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塔克拉玛干沙漠腹地晴天与沙尘暴天气大气边界层对比分析

张建涛 王敏仲 何清 王延慧 潘红林 张志新

沙漠与绿洲气象2024,Vol.18Issue(1):50-58,9.
沙漠与绿洲气象2024,Vol.18Issue(1):50-58,9.DOI:10.12057/j.issn.1002-0799.2024.01.006

塔克拉玛干沙漠腹地晴天与沙尘暴天气大气边界层对比分析

Comparative Analysis of Atmospheric Boundary Layer Between Sunny Days and Sandstorm Weather in the Hinterland of the Taklimakan Desert

张建涛 1王敏仲 1何清 2王延慧 3潘红林 1张志新4

作者信息

  • 1. 中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐 830002||新疆塔克拉玛干沙漠气象国家野外科学观测研究站,新疆乌鲁木齐 830002||中国气象局塔克拉玛干沙漠气象野外科学试验基地,新疆 乌鲁木齐 830002||新疆沙漠气象与沙尘暴重点实验室,新疆 乌鲁木齐 830002
  • 2. 新疆气象局,新疆 乌鲁木齐 830002
  • 3. 新疆气象灾害防御技术中心,新疆乌鲁木齐 830002
  • 4. 中国三峡新能源(集团)股份有限公司新疆分公司,新疆 乌鲁木齐 830000
  • 折叠

摘要

Abstract

Based on GPS sounding and ground observation data from July 2017 and 2019 in the hinterland of the Taklimakan Desert,the characteristics of atmospheric boundary layer structure changes during summer sunny days and sandstorms in the desert hinterland were compared and analyzed by using methods such as potential temperature profile.The results indicate that there are significant differences in the structural characteristics of the atmospheric boundary layer between sunny days and sandstorms.On sunny days,the vertical distribution of various meteorological elements in the atmospheric boundary layer is relatively uniform.During the day,the convective boundary layer is deep,with a height of nearly 5 000 m,and the stable boundary layer is generally around 500 m at night.During sandstorms,the vertical variation of potential temperature and specific humidity in the boundary layer is relatively small,with a high wind speed of up to 24.0 m/s.The convective boundary layer during the day is around 1 500 m,and the stable boundary layer at night is around 1 000 m.The strong radiation on sunny days,rapid surface warming,and strong turbulence are the main factors that form the deep convective boundary layer on sunny days.The dynamic conditions of cold advection in large-scale weather systems,as well as the weakening of radiation intensity reaching the surface by clouds and dust,are the main factors contributing to the unique atmospheric boundary layer structure of sandstorm weather.

关键词

大气边界层/沙尘暴/陆面过程/塔克拉玛干沙漠

Key words

atmospheric boundary layer/sandstorm/land surface process/Taklimakan desert

分类

天文与地球科学

引用本文复制引用

张建涛,王敏仲,何清,王延慧,潘红林,张志新..塔克拉玛干沙漠腹地晴天与沙尘暴天气大气边界层对比分析[J].沙漠与绿洲气象,2024,18(1):50-58,9.

基金项目

中国沙漠气象科学研究基金(Sqj2019001) (Sqj2019001)

新疆自治区杰出青年科学基金项目(2022D01E07) (2022D01E07)

国家自然科学基金(42030612) (42030612)

科技创新团队(天山创新团队)项目(2022TSYCTD0007) (天山创新团队)

沙漠与绿洲气象

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