Moisture sources of summer heavy precipitation in two spatial patterns over Northeast China during 1979–2021

IF 2 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Shibo Yao, Xianmei Lang, Dong Si, Zhiping Tian
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引用次数: 0

Abstract

This study classifies the spatial distribution of heavy precipitation in summer (June–August) from 1979 to 2021 in the three provinces of Northeast China (TPNC) into two patterns by using the self-organizing maps (SOM) neural network, and then quantitatively analyzes their moisture transport channels and sources using the Lagrangian model. The results show that the summer heavy precipitation in TPNC can be divided into the northern and southern patterns according to the distribution of the heavy precipitation. Both patterns of heavy precipitation are affected by the low-level vortex west of TPNC, but the strength and shape of the low vortex are different. The northern pattern is mainly influenced by the westerly flow in the vortex in the mid-high latitudes, which transports moisture from the upstream westerly region into TPNC. The southern pattern is mainly affected by the southerly jet stream southeast of TPNC, which conveys a large amount of moisture from the East Asian summer monsoon region into TPNC. In terms of the summer climatological mean, the northern pattern has a higher precipitation recycling rate, while the southern pattern has a lower recycling rate.

Abstract Image

1979~2021年东北地区夏季强降水两种空间格局的水分来源
本文利用自组织图(SOM)神经网络将1979 - 2021年东北三省夏季(6 - 8月)强降水的空间分布划分为两种类型,并利用拉格朗日模型定量分析了两种类型的水汽输送通道和来源。结果表明:根据强降水的分布特征,青藏高原夏季强降水可分为南北型。两种强降水型均受到太平洋西北偏西低涡的影响,但低涡的强度和形状有所不同。北型主要受中高纬涡旋中西风气流的影响,西风气流将上游西风区的水汽输送到中高纬地区。南向型主要受太平洋东北偏南急流的影响,该急流将东亚夏季风的大量水汽输送到太平洋东北。从夏季气候平均值来看,北方模式降水再循环率较高,而南方模式降水再循环率较低。
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来源期刊
Atmospheric Science Letters
Atmospheric Science Letters METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
4.90
自引率
3.30%
发文量
73
审稿时长
>12 weeks
期刊介绍: Atmospheric Science Letters (ASL) is a wholly Open Access electronic journal. Its aim is to provide a fully peer reviewed publication route for new shorter contributions in the field of atmospheric and closely related sciences. Through its ability to publish shorter contributions more rapidly than conventional journals, ASL offers a framework that promotes new understanding and creates scientific debate - providing a platform for discussing scientific issues and techniques. We encourage the presentation of multi-disciplinary work and contributions that utilise ideas and techniques from parallel areas. We particularly welcome contributions that maximise the visualisation capabilities offered by a purely on-line journal. ASL welcomes papers in the fields of: Dynamical meteorology; Ocean-atmosphere systems; Climate change, variability and impacts; New or improved observations from instrumentation; Hydrometeorology; Numerical weather prediction; Data assimilation and ensemble forecasting; Physical processes of the atmosphere; Land surface-atmosphere systems.
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