Remarkable pattern of global warming in ocean heat content
编号:227 访问权限:仅限参会人 更新:2024-10-10 22:51:11 浏览:177次 张贴报告

报告开始:2025年01月16日 17:50(Asia/Shanghai)

报告时间:15min

所在会场:[S23] Session 23-Sea Level Rise: Understanding, Observing, and Modelling [S23-P] Sea Level Rise: Understanding, Observing, and Modelling

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摘要
Huge heat anomalies in the past few years are not explained by climate models.  Strong characteristic patterns in temperatures for upper layers of the ocean occurred from 2000 to 2023 in the presence of global warming from increasing atmospheric greenhouse gases.  Here we show that the deep tropics are warming, although sharply modulated by El Niño-Southern Oscillation events, with strong heating in the extratropics near 40°N and 40 to 45°S, but little heating near 20°N and 25-30°S.  The heating is most clearly manifested in zonal mean ocean heat content and is evident in sea surface temperatures.  Strongest heating is in the Southern Hemisphere, where aerosol effects are small.  Estimates are made of the contributions of top-of-atmosphere (TOA) radiation, atmospheric energy transports, surface fluxes of energy, and redistribution of energy by surface winds and ocean currents.  The patterns are not directly related to TOA radiation but are strongly evident in net surface energy fluxes.  Changes in the atmospheric circulation, jet streams, and storm tracks are reflected in surface ocean Ekman transports.  As well as climate change, natural variability is likely in play. Hence the atmosphere and ocean currents are systematically redistributing heat from global warming, profoundly affecting local climates.
关键词
ocean heat, ocean warming, climate, pattern
报告人
Lijing Cheng
Professor Institute of Atmospheric Physics, Chinese Academy of Sciences

稿件作者
Lijing Cheng Institute of Atmospheric Physics, Chinese Academy of Sciences
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重要日期
  • 会议日期

    01月13日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 01月17日 2025

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
承办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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