首页|Resonance between projected Tibetan Plateau surface darkening and Arctic climate change
Resonance between projected Tibetan Plateau surface darkening and Arctic climate change
扫码查看
点击上方二维码区域,可以放大扫码查看
原文链接
NETL
NSTL
万方数据
The Tibetan Plateau(TP)exerts a profound influence on global climate over million-year timescales due to its past uplift.However,whether the ongoing climate changes over the TP,particularly the persistent reduction in its local albedo(referred to as"TP surface darkening"),can exert global impacts remains elu-sive.In this study,a state-of-the-art coupled land-atmosphere global climate model has been employed to scrutinize the impact of TP darkening on polar climate changes.Results indicate that the projected TP darkening has the potential to generate a stationary Rossby wave train,thereby modulating the atmo-spheric circulation in the high-latitudes of the Northern Hemisphere and instigating a dipole-like surface air temperature anomaly pattern around the Arctic region.An additional experiment suggests that the projected Arctic warming may in return warm the TP,thus forming a bi-directional linkage between these two climate systems.Given their association with vast ice reservoirs,the elucidation of this mech-anism in our study is crucial in advancing our comprehension of Earth system climate projections.
Shuchang Tang、Shilong Piao、David M.Holland、Fei Kan、Tao Wang、Tandong Yao、Xichen Li
展开 >
Sino-French Institute for Earth System Science,College of Urban and Environmental Sciences,Peking University,Beijing 100871,China
State Key Laboratory of Tibetan Plateau Earth System,Resources and Environment,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China
Courant Institute of Mathematical Sciences,New York University,New York,NY 0711,USA
Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China
展开 >
Second Tibetan Plateau Scientific Expedition and Research ProgramNational Natural Science Foundation of ChinaXplorer Prize