Reduced spread of simulated global warming patterns among CMIP6 models with accelerated pace of warming
编号:294 访问权限:仅限参会人 更新:2025-03-27 15:14:32 浏览:35次 张贴报告

报告开始:2025年04月18日 09:13(Asia/Shanghai)

报告时间:1min

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摘要
Uneven economic impacts of climate change have been largely caused by differentiated warming rates across different geographical regions, affecting the lives of the majority of worlds’ population. Historical and future warming rates are commonly obtained from global climate models, which exhibit considerable spreads in terms of global mean and region-dependent warming rates. While the multi-model spread in global mean warming rate has been widely reported in past literature, the multi-model spread in terms of global warming pattern and its temporal evolution remain unclear. Here we diagnose the CMIP6 multi-model spread in simulated surface air temperature trend in historical and future periods under different emission scenarios, in comparison with the unforced, baseline multi-model spread in the piControl experiment. This study shows that the multi-model spread in the simulated global warming pattern depends closely on the level of warming. The simulated global warming pattern deviates substantially among CMIP6 models before 1985 and converges afterwards, as the greenhouse gases level rises and global mean warming rate accelerates. Moreover, the consistency of model-predicted future warming pattern varies by emission scenario, namely the future trajectory of GHG concentrations.. Models predict highly consistent warming patterns under the high emission scenario during the entire 21st century; whereas under low and intermediate emission scenarios, future warming patterns diverge among these models around middle of the 21st century, as the predicted concentration of carbon dioxide and other GHGs declines. Besides, such multi-model spread in the simulated local warming rate shows a delayed response in the mid-to-high latitude Southern Ocean, likely attributed to the ocean circulations and ocean-atmosphere interactions that postpone the trajectory of regional surface air temperature response to global warming. While our study detects an anthropogenic signal in the temporal evolution of multi-model consistency in the global warming pattern, the physical mechanisms underlying such varying multi-model consistency in the warming pattern merits further investigation.
 
关键词
Global Warmig Patterns, Global Warming Rate, Spatial Correlation, Multi-model Spread
报告人
孟一霖
博士研究生 北京大学物理学院

稿件作者
孟一霖 北京大学物理学院
聂绩 北京大学
俞妍 北京大学
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重要日期
  • 会议日期

    04月17日

    2025

    04月21日

    2025

  • 04月10日 2025

    初稿截稿日期

  • 04月20日 2025

    注册截止日期

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中国科学院大气物理研究所
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