then consider how each of these leads to uncertainty in the future climate. European climate is unique in many regards, and as such it poses a unique challenge for climate prediction. Future European climate must be considered particularly uncertain because (i) the spread between the predictions of current climate models is still considerable and (ii) Europe is particularly strongly affected by several processes which are known to be poorly represented in current models.
引用
收藏
页码:3733 / 3756
页数:24
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