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 |
关键词 | water vapour trend Tibetan Plateau UTWV |
ISSN号 | 0899-8418 |
DOI | 10.1002/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 |
WOS记录号 | WOS:000389310400015 |
出版者 | WILEY-BLACKWELL |
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. |
入库方式: iSwitch采集
来源:寒区旱区环境与工程研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。