Satellite altimeter observed surface water increase across lake-rich regions of the Arctic  

作　　者：Nan Xu Wenyu Li Peng Gong Hui Lu 

机构地区：[1]College of Geography and Remote Sensing,Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources,Hohai University,Nanjing 210098,China [2]Department of Geography and Planning,University of Toronto,Toronto,ON M5S 3G3,Canada [3]Department of Geography,Department of Earth Science,University of Hong Kong,Hong Kong 999077,China [4]Department of Earth System Science,Ministry of Education Key Laboratory for Earth System Modeling,Institute for Global Change Studies,Tsinghua University,Beijing 100084,China [5]State Key Laboratory of Hydroscience and Engineering,Tsinghua University,Beijing 100084,China [6]Tsinghua University(Department of Earth System Science)-Xi’an Institute of Surveying and Mapping Joint Research Center for Next-Generation Smart Mapping,Beijing 100084,China

出　　处：《The Innovation》2024年第6期29-30,共2页创新（英文）

基　　金：supported by the National Natural Science Foundation of China(42101343);the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0206);the Natural Science Foundation of Jiangsu Province(BK20240258).

摘　　要：On our planet,the Arctic region has numerous and widely distributed lakes.These lakes are fundamental components of regional water cycles,carbon cycles,and the energy balance and also play a crucial role in providing habitats for wildlife,maintaining biodiversity,and supplying freshwater.According to satellite observations,in situ measurements,and climate models,the Arctic is the fastest-warming region on Earth.

关 键 词：ARCTIC WARMING Earth 

分 类 号：P33[天文地球—水文科学]