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气象:2024,50(6):770-776
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2024年3月大气环流和天气分析
赵英珊,张涛
(国家气象中心,北京 100081)
Analysis of the March 2024 Atmospheric Circulation and Weather
ZHAO Yingshan,ZHANG Tao
(National Meteorological Centre, Beijing 100081)
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投稿时间:2024-04-28    修订日期:2024-05-15
中文摘要: 2024年3月北半球极涡呈单极偏心型分布,强度偏强;中高纬环流呈异常四波型,亚洲环流较平直。我国北方基本为500 hPa高度场负距平区域,西太平洋副热带高压较常年偏西、偏强,南支槽较常年偏弱。全国平均气温为6.0℃,较常年同期偏高1.2℃。全国平均降水量24.0 mm,较常年同期(29.4 mm)偏少18.4%,然而,内蒙古北部和西北地区中东部降水量较常年同期显著偏多。月内,发生1次大范围降雨过程;强对流天气频繁,出现3次区域性强对流过程,局地强度强;出现2次冷空气过程,降温幅度不大。此外,北方地区出现3次沙尘天气过程,西南地区冬春连旱持续。
Abstract:The main characteristics of the general atmospheric circulation in March 2024 are as follows. There was one polar vortex center in the Northern Hemisphere, which was stronger than usual. The circulation in mid-high latitudes showed an anomalous four-wave pattern, and the Asian circulation was relatively flat and straight. The northern part of China was basically in a negative anomaly zone of the 500 hPa geopotential height field. The strength of Western Pacific subtropical high was stronger and more westward than in normal years, while the south branch trough was a little weaker than usual. The monthly mean temperature was 6.0℃ across China, which is 1.2℃ warmer than normal. The monthly mean precipitation amount was 24.0 mm, 18.4% less than in normal period (29.4 mm). However,the precipitation in the north of Inner Mongolia and the east of Northwest China was significantly more than that in normal years. During this month, one large-scale precipitation process occurred, and severe convection weather appeared frequently with three regional convection events with strong localized intensities. In addition, there were two cold air processes without causing large range of drop in temperature. Three sand-dust weather processes occurred in northern China, and the drought condition continued in winter and spring in the southwestern region of China.
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基金项目:中国气象局青年创新团队(CMA2024QN05)资助
引用文本:
赵英珊,张涛,2024.2024年3月大气环流和天气分析[J].气象,50(6):770-776.
ZHAO Yingshan,ZHANG Tao,2024.Analysis of the March 2024 Atmospheric Circulation and Weather[J].Meteor Mon,50(6):770-776.