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Laboratory of Meteorological Disaster (KLME), Ministry of Education &amp; Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science &amp; Technology","award":["KLME202203"],"award-info":[{"award-number":["KLME202203"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Recent years have witnessed contrasting trends in summer total rainfall (STR) over the Tibetan Plateau (TP), with an increase in the northern and a decrease in the southern TP. This study identifies four significant centers of rainfall trends: eastern TP (\u201cregion A\u201d), Qiangtang Plateau (\u201cB\u201d), Qaidam Basin (\u201cC\u201d), and the northern foothills of the Himalayas (\u201cD\u201d). Heavy rainfall dominates STR trends in regions A and D, accounting for 55.6% and 52.0%, respectively. In region B, moderate and light rainfall contribute almost equally, accounting for 37.3% and 44.8% of the STR trend, respectively. Region C is primarily influenced by light rainfall, explaining 71.2% of the STR trend. Notably, the contributions of different rainfall intensities to STR in each region vary annually, with region A experiencing more heavy rainfall, region B having moderate dominance but less light rainfall, and region C and D showing reduced and increased light rainfall contributions, respectively. Mechanistically, the strengthening of the upper-level westerly jet and the South Asian High, coupled with changes in moisture transport and convective available potential energy, collectively cause variations in rainfall intensity, characterizing the spatial heterogeneity in STR in the TP.<\/jats:p>","DOI":"10.3390\/rs15235587","type":"journal-article","created":{"date-parts":[[2023,12,1]],"date-time":"2023-12-01T04:12:56Z","timestamp":1701403976000},"page":"5587","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":2,"title":["Spatial Heterogeneity of Summer Rainfall Trends over the Tibetan Plateau Contributed by Different Rainfall Intensities"],"prefix":"10.3390","volume":"15","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-9808-8658","authenticated-orcid":false,"given":"Meirong","family":"Wang","sequence":"first","affiliation":[{"name":"Joint Center for Data Assimilation Research and Applications\/Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)\/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD)\/Joint International Research Laboratory of Climate and Environment Change (ILCEC), School of Atmospheric Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China"},{"name":"State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China"}]},{"given":"Xiuping","family":"Yao","sequence":"additional","affiliation":[{"name":"China Meteorological Administration Training Center, Beijing 100081, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7359-1647","authenticated-orcid":false,"given":"Jun","family":"Wang","sequence":"additional","affiliation":[{"name":"International Institute for Earth System Science, Nanjing University, Nanjing 210033, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7606-8747","authenticated-orcid":false,"given":"Boqi","family":"Liu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China"}]},{"given":"Zhu","family":"Zhu","sequence":"additional","affiliation":[{"name":"Joint Center for Data Assimilation Research and Applications\/Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)\/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD)\/Joint International Research Laboratory of Climate and Environment Change (ILCEC), School of Atmospheric Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China"}]},{"given":"Shunwu","family":"Zhou","sequence":"additional","affiliation":[{"name":"Joint Center for Data Assimilation Research and Applications\/Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)\/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD)\/Joint International Research Laboratory of Climate and Environment Change (ILCEC), School of Atmospheric Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China"}]},{"given":"Jiashuang","family":"Yuan","sequence":"additional","affiliation":[{"name":"National Climate Center, Beijing 100081, China"}]}],"member":"1968","published-online":{"date-parts":[[2023,11,30]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"180","DOI":"10.2151\/jmsj1923.35A.0_180","article-title":"1957 Large-scale aspects of the summer monsoon in South and East Asia","volume":"35","author":"Flohn","year":"1957","journal-title":"J. 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