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协调大集合模拟下全球海表面温度对北极对流层早冬增暖的影响

Lutao Wang Yongqi Gao Dong Guo Tao Wang Ying Zhang Wei Hua

大气和海洋科学快报(英文版)2021,Vol.14Issue(1):57-62,6.
大气和海洋科学快报(英文版)2021,Vol.14Issue(1):57-62,6.

协调大集合模拟下全球海表面温度对北极对流层早冬增暖的影响

Impact of global sea surface temperature on the recent early winter Arctic tropospheric warming in coordinated large ensemble simulations

Lutao Wang 1Yongqi Gao 2Dong Guo 3Tao Wang 4Ying Zhang 2Wei Hua5

作者信息

  • 1. School of Atmospheric Science, Chengdu University of Information Technology, Chengdu, China
  • 2. Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing China
  • 3. Nansen Environmental and Remote Sensing Center and Bjerknes Centre for Climate Research, Bergen, Norway
  • 4. Climate Change Research Center, Chinese Academy of Sciences, Beijing, China
  • 5. Joint Laboratory for Climate and Environmental Change, Chengdu University of Information Technology, Chengdu, China
  • 折叠

摘要

Abstract

Coordinated numerical ensemble experiments with six different state-of-the-art atmosphere models were used to evaluate and quantify the impact of global SST (from reanalysis data) on the early winter Arctic warming during 1982-2014.Two sets of experiments were designed: in the first set (EXP1),OISSTv2 daily sea-ice concentration and SST variations were used as the lower boundary forcing,while in the second set (EXP2) the SST data were replaced by the daily SST climatology.In the results,the multi-model ensemble mean of EXP1 showed a nearsurface (~850 hPa) warming trend of 0.4 ℃/10 yr,which was 80% of the warming trend in the reanalysis.The simulated warming trend was robust across the six models,with a magnitude of 0.36-0.50 ℃/10 yr.The global SST could explain most of the simulated warming trend in EXP1 in the mid and low troposphere over the Arctic,and accounted for 58% of the simulated near-surface warming.The results also suggest that the uppertropospheric warming (~200 hPa) over the Arctic in the reanalysis is likely not a forced signal;rather,it is caused by natural climate variability.The source regions that can potentially impact the early winter Arctic warming are explored and the limitations of the study are discussed.

关键词

北极增暖/海表面温度/多模式协调试验/E-P通量/行星波

Key words

Arctic warming/Sea surface temperature/Multi-model coordinated experiment/Eliassen-Palm flux/Planetary wave

引用本文复制引用

Lutao Wang,Yongqi Gao,Dong Guo,Tao Wang,Ying Zhang,Wei Hua..协调大集合模拟下全球海表面温度对北极对流层早冬增暖的影响[J].大气和海洋科学快报(英文版),2021,14(1):57-62,6.

基金项目

This work was supported by the National Key R&D Program of China[grant number 2017YFE0111800]and the National Natural Science Foundation of China[grant numbers 41790472 and 41661144005].The second author was also partly supported by the EU H2020 Blue-Action project[grant number 727852]. ()

大气和海洋科学快报(英文版)

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1674-2834

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