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Updated: Mar 15, 2026

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A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
Published on: April 3, 2014
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热带气旋降雨延伸到内陆地区
E Deng1, Qian Xiang2, De-Hui Ouyang1
1State Key Laboratory of Climate Resilience for Coastal Cities, Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, China.
Nature communications
|March 14, 2026
概括
热带气旋降雨正在全球范围内进一步延伸到内陆. 这一由海洋变暖带来的趋势增加了内陆沿海社区的洪水风险.
科学领域:
- 气候学 气候学 气候学
- 气象学 天气学
- 海洋学 海洋学 海洋学
背景情况:
- 热带气旋 (TC) 在海洋上的降雨强度得到了充分记录.
- 沿海地区面临着TC引起的降雨造成的洪水风险日益增加.
- 距离海岸线100公里以外的内陆地区往往没有为TC洪水做好准备.
研究的目的:
- 评估陆地热带气旋降雨的全球变化,特别是大雨事件.
- 为了确定TC降雨是否在全球范围内扩展到内陆,并量化这一趋势.
主要方法:
- 1980年至2023年全球TC降雨数据的分析.
- 统计评估大雨 (≥30毫米每3小时) 的陆地范围.
- 利用观测和模型模拟来调查导致因素.
主要成果:
- 全球TC降雨量在1980年至2023年期间扩展到内陆.
- 北半球的大陆海岸显示,每十年3.8±1.8公里的重型TC降雨量增加.
- 近岸海面温度 (SST) 的升温与这种向陆地延伸有关.
结论:
- 热带气旋大雨正在全球范围内越来越多地延伸到内陆.
- 海面温度升温和沿海城市化可能是这种现象的驱动因素.
- 在TC降雨中的陆地转移给内陆沿海人口带来了不断升级的洪水风险.
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