Characteristics of orographic clouds and associated mechanisms in the Qilian Mountains, northeastern Tibetan Plateau based on FengYun-4A satellite TBB product

IF 4.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Yi Chang , Qianrong Ma , Peng Qi , Xueliang Guo , Dawei Lin , Lijun Guo , Di Di , Yang Zhao , Hui Wang , Tianyu Chen
{"title":"Characteristics of orographic clouds and associated mechanisms in the Qilian Mountains, northeastern Tibetan Plateau based on FengYun-4A satellite TBB product","authors":"Yi Chang ,&nbsp;Qianrong Ma ,&nbsp;Peng Qi ,&nbsp;Xueliang Guo ,&nbsp;Dawei Lin ,&nbsp;Lijun Guo ,&nbsp;Di Di ,&nbsp;Yang Zhao ,&nbsp;Hui Wang ,&nbsp;Tianyu Chen","doi":"10.1016/j.atmosres.2025.108031","DOIUrl":null,"url":null,"abstract":"<div><div>The Qilian Mountains (QM) in northwest China is a key source of orographic cloud formation, significantly influencing regional weather, climate, and hydrological balance. However, due to the sparse distribution of ground-based observational stations, the characteristics of orographic clouds and their associated precipitation remain insufficiently understood. Utilizing FengYun-4A black body temperature (TBB) data from 2018 to 2021 in boral summer, this study investigated the spatial and diurnal characteristics of orographic clouds and associated mechanisms over the QM. Results indicate that orographic clouds primarily form over the mountainous terrain, with deep convective clouds concentrated in the central and eastern QM. A distinct diurnal cycle is observed, with peak cloud activity occurring in the afternoon to early evening (15:00–19:00 local solar time), minimal activity late at night, and the weakest development in the morning. These variations are more pronounced in the central and eastern QM, where cloud formation persists for longer durations, compared to the western region. Three dominant diurnal cloud cycles are identified in the southeast, northeast, and eastern fringes of the western, central, and eastern QM, respectively, along with smaller-scale cycles along mountain ridges. Orographic cloud formation is driven by the convergence of low-level westerlies and the Asian monsoon, with moisture contributions from the westerlies, the Tibetan Plateau, and the monsoon system. Additionally, interactions between solar heating and complex terrain shape the spatial and diurnal distribution of these clouds. These findings enhance our understanding of regional water cycles and provide valuable insights for weather and climate research.</div></div>","PeriodicalId":8600,"journal":{"name":"Atmospheric Research","volume":"320 ","pages":"Article 108031"},"PeriodicalIF":4.5000,"publicationDate":"2025-03-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169809525001231","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0

Abstract

The Qilian Mountains (QM) in northwest China is a key source of orographic cloud formation, significantly influencing regional weather, climate, and hydrological balance. However, due to the sparse distribution of ground-based observational stations, the characteristics of orographic clouds and their associated precipitation remain insufficiently understood. Utilizing FengYun-4A black body temperature (TBB) data from 2018 to 2021 in boral summer, this study investigated the spatial and diurnal characteristics of orographic clouds and associated mechanisms over the QM. Results indicate that orographic clouds primarily form over the mountainous terrain, with deep convective clouds concentrated in the central and eastern QM. A distinct diurnal cycle is observed, with peak cloud activity occurring in the afternoon to early evening (15:00–19:00 local solar time), minimal activity late at night, and the weakest development in the morning. These variations are more pronounced in the central and eastern QM, where cloud formation persists for longer durations, compared to the western region. Three dominant diurnal cloud cycles are identified in the southeast, northeast, and eastern fringes of the western, central, and eastern QM, respectively, along with smaller-scale cycles along mountain ridges. Orographic cloud formation is driven by the convergence of low-level westerlies and the Asian monsoon, with moisture contributions from the westerlies, the Tibetan Plateau, and the monsoon system. Additionally, interactions between solar heating and complex terrain shape the spatial and diurnal distribution of these clouds. These findings enhance our understanding of regional water cycles and provide valuable insights for weather and climate research.
求助全文
约1分钟内获得全文 求助全文
来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信