Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet

Rainstorms and blizzards are common extreme weather events occurring in the eastern Tibet region. Their complex dynamic and thermodynamic mechanisms present challenges for regional meteorological research and forecasting. Based on station observation data and ERA5 atmospheric reanalysis datasets, a...

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Main Authors: Xiaotao Zhao, Lunzhu Danzeng, Qu Chi, Xulin Ma, Yuting Tan, Luozhu Duodian, Ranzhen Danzeng
Format: Article
Language:English
Published: MDPI AG 2024-12-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/16/1/30
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author Xiaotao Zhao
Lunzhu Danzeng
Qu Chi
Xulin Ma
Yuting Tan
Luozhu Duodian
Ranzhen Danzeng
author_facet Xiaotao Zhao
Lunzhu Danzeng
Qu Chi
Xulin Ma
Yuting Tan
Luozhu Duodian
Ranzhen Danzeng
author_sort Xiaotao Zhao
collection DOAJ
description Rainstorms and blizzards are common extreme weather events occurring in the eastern Tibet region. Their complex dynamic and thermodynamic mechanisms present challenges for regional meteorological research and forecasting. Based on station observation data and ERA5 atmospheric reanalysis datasets, a diagnostic analysis of the heavy rain and snow event in eastern Tibet from 24 to 27 October 2022 was conducted. The results indicate that (1) the influence of the cloud systems surrounding the Bay of Bengal storm “Sitrang” was a significant factor contributing to the occurrence of this heavy rain and snow weather. (2) Sustained stability of the southern branch trough and the western Pacific subtropical high favored the establishment and maintenance of the mid-level jet stream ahead of the storm. Storm “Sitrang” transported warm and moist air to eastern Tibet through the southwest mid-level jet stream, providing favorable moisture, dynamic, and thermal conditions for the heavy rain and snow. (3) Most importantly, symmetrical instability generated by the inclined motion of the storm’s warm and moist air emerged as the decisive mechanism driving the occurrence and development of the heavy rain and snow.
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institution Kabale University
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publisher MDPI AG
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series Atmosphere
spelling doaj-art-7c40e0137fa74afca8c21b5f40c431062025-01-24T13:21:45ZengMDPI AGAtmosphere2073-44332024-12-011613010.3390/atmos16010030Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern TibetXiaotao Zhao0Lunzhu Danzeng1Qu Chi2Xulin Ma3Yuting Tan4Luozhu Duodian5Ranzhen Danzeng6Key Laboratory of Meteorological Disaster, Ministry of Education/International Joint Research Laboratory of Climate and Environment Change, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaMeteorological Observatory of Tibet Autonomous Region, Lhasa 850000, ChinaMeteorological Observatory of Tibet Autonomous Region, Lhasa 850000, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education/International Joint Research Laboratory of Climate and Environment Change, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education/International Joint Research Laboratory of Climate and Environment Change, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaMeteorological Observatory of Tibet Autonomous Region, Lhasa 850000, ChinaMeteorological Observatory of Tibet Autonomous Region, Lhasa 850000, ChinaRainstorms and blizzards are common extreme weather events occurring in the eastern Tibet region. Their complex dynamic and thermodynamic mechanisms present challenges for regional meteorological research and forecasting. Based on station observation data and ERA5 atmospheric reanalysis datasets, a diagnostic analysis of the heavy rain and snow event in eastern Tibet from 24 to 27 October 2022 was conducted. The results indicate that (1) the influence of the cloud systems surrounding the Bay of Bengal storm “Sitrang” was a significant factor contributing to the occurrence of this heavy rain and snow weather. (2) Sustained stability of the southern branch trough and the western Pacific subtropical high favored the establishment and maintenance of the mid-level jet stream ahead of the storm. Storm “Sitrang” transported warm and moist air to eastern Tibet through the southwest mid-level jet stream, providing favorable moisture, dynamic, and thermal conditions for the heavy rain and snow. (3) Most importantly, symmetrical instability generated by the inclined motion of the storm’s warm and moist air emerged as the decisive mechanism driving the occurrence and development of the heavy rain and snow.https://www.mdpi.com/2073-4433/16/1/30cyclonic storm “Sitrang” over the Bay of Bengalheavy rain and snowmoist potential vorticitywater vapor transport
spellingShingle Xiaotao Zhao
Lunzhu Danzeng
Qu Chi
Xulin Ma
Yuting Tan
Luozhu Duodian
Ranzhen Danzeng
Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
Atmosphere
cyclonic storm “Sitrang” over the Bay of Bengal
heavy rain and snow
moist potential vorticity
water vapor transport
title Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
title_full Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
title_fullStr Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
title_full_unstemmed Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
title_short Impact of Cyclonic Storm “Sitrang” over the Bay of Bengal on Heavy Rain and Snow in Eastern Tibet
title_sort impact of cyclonic storm sitrang over the bay of bengal on heavy rain and snow in eastern tibet
topic cyclonic storm “Sitrang” over the Bay of Bengal
heavy rain and snow
moist potential vorticity
water vapor transport
url https://www.mdpi.com/2073-4433/16/1/30
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