中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Trends in upper tropospheric water vapour over the Tibetan Plateau from remote sensing

文献类型:期刊论文

作者You, Qinglong1,2,3,4,5; Jiang, Zhihong1,2,3; Bao, Yansong6,7; Pepin, Nick8; Fraedrich, Klaus5
刊名INTERNATIONAL JOURNAL OF CLIMATOLOGY
出版日期2016-12-01
卷号36期号:15页码:4862-4872
ISSN号0899-8418
关键词water vapour trend Tibetan Plateau UTWV
DOI10.1002/joc.4674
通讯作者You, Qinglong(yqingl@126.com)
英文摘要Water vapour in the upper troposphere is the dominant greenhouse gas and provides a large feedback mechanism for amplifying climate change. However, lack of high elevation observations has limited our understating of its long term variability. In this study, the homogenized time series of the upper tropospheric water vapour (UTWV) brightness temperature (BT) over the Tibetan Plateau (TP) during 1979-2012, developed through inter-satellite calibration of high-resolution infrared radiation sounder (HIRS) channel 12 clear-sky measurements, is examined. The HIRS UTWV BT above the TP is increasing (drying), with an annual rate of 0.6K decade(-1) (p<0.05), with the largest increases above the western TP. On a seasonal basis, HIRS UTWV BT shows only slight changes during 1979-1995, but rapidly increases from 1996 to 2012. Thus, drying is concentrated during recent decades, consistent with reduced water vapour flux and relative humidity. The time series of HIRS UTWV BT is correlated with a Mongolian geopotential height index at 400 hPa and the South Asian summer monsoon index derived from National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis. Thus atmospheric circulation anomalies are a control of changes in UTWV. In summer, increasing horizontal divergence at 400 hPa has suppressed the upward motion of air from the lower to the upper troposphere, reducing conveyance of sensible heat to the upper troposphere and contributing to the drying observed.
收录类别SCI
WOS关键词HIRS LONGWAVE CHANNELS ; HUMIDITY ; SATELLITE ; CLIMATOLOGY ; TEMPERATURE ; SUMMER ; MODEL ; CYCLE
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
出版者WILEY-BLACKWELL
WOS记录号WOS:000389310400015
URI标识http://www.irgrid.ac.cn/handle/1471x/2557514
专题寒区旱区环境与工程研究所
通讯作者You, Qinglong
作者单位1.NUIST, Climate Dynam Res Ctr, Nanjing, Jiangsu, Peoples R China
2.NUIST, Earth Syst Modeling Ctr, Nanjing, Jiangsu, Peoples R China
3.NUIST, Minist Educ, Key Lab Meteorol Disaster, Nanjing, Jiangsu, Peoples R China
4.Chinese Acad Sci, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou, Peoples R China
5.Max Plank Inst Meteorol, Hamburg, Germany
6.NUIST, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China
7.NUIST, China Meteorol Adm, Key Lab Aerosol Cloud Precipitat, Nanjing, Jiangsu, Peoples R China
8.Univ Portsmouth, Dept Geog, Portsmouth, Hants, England
推荐引用方式
GB/T 7714
You, Qinglong,Jiang, Zhihong,Bao, Yansong,et al. Trends in upper tropospheric water vapour over the Tibetan Plateau from remote sensing[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2016,36(15):4862-4872.
APA You, Qinglong,Jiang, Zhihong,Bao, Yansong,Pepin, Nick,&Fraedrich, Klaus.(2016).Trends in upper tropospheric water vapour over the Tibetan Plateau from remote sensing.INTERNATIONAL JOURNAL OF CLIMATOLOGY,36(15),4862-4872.
MLA You, Qinglong,et al."Trends in upper tropospheric water vapour over the Tibetan Plateau from remote sensing".INTERNATIONAL JOURNAL OF CLIMATOLOGY 36.15(2016):4862-4872.

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来源:寒区旱区环境与工程研究所

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