当前位置： 首页»科研成果» 2016 谢飞、李建平与合作者在SOLA上发表论文 全球院

Fei Xie^{1, 2}, Jianping Li^{1, 2}, Wenshou Tian³, Xin Zhou^{4, 5} and Xuan Ma^1,2

 

1 College of Global Change and Earth System Science, Beijing Normal University, Beijing, China

2 Joint Center for Global Change Studies, Beijing, China

3 Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, China

4 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China

5 University of Chinese Academy of Sciences, Beijing, China

 

Abstract

The radiative and chemical interactions of stratospheric water vapour (SWV) mean that SWV has a significant influence on the climate. Based on the Stratospheric Water and OzOne Satellite Homogenized (SWOOSH) SWV data (100−1 hPa, 60°S to 60°N), variations in the middle and upper SWV are mainly investigated over the past two decades. Water vapour variations below 10 hPa are found to result from upward transport of the lower SWV.

Using empirical orthogonal function analysis and regression analysis of the anomalous upper SWV variability, it is found that upper SWV variations have an 11-year period controlled by the solar cycle as well as a 2-year cycle regulated by the quasi-biennial oscillation (QBO). Our results also show that state-of-the-art chemistry–climate models perform poorly in simulating the upper SWV variations. It is possibly because the effect of lower–middle SWV changes on the upper SWV variations is too strong in the simulations.

 

PUBLISHED BY : SOLA,  12, 127−134, doi: 10.2151/sola.2016-028

SOURCE:https://www.jstage.jst.go.jp/article/sola/12/0/12_2016-028/_article