A new paradigm of internal wave in the Arctic Ocean  

作　　者：LI Qun 

机构地区：[1]MNR Key Laboratory for Polar Science,Polar Research Institute of China,Shanghai 200136,China [2]Ocean Academy,Zhejiang University,Zhoushan 316021,China

出　　处：《Advances in Polar Science》2025年第1期1-4,共4页极地科学进展(英文版)

基　　金：supported by the National Natural Science Foundation of China(Grant no.42176244);CAS Key Deployment Project of Centre for Ocean Mega-Research of Science(Grant no.COMS2020Q07)。

摘　　要：In the Arctic Ocean,turbulent mixing drives vertical heat flux,thereby affecting the sea ice variability.Internal wave is regarded as one of the important energy sources of mixing in this region.The high latitude and sea ice cover make internal wave in the Arctic Ocean apparently differs from that in mid-and low-latitude oceans.However,the internal wave and its underlying mechanism are less understood due to the lack of observations.This paper briefly reviews the recent studies and unresolved questions on the internal wave in the Arctic Ocean,including wind-driven near-inertial wave,internal tide,and high-frequency internal wave.The aim is to provide new insights for in-depth research in the future,with a focus on the mechanisms responsible for the evolution of internal wave under the rapidly changing Arctic climate.

关 键 词：internal wave turbulent mixing Arctic Ocean sea ice TIDE 

分 类 号：P73[天文地球—海洋科学]