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河西走廊东部西北气流型沙尘暴的大气物理特征

杨梅 李岩瑛 罗晓玲 杨吉萍 聂羽彗 聂鑫

沙漠与绿洲气象2024,Vol.18Issue(3):121-128,8.
沙漠与绿洲气象2024,Vol.18Issue(3):121-128,8.DOI:10.12057/j.issn.1002-0799.2024.03.016

河西走廊东部西北气流型沙尘暴的大气物理特征

Atmospheric Physical Characteristics of Northwest Airflow Type Sandstorm in the East of Hexi Corridor

杨梅 1李岩瑛 2罗晓玲 1杨吉萍 3聂羽彗 3聂鑫4

作者信息

  • 1. 武威市气象局,甘肃 武威 733000||武威国家气候观象台,甘肃 武威 733000
  • 2. 武威市气象局,甘肃 武威 733000||中国气象局兰州干旱气象研究所,甘肃 兰州 730020
  • 3. 民勤县气象局,甘肃 民勤 733300
  • 4. 中国气象局兰州干旱气象研究所,甘肃 兰州 730020
  • 折叠

摘要

Abstract

Based on the conventional high altitude,ground observation data and encrypted observation data with interval of 50 m at 08:00 and 20:00 of Minqin station in the east of Hexi Corridor from 2006 to 2022,the surface time variations of meteorological elements,characteristics of vertical structure and atmospheric stratification were analyzed.The results showed that:(1)The northwest airflow type sandstorm occurred when ground-air temperature and temperature difference were maximum,relative humidity was minimum,surface air pressure and wind speed increased sharply.Especially in spring,the sandstorm occurred with big wind,dry surface and strong thermal convection near surface layer.(2)The vertical structure was dry in the morning but wet in the evening,the wind speed increased with height,the wind direction turned clockwise and then reversed,the lower layer was warm and the upper layer was cold.The lower layer air temperature was higher,vertical gradient increased greatly,T-Td was bigger,intensity of cold-warm air was stronger and intersection height(near 1 km)in spring,the stratification was more unstable and sandstorms were prone to occur.(3)The bigger vertical gradient of potential temperature resulted more unstable atmosphere at 08:00 in spring and 20:00 in winter,so sandstorm appeared earlier in the day in spring.There were deeper and lower unstable stratification heights at 20:00 in spring and 08:00 in winter,so the strong sandstorm often concentrated from afternoon to night in spring and noon in winter.(4)When the center strength of cold advection(≥-34℃)and northwest jet stream(≥26 m/s)were stronger at 500 hPa,and the corresponding wind speed was greater than 20.0 m/s at 700 hPa over Hexi and the larger area of lower warm zone,the stronger the intensity and the longer the duration of the sandstorm.

关键词

西北气流型沙尘暴/地面要素/垂直结构/大气层结

Key words

morthwest airflow type sandstorm/ground elements/vertical structurel/atmospheric stratification

分类

天文与地球科学

引用本文复制引用

杨梅,李岩瑛,罗晓玲,杨吉萍,聂羽彗,聂鑫..河西走廊东部西北气流型沙尘暴的大气物理特征[J].沙漠与绿洲气象,2024,18(3):121-128,8.

基金项目

国家自然科学基金面上项目(41975015) (41975015)

武威市市列科技项目(WW2101101) (WW2101101)

沙漠与绿洲气象

OACSTPCD

2097-6801

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