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Reduced Wind Power on Oceanic Near-Inertial Internal Waves in a Warming Climate
编号：514 访问权限：仅限参会人 更新：2026-08-31 16:59:03 浏览：0次 张贴报告

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摘要
Wind power on oceanic near-inertial internal waves (WI) is one of the major energy sources to sustain ocean turbulent diapycnal mixing. However, its response to global warming remains poorly understood. Using a high-resolution climate simulation that simulates WI reasonably well, we show that under a high-emission scenario, the quasi-globally (5{degree sign}-60{degree sign} latitudes) integrated WI exhibits a significant negative trend of -5.1×10-2 TW per century during 2001-2100, decreasing by about 13% by the end of the 21st century compared to its present level. This decline is driven by reduced near-inertial wind stress variance, primarily due to weakened mid-latitude storm activities resulting from a poleward shift of storm tracks in both hemispheres and weakening of storm tracks in the Northern Hemisphere. Our findings suggest that near-inertial internal waves should likely weaken in a warming climate, with important implications for ocean turbulent diapycnal mixing.
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报告人
Shuyi Huang
Ocean University of China

稿件作者
Shuyi Huang Ocean University of China
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重要日期

  • 会议日期

    01月12日

    2027

    至

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

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