通过高分辨率气候模式集合预测中国沿海陆地和海洋的高温、极端降水及其空间复合事件的变化

Runkai Zhang, Jinxin Zhu, Dagang Wang, Chunzhu WEI, Cong Dong
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摘要

中国沿海地区人口稠密,经济活动频繁,极易受到环境变化的影响。与其他地区相比,这些地区受到气候变化引发的极端事件的影响更为严重。气候变化最明显的影响是极端高温和极端降水。我们采用多种区域气候模式(RCMs)的组合,研究和预测了中国沿海部分陆地和海洋在历史时期(1985-2004 年)和未来时期(2080-2099 年)的气温、降水和复合热降水极端事件(CHPEs)的变化。多模式集合预测,中国沿海陆地和海洋的日极端气温将上升 2.9°C 至 5.4°C,陆地地区的气温上升幅度高于海洋地区。极端降水的地域差异很大,北纬 15-25° 海洋地区的极端降水量将减少 2.8-3.9 毫米/天,而北纬 25-35° 陆地地区的极端降水量将增加 2.2-5.4 毫米/天。我们利用克劳修斯-克拉皮隆关系揭示,日极端降水峰值将增加 2-7 毫米/天,极端降水峰值的温度将因气候变暖而升高 2°C 至 6°C。北纬 25-30° 的陆地地区降水量峰值增幅最大,为 9.87 毫米/天,温度峰值增幅为 6°C。随着日极端气温的升高,极端降水量也会增加,预计陆地和海洋地区将更频繁地出现 CHPE。与历史同期相比,未来海洋地区发生 CHPE 的频率将增加 40.9%-161.2%,陆地地区将增加 36.2%-163.6%。在两种不同的情景下,北纬 15-20° 区域的 CHPE 事件频率增加最多,而北纬 25-30° 区域的频率增加差异最大。这表明北纬 25-30 度地区更容易受到气候变化的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Projected Changes in Heat, Extreme Precipitation, and Their Spatially Compound Events over China’s Coastal Lands and Seas through a High-Resolution Climate Models Ensemble
China’s coastal lands and seas are highly susceptible to the changing environment due to their dense population and frequent economic activities. These areas experience more significant impacts from climate change-induced extreme events than elsewhere. The most noticeable effects of climate change are extreme high temperatures and extreme precipitation. We employ an ensemble of multiple RCMs (Regional Climate Models) to investigate and project changes in temperature, precipitation, and Compound Heat-Precipitation Extreme events (CHPEs) over selected China’s coastal lands and seas for both historical (1985-2004) and future periods (2080-2099). The multi-model ensemble projects that daily temperature extremes will increase by 2.9°C to 5.4°C across China’s coastal lands and seas, with land areas showing a higher temperature increase than marine areas. Extreme precipitation shows a high geographical heterogeneity with a 2.8-3.9mm/d reduction over the 15-25°N marine areas while a 2.2-5.4mm/d increment over the 25°N-35°N land areas. We use the Clausius-Clapeyron relationship to reveal that the peak of daily extreme precipitation will increase by 2-7mm/d and the temperature at which extreme precipitation peaks will increase by 2°C to 6°C by warming. The land area of 25-30°N has the highest peak precipitation increase of 9.87mm/d and a peak temperature increase of 6°C. As precipitation extremes intensify with daily temperature extremes increase, CHPEs are projected to occur more frequently over both land and marine areas. Compared with the historical period, the frequency of CHPEs will increase by 40.9%-161.2% over marine areas, and by 36.2%-163.6% over land areas in the future. The 15-20°N area has the highest frequency increase of CHPE events, and the 25-30°N area has the largest difference in frequency increase under two different scenarios. It indicated that the 25-30°N area will be more easily affected by climate change.
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