Atmospheric Latent Energy Transport Pathways into the Arctic and Their Connections to Sea Ice Loss during Winter over the Observational Period
文献类型:期刊论文
作者 | Liang, Yu1,2,4; Bi, Haibo1,2,3; Lei, Ruibo4,5; Vihma, Timo6; Huang, Haijun1,2 |
刊名 | JOURNAL OF CLIMATE
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出版日期 | 2023-10-01 |
卷号 | 36期号:19页码:6695-6712 |
关键词 | Arctic Sea ice Atmosphere-ocean interaction Atmospheric circulation |
ISSN号 | 0894-8755 |
DOI | 10.1175/JCLI-D-22-0789.1 |
通讯作者 | Bi, Haibo(bhb@qdio.ac.cn) ; Lei, Ruibo(leiruibo@pric.org.cn) |
英文摘要 | To investigate patterns of horizontal atmospheric latent energy (LE) transport toward the Arctic, we ap-plied the self-organizing maps (SOM) method to the daily vertically integrated horizontal LE flux from ERA5 in winter (January-March) during 1979-2021. A clear picture depicting the LE transport to the Arctic at a synoptic scale then emerged, with four primary transport pathways identified: the northern Europe, the Davis Strait, the Greenland Sea, and the Bering Strait pathways. The four primary pathways occurred at a comparable frequency, and noticeable interannual variability was observed in their time series of frequency during 1979-2021. Further analysis suggested that the northward LE transport through all these pathways is significantly modulated by cyclones, with the northern Europe and the Green -land Sea pathways being mostly affected. Generally, more frequent and stronger cyclones were observed near the entry re-gions of LE transport compared to other regions. Moreover, this study provides a comprehensive picture of how atmospheric LE transport is related to air temperature, moisture, surface heat flux, and sea ice anomalies over the Arctic Ocean in winter. Through a thermodynamic perspective, we argue that the deleterious impacts of poleward LE transport on Arctic sea ice are to a large extent attributable to the enhanced local atmosphere-ice interactions, which increase down-ward longwave radiation (DLR) plus turbulent fluxes, consequently warming the surface and promoting the loss of sea ice. According to the quantitative results, among the four primary pathways, LE transport through the Davis Strait and the Greenland Sea could cause the loss of Arctic sea ice most efficiently. |
WOS关键词 | MOISTURE TRANSPORT ; CYCLONE ACTIVITY ; POLEWARD MOISTURE ; MELT-SEASON ; VARIABILITY ; OCEAN ; SURFACE ; AMPLIFICATION ; CLIMATOLOGY ; DRIVERS |
资助项目 | Laoshan Laboratory[22XD1403600] ; Laoshan Laboratory[LSKJ202202303] ; National Natural Science Foundation of China[52192691] ; National Natural Science Foundation of China[41976219] ; General Project of Natural Science Foundation of Shandong Province[ZR2020MD100] ; Program of Shanghai Academic/Technology Research Leader[22XD1403600] |
WOS研究方向 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS记录号 | WOS:001079709700001 |
出版者 | AMER METEOROLOGICAL SOC |
源URL | [http://ir.qdio.ac.cn/handle/337002/181676] ![]() |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
通讯作者 | Bi, Haibo; Lei, Ruibo |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 4.Polar Res Inst China, Key Lab Polar Sci, MNR, Shanghai, Peoples R China 5.Zhejiang Univ, Technol & Equipment Engn Ctr Polar Observat, Zhoushan, Peoples R China 6.Finnish Meteorol Inst, Helsinki, Finland |
推荐引用方式 GB/T 7714 | Liang, Yu,Bi, Haibo,Lei, Ruibo,et al. Atmospheric Latent Energy Transport Pathways into the Arctic and Their Connections to Sea Ice Loss during Winter over the Observational Period[J]. JOURNAL OF CLIMATE,2023,36(19):6695-6712. |
APA | Liang, Yu,Bi, Haibo,Lei, Ruibo,Vihma, Timo,&Huang, Haijun.(2023).Atmospheric Latent Energy Transport Pathways into the Arctic and Their Connections to Sea Ice Loss during Winter over the Observational Period.JOURNAL OF CLIMATE,36(19),6695-6712. |
MLA | Liang, Yu,et al."Atmospheric Latent Energy Transport Pathways into the Arctic and Their Connections to Sea Ice Loss during Winter over the Observational Period".JOURNAL OF CLIMATE 36.19(2023):6695-6712. |
入库方式: OAI收割
来源:海洋研究所
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