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闽南沿海一次海雾过程的多源资料综合分析
张伟1, 李菲1, 吕巧谊1,2, 崔梦雪3, 孙学金4,4, 陈德花1
(1.厦门市海峡气象开放重点实验室 厦门;2.厦门市气象台 厦门;3.厦门市海峡气象开放重点实验室;4.国防科技大学气象海洋学院 长沙)
Comprehensive analysis of a sea fog event in Southern coast of Fujian based on Multi-source data
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投稿时间:2022-11-01    修订日期:2023-04-12
中文摘要: 基于自动站资料、ERA5再分析资料、葵花8卫星资料、翔安站多源观测资料,分析了2021年4月1日闽南沿海一次大雾过程的环流形势、演变特征和微物理结构。结果表明本次是一次典型的海雾过程。雾形成时500 hPa为偏西-西南气流,低层为一致的西南气流与反气旋下沉气流,近地面存在逆温层和湿层,为海雾的发生发展提供静稳的环流形势和充沛的水汽条件。此次大雾过程存在雾和低云互相转化的过程。白天以低云为主,傍晚随着气温的下降和整层风速的减小,低云逐渐接地转变为雾。清晨由于偏西气流的作用,沿海的雾再次转变为低云。气溶胶激光雷达则可用于推演雾顶的高度,雾的初生和发展阶段厚度相对较低且波动性大,成熟阶段雾顶高度约为100 m。微物理参数分析表明雾过程的平均粒子数浓度为52.4 cm-3,液态水含量为0.084 g·m-3,平均直径为9.4 μm。1分钟平均粒子数浓度最大达到132.6 cm-3,液态水含量达到0.7321 g·m-3。不同阶段粒子数浓度和液态水含量的谱分布特征具有较大差异,其中数浓度的谱分布在初生、发展和消散阶段以单峰结构为主,峰值直径为4~6 μm。成熟阶段表现为双峰结构特征,主峰位于4~5 μm,次峰位于24~26 μm。液态水含量同样为双峰分布,但主峰位于24~26 μm,次峰位于5~6 μm。以上两参数谱分布特征表明雾的粒子数浓度受小粒子影响为主,但液态水含量以20~30 μm的粒子贡献最大。从发展到成熟阶段谱对比来看,20~30 μm粒子数量的增加,导致液态水含量明显增大,是导致能见度进一步下降的主要原因。
Abstract:Using observation data from automatic weather station (AWS), ERA5 reanalysis data, Himawari 8 satellite data and multi-source observation data at Xiangan Station, We analysis the circulation situation, Evolution characteristics and microphysical structure of a sea fog event in Southern Fujian Coastal Area(SFCA) on April 1th, 2021. Result shows this is a typical advection fog event. Multiple weather conditions providing the stable circulation situation and abundant water vapor conditions for the occurrence and development of sea fog, which were the west-southwest airflow at 500hPa, the low layer was controlled by consistent southwest airflow and anti-cyclonic sinking airflow, the temperature inversion layer derived from sounding. Low level cloud and sea fog change into each other during the whole event. Daytime was dominated by low level cloud while after sunset, low level cloud changes into fog with temperature dropping and wind blast. Fog changes into low level cloud while west wind dominates. Micro physical analysis shows that average fog droplet number concentration(N) was 52.4 cm-3, the average fog droplet liquid water content(LWC) was 0.084 g·m-3, the mean diameter(MD) was 9.4 μm during this event. The maximum of the average N per minute and the average LWC per minute were 132.6 cm-3 and 0.7321 g·m3. Spectrum of N and LWC at different stages exhibits quite different characteristics, which the size distribution of N was mainly a unimodal structure with the peak diameter at 4~6 μm in the preliminary, development and dissipation stages, and it was a bimodal structure with the main peak at 4~5 μm and the secondary peak at 24~26 μm of the maturity stage. In parallel to LWC, the size distribution characteristics are reversed, with the main peak at 24~26 μm and the secondary peak at 5~6 μm. It reveals that the N should dominantly influenced by small particles, the greatest influence to LWC is fog droplets of 20~30 μm. Comparative analysis of size distribution at the development and maturity stages shows that the main reason for the further deterioration of visibility should be the significant increase in LWC which led by the increase in the particle at 20~30 μm.
文章编号:202211010318     中图分类号:    文献标志码:
基金项目:厦门市科技局指导性专项(3502Z20214ZD4007),厦门市气象局海洋气象创新团队共同资助
Author NameAffiliationAddress
Zhang Wei Xiamen meteorological observatory 厦门市湖里区气象台路85号
Li Fei  厦门市湖里区气象台路85号
Lv Qiaoyi  
Cui Mengxue  
Sun Xuejin  
Chen Dehua  
引用文本:
Zhang Wei,Li Fei,Lv Qiaoyi,Cui Mengxue,Sun Xuejin,Chen Dehua,0.Comprehensive analysis of a sea fog event in Southern coast of Fujian based on Multi-source data[J].Meteor Mon,():-.
Zhang Wei,Li Fei,Lv Qiaoyi,Cui Mengxue,Sun Xuejin,Chen Dehua,0.Comprehensive analysis of a sea fog event in Southern coast of Fujian based on Multi-source data[J].Meteor Mon,():-.