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2023年内蒙古一次区域性强沙尘暴气象成因及来源分析OA

Meteorological cause and source analysis of regional strong sandstorm in Inner Mongolia in 2023

中文摘要英文摘要

利用 2023 年3 月 21-22 日内蒙古各站高空和地面常规观测资料、NCEP/NCAR和ERA5 再分析资料,分析了此次沙尘暴天气的成因.同时,结合呼和浩特站PM10浓度数据,运用HYSPLIT 模式、潜在源贡献因子分析法和浓度权重轨迹分析法,探讨了其沙尘潜在来源并量化了源区贡献率.结果表明:本次区域性强沙尘暴主要影响系统为强烈发展的蒙古气旋,沙尘暴区呈涡旋状自西向东延伸,与气旋中心移动路径关系密切.位于内蒙古不同地区发生沙尘天气的剧烈程度不同,气象要素变化程度也不尽相同,能见度和PM10浓度与地面风速具有非常好的反(正)相关关系.东移南下的300 hPa 极锋急流是造成本次强沙尘暴的主要高空动力系统,强沙尘暴发生的时间地点、强度、移动路径与急流的入侵时间、强度、轴位置有密切关系.次级环流的上升支将沙尘卷扬至高空,下沉支一方面将其在下游地区释放,另一方面使得高空急流动量下传至地面,加大地面风速,使沙尘暴天气强度升级.深厚混合层是本次沙尘暴对流层中低层的重要层结特征.本次强沙尘天气过程中,内蒙古沙尘主要贡献区为新疆北部沙漠、蒙古国西南部荒漠以及内蒙古中西部偏北地区荒漠,其主要沿东南路径对下游北京和河北省造成影响.

Based on the observation data of upper air and ground at various stations in Inner Mongolia from March 21 to 22,2023,NCEP/NCAR and ERA5 reanalysis data,the causes of the strongest sandstorm weather in Inner Mongolia in the past six years were analyzed.Combined with PM10 concentration data at Hohhot station,HYSPLIT model,potential source contribution factor analysis and concentration weighted trajectory analysis were used to ana-lyze the potential sources of dust and quantify the contribution rate of source areas.The results show that the main influence system of this regional strong sandstorm is the Mongolian cyclone with strong development,and the sand-storm area extends from west to east in a vortex shape,which is closely related to the moving path of the cyclone center.The severity of sandstorm weather in different areas of Inner Mongolia is different,and the change degree of meteorological elements is also different.Visibility and PM10 concentration have a very good inverse(positive)cor-relation with wind speed.The 300 hPa polar front jet moving eastward and southward is the main high-altitude dy-namic system that caused the severe sandstorm.The time,place,intensity and moving path of the severe sandstorm are closely related to the invasion time,intensity and axis position of the jet.On the one hand,the ascending branch of the secondary circulation lifts the dust into the upper air,while the descending branch releases it in the down-stream area,on the other hand,it makes the upper air jet flow down to the ground,increases the ground wind speed,and upgrades the dust storm weather intensity.The deep mixed layer is an important stratification feature in the middle and lower troposphere.During this heavy dust weather,the main contribution areas of dust sources are the desert in northern Xinjiang,the desert in southwestern Mongolia and in the north part of central and western In-ner Mongolia,which mainly passes through central Inner Mongolia along the southeast path and then affects Bei-jing and Hebei Province.

王慧清;姜艳丰;裴浩;张凯霞;吴拥军;徐洋

内蒙古自治区气象台,内蒙古 呼和浩特 010051内蒙古气象科学研究所,内蒙古 呼和浩特 010051内蒙古自治区气象局,内蒙古 呼和浩特 010051锡林浩特国家气候观象台,内蒙古锡林浩特 026000东乌珠穆沁旗气象局,内蒙古锡林郭勒 026300那仁宝力格气象站,内蒙古锡林郭勒 011408

天文与地球科学

强沙尘暴PM10潜在源区沙尘贡献率

Strong sandstormPM10Potential sourcesDust contribution rate

《气象与环境学报》 2026 (1)

75-84,10

内蒙古自治区自然科学基金项目(2025MS04039、2025LHMS04007)和内蒙古自治区科技计划项目(2025YFDZ0054)共同资助.

10.3969/j.issn.1673-503X.2026.01.008

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