[1]National Meteorological Information Center, China Meteorological Administration, Beijing 100081, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[3]Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081, China;
[4]University of Chinese Academy of Sciences, Beijing 100049, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[5]Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing 100081, China;
[6]International Centre for Integrated Mountain Development, Kathmandu 3226, Nepal;
[7]Department of Meteorology, Tri-Chandra Campus, Tribhuvan University, Kathmandu 3226, Nepal;
[5]Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing 100081, China;
[8]Indian Institute of Tropical Meteorology, Pune 411008, India;
[1]National Meteorological Information Center, China Meteorological Administration, Beijing 100081, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[5]Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing 100081, China;
[9]College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044, China;
[9]College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044, China;
[1]National Meteorological Information Center, China Meteorological Administration, Beijing 100081, China;
Climate; change; Trend; Extreme; precipitation; events; HKH; region; Tibetan; Plateau;