The impact of warm and moist atmospheric flow on the record minimum Arctic sea ice extent in July 2020
编号:1709 稿件编号:1307 访问权限:仅限参会人 更新:2021-06-16 14:30:53 浏览:675次 口头报告

报告开始:2021年07月10日 17:37 (Asia/Shanghai)

报告时间:12min

所在会议:[S16A] 16A、冰冻圈科学 » [S16A-1] 16A、冰冻圈科学-1

暂无文件

摘要
The satellite observations unveiled that the July sea ice extent of the Arctic shrank to the lowest value in 2020 since 1979, with a major ice retreat in the Eurasian shelf seas including Kara, Laptev, and East Siberian Seas. Based on the ERA-5 reanalysis products, we explored the impacts of warm and moist air-mass transport on this extreme event. The results reveal that anomalously high energy and moisture converged into these regions in the spring months (April to June) of 2020, leading to a burst of high moisture content and warming within the atmospheric column. The convergence is accompanied by local enhanced downward longwave radiation and turbulent fluxes, which is favorable for initiating an early melt onset in the areas with severe ice loss. Once the melt begins, solar radiation played a decisive role in leading to further sea ice depletion due to ice-albedo positive feedback. The typical trajectories of the synoptic cyclones that occurred on the Eurasian side in spring 2020 agree well with the path of atmospheric flow. Assessments suggest that variations in characteristics of the spring cyclones are conducive to the severe melt of sea ice. We argue that large-scale atmospheric circulation and synoptic cyclones act in concert to trigger the exceptional poleward transport of total energy and moisture from April to June to cause this new record minimum of sea ice extent in the following July.
 
关键字
sea ice extent
报告人
梁钰
中科院海洋研究所

稿件作者
梁钰 中科院海洋研究所
发表评论
验证码 看不清楚,更换一张
全部评论
登录 会议管理 酒店预订 提交摘要