作者:KunXin Wang,YinSheng Zhang,Ning Ma,YanHong Guo,YaoHui Qiang
摘要:Land surface actual evapotranspiration is an important process that influences the Earth's energy and water cycles and determines the water and heat transfer in the soil-vegetation-atmosphere system.Meanwhile,the cryosphere's hydrological process is receiving extensive attention,and its water problem needs to be understood from multiple perspectives.As the main part of the Chinese cryosphere,the Tibetan Plateau faces significant climate and environmental change.There are active interaction and pronounced feedback between the environment and ETa in the cryosphere.This article mainly focuses on the research progress of ETa in the Tibetan Plateau.It first reviews the ETa process,characteristics,and impact factors of typical underlying surfaces in the Tibetan Plateau(alpine meadows,alpine steppes,alpine wetlands,alpine forests,lakes).Then it compares the temporal and spatial variations of ETa at different scales.In addition,considering the current greening of cryosphere vegetation due to climate change,it discusses the relationship between vegetation greening and transpiration to help clarify how vegetation activities are related to the regional water cycle and surface energy budget.
发文机构:Key Laboratory of Tibetan Environment Changes and Land Surface Processes University of Chinese Academy of Sciences CAS Center for Excellence in Tibetan Plateau Earth Sciences Key Laboratory of Water Cycle and Related Land Surface Processes State Key Laboratory of Cryospheric Science China-Pakistan Joint Research Center on Earth Sciences
关键词:cryosphereevapotranspirationTibetanPlateauTRANSPIRATIONEVAPORATION
分类号: D67[政治法律—中外政治制度]