Influence of Early Spring Arctic Sea Ice on Midsummer Precipitation in Northeast China: The Intermediate Links and Temporal-Spatial Channels

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Dian Yuan, Er Lu
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引用次数: 0

Abstract

Previous studies revealed that the Arctic sea ice in March can influence the July–August (JA) precipitation over northeast China (NEC). We are curious about what happens in the atmosphere during the intermediate months of April, May, and June. In this study, we use atmospheric heat source as an intermediate quantity to link the sea ice and precipitation, and aim to find the intermediate stations where atmospheric heat source can well link to both March Arctic sea ice and the JA precipitation in NEC. The stations can appear in different locations and different intermediate months. Lagged correlations are calculated to infer the response of the heat source to sea ice and the response of precipitation to the heat source. Results show that there exist two spatial-temporal channels. The first is a direct path over high latitudes, with intermediate station appearing in April at a location between Arctic and NEC. The second is a circuitous path, with intermediate station appearing in June over the equatorial Indian Ocean, which can excite a wave train that finally affects the JA precipitation in NEC. The influence of March Arctic sea ice on the JA precipitation in NEC can be contributed jointly by these two temporal-spatial channels.

早春北极海冰对中国东北仲夏降水的影响:中间环节和时空通道
以往的研究表明,3月北极海冰对中国东北地区7 - 8月降水具有一定的影响。我们很好奇在四月、五月和六月中间的几个月里大气中发生了什么。本研究以大气热源作为海冰与降水联系的中间量,旨在寻找大气热源与3月北极海冰和东北地区JA降水都能很好联系的中间站。监测站可以出现在不同的位置和不同的中间月份。通过计算滞后相关性来推断热源对海冰的响应和降水对热源的响应。结果表明,存在两个时空通道。第一种是高纬度地区的直接路径,中间站出现在4月份北极和NEC之间的位置。第二种是迂回路径,6月在赤道印度洋上空出现中间站,可以激发波列,最终影响东北地区的JA降水。3月北极海冰对东北地区JA降水的影响可以由这两个时空通道共同贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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