首页|气候变化对中国本世纪中叶热浪、静稳及其复合事件的影响

气候变化对中国本世纪中叶热浪、静稳及其复合事件的影响

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热浪、静稳及其复合事件(简称复合热稳)的发生可加剧空气污染,损害人体健康.基于动力降尺度方法和两种共享社会经济路径(Shared socioeconomic pathways,SSPs),本研究利用区域模式模拟并探究了中国历史时期(2000-2019年)和本世纪中叶(2050-2069年)SSPs情景下的气候和极端天气的变化.相较于全球模式,区域模式对2 m气温和边界层高度的模拟偏差显著降低94%和85%,并再现了极端天气的空间分布.在类似碳中和的SSP1-2.6情景下,本世纪中叶中国热浪和复合热稳总天数相比历史时期分别增加31%和35%;而在以使用化石燃料为主的SSP5-8.5情景下,两者平均增幅达74%和85%.与SSP1-2.6情景相比,SSP5-8.5情景下热浪等单一极端天气和复合热稳增加更为显著,因此减少化石燃料使用并实现碳中和政策目标,能有效缓解极端天气特别是复合极端天气的增加.
Impacts of Climate Change on Heat Waves,Atmospheric Stagnation and Their Compound Events in China
The occurrence of heat waves,atmospheric stagnation and their compound events(referred to as compound heat wave and atmospheric stagnation)can exacerbate air pollution and harm human health.Based on the dynamical downscaling method and two shared socioeconomic pathways(SSPs),this study uses a regional model to simulate and explore the changes in climate and weather extremes under the SSPs scenarios for China's historical period(2000-2019)and mid-century(2050-2069).Compared with the global model,the regional model significantly reduces the simulation bias of 2 m temperature and boundary layer height by 94%and 85%,and reproduces the spatial distribution of ex-treme weather.Under the carbon-neutral-like SSP1-2.6 scenario,the total number of heat wave and compound heat wave and atmospheric stagnation event days in mid-century China increases by 31%and 35%,respectively,compared with the historical period;while under the fossil fuel-dominated SSP5-8.5 scenario,the average increase of the two reaches 74%and 85%.The increase in single extremes such as heat waves and compound heat wave and atmospheric stagnation events are more pronounced in the SSP5-8.5 scenario than in the SSP1-2.6 scenario,and therefore reducing fossil fuel use and achieving carbon neutral policy goals can effectively mitigate the increase in extremes,especially compound ex-tremes.

climate changeheat wavescompound heat wave and atmospheric stagnation eventsnu-merical modellingdynamical downscaling

曲炳霖、高阳

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中国海洋大学深海圈层与地球系统前沿科学中心海洋环境与生态教育部重点实验室,山东青岛 266100

气候变化 热浪 复合热稳事件 数值模拟 动力降尺度

2025

中国海洋大学学报(自然科学版)
中国海洋大学

中国海洋大学学报(自然科学版)

北大核心
影响因子:0.474
ISSN:1672-5174
年,卷(期):2025.55(2)
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