CCPortal
DOI10.1016/j.earscirev.2021.103625
Warming amplification over the Arctic Pole and Third Pole: Trends, mechanisms and consequences
You Q.; Cai Z.; Pepin N.; Chen D.; Ahrens B.; Jiang Z.; Wu F.; Kang S.; Zhang R.; Wu T.; Wang P.; Li M.; Zuo Z.; Gao Y.; Zhai P.; Zhang Y.
发表日期2021
ISSN0012-8392
卷号217
英文摘要Warming amplification over the Arctic Pole (AP hereafter) and Third Pole (Tibetan Plateau, TP hereafter) can trigger a series of climate responses and have global consequences. Arctic amplification (AA) and Tibetan amplification (TA) are the most significant characteristics of climate change patterns over the two Poles. In this study, trends, mechanisms and consequences of both AA and TA are compared. Based on ERA5 reanalysis during 1979–2020, both AP and TP have undergone significant warming with an annual rate of 0.72 °C/decade and 0.34 °C/decade respectively, which exceeds the rates for the Northern Hemisphere (0.29 °C/decade) and the global means (0.19 °C/decade) over the same period. Based on 22 Coupled Model Intercomparison Project Phase 6 models, AA over the AP is warming at a rate almost four times than the global means and twice as fast over the TP. Although both AA and TA are projected to continue in the future, currently there is no consensus on the dominant mechanisms for AA or TA over the two Poles. Proposed mechanisms of AA can be divided into two types: local climate factors (sea ice-albedo feedback, Planck feedback, temperature gradient feedback, cloud feedback, and water vapor feedback); and poleward heat and moisture transport from lower latitudes (atmospheric circulation effect, ocean circulation effect, and modulation of Pacific and Atlantic SST). Consequences of AA include decline of sea ice cover, retreat of the Greenland ice sheet, permafrost degradation, accelerated disturbances in marine and terrestrial ecosystems, and influences on extreme climate events at lower latitudes. Anthropogenic greenhouse gas emission, snow/ice-albedo feedback, cloud-radiation interactions, water vapor and radiative flux feedbacks, local forcing and feedback processes, land use changes and reduction in total ozone, are generally considered to be the main mechanisms causing TA. TA has caused significant change within the atmosphere and cryosphere over the TP and its surroundings, such as changes in climate extremes, snow cover, the retreat of glaciers, and permafrost degradation. Similarities and differences of warming amplifications over the two Poles are proposed, and the relative contribution of each mechanism to the warming amplifications and how the specific consequences may compare over the two Poles remain unclear and under continuing investigation. © 2021 Elsevier B.V.
英文关键词Arctic amplification; Arctic Pole; Physical mechanisms; Third Pole; Tibetan amplification
语种英语
scopus关键词climate change; climate modeling; greenhouse gas; ice cover; ice sheet; land use change; Northern Hemisphere; regional climate; sea ice; snow cover; trend analysis; warming; Arctic; Greenland; Greenland Ice Sheet
来源期刊EARTH-SCIENCE REVIEWS
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/209321
作者单位Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, Shanghai, 200438, China; Innovation Center of Ocean and Atmosphere System, Zhuhai Fudan Innovation Research Institute, Zhuhai, 518057, China; Department of Geography, University of PortsmouthPO1 3HE, United Kingdom; Department of Earth Sciences, University of Gothenburg, Gothenburg, S-405 30, Sweden; Institute for Atmospheric and Environmental Sciences, Goethe-Universitaet Frankfurt am Main, Frankfurt/Main, D-60438, Germany; Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science and Technology, Nanjing, 210044, China; State Key Laboratory of Cryospheric Science, Chinese Academy of Sciences (CAS), Lanzhou, 730000, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China; National Climate Center, China Meteorological Administration, Beijing, 100081, China; Tianjin Institute of Meteorological Science, Tianjin, 300074, Chin...
推荐引用方式
GB/T 7714
You Q.,Cai Z.,Pepin N.,et al. Warming amplification over the Arctic Pole and Third Pole: Trends, mechanisms and consequences[J]. 中国科学院青藏高原研究所,2021,217.
APA You Q..,Cai Z..,Pepin N..,Chen D..,Ahrens B..,...&Zhang Y..(2021).Warming amplification over the Arctic Pole and Third Pole: Trends, mechanisms and consequences.EARTH-SCIENCE REVIEWS,217.
MLA You Q.,et al."Warming amplification over the Arctic Pole and Third Pole: Trends, mechanisms and consequences".EARTH-SCIENCE REVIEWS 217(2021).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[You Q.]的文章
[Cai Z.]的文章
[Pepin N.]的文章
百度学术
百度学术中相似的文章
[You Q.]的文章
[Cai Z.]的文章
[Pepin N.]的文章
必应学术
必应学术中相似的文章
[You Q.]的文章
[Cai Z.]的文章
[Pepin N.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。