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
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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 |
DOI | 10.1002/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 |
推荐引用方式 GB/T 7714 | 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. |
入库方式: iSwitch采集
来源:寒区旱区环境与工程研究所
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