首页|期刊导航|Advances in Polar Science|Characteristics and formation mechanisms of Arctic amplification: progress, challenges and ways forward

Characteristics and formation mechanisms of Arctic amplification: progress, challenges and ways forwardOA

中文摘要

In recent decades, the Arctic has experienced persistent warming, with near-surface warming three to four times higher than the global average, accompanied by the melting of sea ice, snow cover, and ice sheets. This anomalous warming phenomenon is referred to as Arctic amplification(referred to as AA). With the recent advances in AA research, significant understanding has been developed regarding its temporal evolution, spatial distribution, and influencing mechanisms. However, controversies remain concerning the primary drivers of AA, the quantitative contributions of various drivers, and some of the underlying processes. This paper synthesizes recent research findings, revisiting the spatiotemporal characteristics of AA and its driving factors, and analyzes the influencing mechanisms from four perspectives, including albedo feedback, temperature feedback, aerosol–water vapor–cloud feedback, and poleward energy transport via ocean and atmosphere circulation. Existing studies are summarized to several major conclusions, including: AA is characterized by a short emergence time(appearing in the last ~40 years), a strong influence from underlying surface properties, albeit with significant seasonal variations;AA is influenced by a combination of drivers both within and outside the Arctic, and the interactions among these factors are highly complex, preventing a conclusive, overarching understanding of the formation mechanisms from being established. We suggest that future research would benefit from the following three key foci:(1) enhancing studies on the impacts of land surface albedo feedback, aerosols, the Atlantic Meridional Overturning Circulation, and stratospheric processes on AA;(2) optimizing parameterizations of cloud–aerosol and land surface processes in climate and Earth system models, and integrating sea ice drift dynamics into these models;and(3) investigating the interactive mechanisms among various driving factors from a holistic perspective.

YANG Yundi;WANG Xuejia;OU Tinghai;WANG Tao;PANG Guojin;GOU Xiaohua;Hans W.LINDERHOLM

Key Laboratory of Western China’s Environmental Systems(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,ChinaKey Laboratory of Western China’s Environmental Systems(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China Gansu Liancheng Forest Ecosystem Field Observation and Research Station,Lanzhou University,Lanzhou 730000,ChinaRegional Climate Group,Department of Earth Sciences,University of Gothenburg,Gothenburg 40530,SwedenCollege of Atmospheric Sciences,Lanzhou University,Lanzhou 730000,ChinaFaculty of Geomatics,Lanzhou Jiaotong University,Lanzhou 730070,ChinaKey Laboratory of Western China’s Environmental Systems(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China Gansu Liancheng Forest Ecosystem Field Observation and Research Station,Lanzhou University,Lanzhou 730000,ChinaRegional Climate Group,Department of Earth Sciences,University of Gothenburg,Gothenburg 40530,Sweden

天文与地球科学

Arctic amplificationsea ice meltingalbedo feedbacktemperature feedbackpoleward energy transportAtlantic Meridional Overturning Circulationatmospheric and oceanic circulation

《Advances in Polar Science》 2026 (2)

P.102-122,21

funded by the Fundamental and Interdisciplinary Disciplines Breakthrough Plan of the Ministry of Education of China (Grant no. JYB2025XDXM910)the National Natural Science Foundation of China (Grant no. 42477483)the Start-up Funds for Introduced Talent at Lanzhou University (Grant no. 561120217)supported by the Swedish Research Council (Vetenskapsradet, 2021-03866)supported by the Supercomputing Center of Lanzhou University,China。

10.12429/j.advps.2026.0023

评论