[1]Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing 100081, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[1]Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing 100081, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[3]College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044, China;
[4]International Centre for Integrated Mountain Development, Kathmandu 3226, Nepal;
[3]College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044, China;
[5]National Meteorological Information Center, China Meteorological Administration, Beijing 100081, China;
[6]Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081, China;
[7]Department of Meteorology, Tri-Chandra Campus, Tribhuvan University, Kathmandu 3226, Nepal;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
[2]Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China;
Climate; change; Temperature; Precipitation; Trend; Hindu; Kush; Himalayan; Tibetan; Plateau;