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天山北坡一次区域性暴雪形成机制及水汽输送特征

万瑜 魏娟娟 李伟 仇会民

沙漠与绿洲气象2024,Vol.18Issue(3):9-16,8.
沙漠与绿洲气象2024,Vol.18Issue(3):9-16,8.DOI:10.12057/j.issn.1002-0799.2024.03.002

天山北坡一次区域性暴雪形成机制及水汽输送特征

Mechanism and Water Vapor Transport Characteristics of a Regional Snowstorm in the North Slope of Middle Tianshan Mountains

万瑜 1魏娟娟 1李伟 1仇会民2

作者信息

  • 1. 新疆气象台,新疆 乌鲁木齐 830002
  • 2. 巴音郭楞蒙古自治州气象局,新疆 库尔勒 841000
  • 折叠

摘要

Abstract

Based on the conventional observation data at high altitude and ground,NCEP/NCAR reanalysis data,the characteristics and causes of snowstorm process in the north slope of middle Tianshan Mountains on February 2017 were diagnosed and analyzed.Combined with GDAS reanalysis data and HYSPLIT model,the water vapor source,main water vapor transport channels and their contribution to water vapor transport were simulated and tracked.The results show that the stable confrontation of warm and cold advection and strong frontal zone provide stable synoptic scale condition for the snowstorm when the regional snowstorm occurs.The continuous cold cushion uplift in the middle and lower layers is the main dynamic mechanism,the coupling of high and low jet streams stimulates the mesoscale vertical ascending branch and secondary circulation has an increasing effect on snowstorm.The main water vapor sources of snowstorm are located in the Red Sea on the west side of Arabian Peninsula and Persian Gulf to the north of Arabian Sea on the southwest side of Iranian Plateau.The water vapor channel is mainly concentrated in 500-850 hPa,and the water vapor convergence area is located in 700-850 hPa.There is southwest airflow in the middle and upper layers,westerly airflow in the middle layer and northwest jet stream in the lower layer to relay water vapor to snowstorm area.By use of HYSPLIT model,it is found that water vapor input in the west and north boundaries which plays an important role during the snowstorm.The main water vapor transport channels are westward path,southwestern path and local water vapor path,their contribution rates are roughly equal at 1 500 m height tracking,and local water vapor and westward path have greater contribution rates at 3 000 m height.

关键词

区域性暴雪/动力机制/HYSPLIT模式/水汽输送

Key words

regional snowstorm/dynamical mechanism/HYSPLIT model/water vapor transportation

分类

天文与地球科学

引用本文复制引用

万瑜,魏娟娟,李伟,仇会民..天山北坡一次区域性暴雪形成机制及水汽输送特征[J].沙漠与绿洲气象,2024,18(3):9-16,8.

基金项目

新疆科技厅自然科学计划面上项目(2021D01A151) (2021D01A151)

新疆气象局面上项目(MS202314) (MS202314)

沙漠与绿洲气象

OACSTPCD

2097-6801

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