中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Contribution of atmospheric moisture transport to winter Arctic warming

文献类型:期刊论文

作者Hao, Mingju1,2; Luo, Yong1,2,3; Lin, Yanluan1,2; Zhao, Zongci1,2; Wang, Lei1,2; Huang, Jianbin1,2
刊名INTERNATIONAL JOURNAL OF CLIMATOLOGY
出版日期2019-04-01
卷号39期号:5页码:2697-2710
关键词Arctic atmospheric moisture content atmospheric moisture transport Polar-WRF surface air temperature surface radiation balance water cycle
ISSN号0899-8418
DOI10.1002/joc.5982
通讯作者Luo, Yong(yongluo@tsinghua.edu.cn)
英文摘要Atmospheric moisture transport (AMT) is known to have an influence on the winter Arctic surface air temperature (SAT). However, a systematic investigation involving a verification of the physical linkages and spatial sensitivity within the Arctic, as well as a quantification of such contribution is still lacking. Our work first verifies the variation coherence between AMT and the SAT over the winters of 1979-2015, based on multiple data sets. Climate model projections reveal tendencies towards more frequent high values in both SAT and AMT from 2010 to 2065 relative to that from 1950 to 2005, as well as a high correlation coefficient between their detrended series. Then, a composite analysis is applied based on different AMT values. During high-AMT episodes, enhanced AMT intrudes into the Arctic, with the Norwegian Sea as the gateway, and further induces unevenly distributed warming inside the Arctic. The greatest warming occurs in the Barents-Kara Sea, which is tightly associated with the altered atmospheric moisture content and its subsequent changes of surface radiation balance. In addition, the intruding moisture can induce latent heat release and sea ice melting, which also influences the warming. Furthermore, by conducting numerical model experiments in the winter of 2012/2013, a total warming effect of 9.66 degrees C averaged across the Arctic for the original AMT is revealed. By setting different incremental AMT values in five cases, the leading role of AMT is found to switch in the 0.5MT case (the case wherein the AMT value is 0.5 times the original) from altering the atmospheric moisture content to producing precipitation. This finding suggests that evenly spaced AMTs result in the alleviation of SAT increases.
收录类别SCI
WOS关键词SEA-ICE ; POLAR AMPLIFICATION ; POLEWARD MOISTURE ; WEATHER RESEARCH ; FORECASTING-MODEL ; LONG-TERM ; PART I ; TEMPERATURE ; IMPACT ; CLIMATE
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000467048900014
出版者WILEY
URI标识http://www.irgrid.ac.cn/handle/1471x/2555487
专题寒区旱区环境与工程研究所
通讯作者Luo, Yong
作者单位1.Tsinghua Univ, Dept Earth Syst Sci, Minist Educ, Key Lab Earth Syst Modeling, Beijing 100084, Peoples R China
2.Joint Ctr Global Change Studies, Beijing, Peoples R China
3.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryosphere Sci, Lanzhou, Gansu, Peoples R China
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Hao, Mingju,Luo, Yong,Lin, Yanluan,et al. Contribution of atmospheric moisture transport to winter Arctic warming[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2019,39(5):2697-2710.
APA Hao, Mingju,Luo, Yong,Lin, Yanluan,Zhao, Zongci,Wang, Lei,&Huang, Jianbin.(2019).Contribution of atmospheric moisture transport to winter Arctic warming.INTERNATIONAL JOURNAL OF CLIMATOLOGY,39(5),2697-2710.
MLA Hao, Mingju,et al."Contribution of atmospheric moisture transport to winter Arctic warming".INTERNATIONAL JOURNAL OF CLIMATOLOGY 39.5(2019):2697-2710.

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来源:寒区旱区环境与工程研究所

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