Resolving the 21st century temperature trends of the upper troposphere-lower stratosphere with satellite observations

被引:9
|
作者
Ladstaedter, Florian [1 ]
Steiner, Andrea K. [1 ]
Gleisner, Hans [2 ]
机构
[1] Karl Franzens Univ Graz, Wegener Ctr Climate & Global Change, Graz, Austria
[2] Danish Meteorol Inst, Lyngbyvej 100, Copenhagen, Denmark
关键词
GPS RADIO OCCULTATION; BREWER-DOBSON CIRCULATION; MODEL; RADIOSONDES; SIMULATIONS; UNCERTAINTY; PROFILES; MYSTERY;
D O I
10.1038/s41598-023-28222-x
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
Historically, observational information about atmospheric temperature has been limited due to a lack of suitable measurements. Recent advances in satellite observations provide new insight into the fine structure of the free atmosphere, with the upper troposphere and lower stratosphere comprising essential components of the climate system. This is a prerequisite for understanding the complex processes of this part of the atmosphere, which is also known to have a large impact on surface climate. With unprecedented resolution, latest climate observations reveal a dramatic warming of the atmosphere. The tropical upper troposphere has already warmed about 1 K during the first two decades of the 21st century. The tropospheric warming extends into the lower stratosphere in the tropics and southern hemisphere mid-latitudes, forming a prominent hemispheric asymmetry in the temperature trend structure. Together with seasonal trend patterns in the stratosphere, this indicates a possible change in stratospheric circulation.
引用
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页数:8
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