DOI码：10.1029/2021GL097609
发表刊物：Geophysical Research Letters
摘要：The significant climate feedback of stratospheric water vapor (SWV) necessitates quantitative estimates of SWV budget changes. Model simulations driven by the newest European Centre for Medium-Range Weather Forecast reanalysis ERA5, satellite observations from the Stratospheric Water and OzOne Satellite Homogenized data set, Microwave Limb Sounder, and in situ frost point hygrometer observations from Boulder all show substantial and persistent stratospheric moistening after a sharp drop in water vapor at the turn of the millennium. This moistening occurred mainly during 2000–2006 and SWV abundances then remained high over the last decade. We find strong positive trends in the Northern Hemisphere and weak negative trends over the South Pole, mainly during austral winter. Moistening of the tropical stratosphere after 2000 occurred during late boreal winter/spring, reached values of ∼0.2 ppm/decade, was well correlated with a warming of the cold point tropopause by ∼0.4 K/decade and can only be partially attributed to El Nino-Southern Oscillation and volcanic eruptions.
备注：Konopka, P., M. Tao, F. Ploeger, D. F. Hurst, M. L. Santee, J. S. Wright and M. Riese
论文类型：期刊论文
论文编号：e2021GL097609
学科门类：理学
一级学科：大气科学
卷号：49
期号：8
页面范围：e2021GL097609
是否译文：否
收录刊物：SCI
发布期刊链接：https://doi.org/10.1029/2021GL097609