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基于FY-4A的庐山云海特征及其成因研究

陈勇 段婧 王新 郭强 张小鹏

气象学报2023,Vol.81Issue(6):973-984,12.
气象学报2023,Vol.81Issue(6):973-984,12.DOI:10.11676/qxxb2023.20220188

基于FY-4A的庐山云海特征及其成因研究

Identifying the seas of clouds around Mt.Lu based on FY-4A satellite observations:Formation and sustenance

陈勇 1段婧 2王新 3郭强 3张小鹏4

作者信息

  • 1. 中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室,北京,100029
  • 2. 中国气象局云降水物理与人工影响天气重点开放实验室,北京,100081
  • 3. 国家卫星气象中心(国家空间天气监测预警中心)/中国遥感卫星辐射测量和定标重点开放实验室/许健民气象卫星创新中心,北京,100081
  • 4. 庐山气象局,九江,332900
  • 折叠

摘要

Abstract

The characteristics,recognition and formation of seas of clouds(SOC)around Mt.Lu are studied based on FY-4A observations and other data.From 2019 to 2021,19 events of SOCs are recorded in the dataset,including 12 traditional SOCs(TSOC)and 7 small-scale SOCs with cloud waterfalls over Mt.Lu(SSOC).The FY-4A visible-channel cloud image can identify the area and development of TSOC but cannot capture the detailed structure of SSOC.The L2 cloud-top-height product of FY-4A can be used for the recognition of TSOC around Mt.Lu but cannot be used for the recognition except of SSOC.Normally the wake phenomena of SOC(WSOC)occur on islands over the sea,but three WSOC events are found in Mt.Lu,although it is located in the land.The WSOC in Mt.Lu exhibits a comma-type cloud pattern with regular fluctuations but without continuous vortexes.The formation of the WSOC in Mt.Lu is mainly caused by the isolated ellipse shape of Mt.Lu,the northernly low-level jet,and the temperature inversion layer below the mountain top.Besides,for most SOC events,Mt.Lu is under the control of high-pressure systems and located in high-humidity region,where the synoptic-scale subsidence inversion layer and sufficient moisture could play an important role in the forming and maintenance of SOCs over Mt.Lu.

关键词

庐山/云海/FY-4A/可见光/尾流

Key words

Mt.Lu/Sea of cloud/FY-4A/Visible channel/Wake phenomena

分类

天文与地球科学

引用本文复制引用

陈勇,段婧,王新,郭强,张小鹏..基于FY-4A的庐山云海特征及其成因研究[J].气象学报,2023,81(6):973-984,12.

基金项目

国家自然科学基金项目(42175109、41675137)、中国气象局重点创新团队(CMA2022ZD10). (42175109、41675137)

气象学报

OA北大核心CSCDCSTPCD

0577-6619

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