Scenario Dependence of Future Precipitation Changes across Japan in CMIP6

IF 1.7 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
Sola Pub Date : 2024-05-22 DOI:10.2151/sola.2024-028
Michiya Hayashi, Hideo Shiogama, Noriko N. Ishizaki, Yasutaka Wakazuki
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引用次数: 0

Abstract

A bias-corrected downscaled 1-km mesh future climate dataset across Japan called NIES2020, based on five global climate models (GCMs) selected from the Coupled Model Intercomparison Project Phase 6 (CMIP6), has been used for regional impact assessments and adaptation studies under various emission scenarios. However, it is not yet revealed what determines the scenario dependence of the Japanese precipitation changes unscaled with global mean temperature changes. Here, we disentangled the inter-scenario differences in precipitation changes averaged across Japan. In the CMIP6 GCMs, the ensemble mean precipitation increases more in the mid-21st century under low-emission scenarios than higher-emission scenarios, consistent with NIES2020. In the low-emission scenarios, rapid reductions of anthropogenic aerosol emissions from East Asia enhance the surface downward shortwave radiation around Japan, promoting evaporation and precipitation. Such high precipitation sensitivity per degree of global warming is confirmed regardless of the season. In contrast, the precipitation increase is most suppressed under a high-emission scenario with weak air pollutant mitigation. Therefore, future precipitation changes across Japan are more constrained by aerosol emission changes than global warming levels, especially in the mid-21st century. This suggests climate response to air pollutant mitigations needs to be considered for implementing impact assessments and adaptation strategies in Japan.

CMIP6 中日本各地未来降水变化的情景依赖性
基于从耦合模式相互比较项目第六阶段(CMIP6)中选出的五个全球气候模式(GCMs)的一个名为 "NIES2020 "的日本全境 1 公里网格未来气候数据集经过偏差校正降尺度处理,已被用于各种排放情景下的区域影响评估和适应研究。然而,日本降水量变化与全球平均气温变化的无标度关系是如何决定的,目前尚未揭示。在此,我们分析了日本各地平均降水量变化的情景间差异。在 CMIP6 GCMs 中,低排放情景下 21 世纪中叶的集合平均降水量比高排放情景下增加得更多,这与 NIES2020 一致。在低排放情景下,东亚人为气溶胶排放的快速减少增强了日本周围的地表向下短波辐射,促进了蒸发和降水。全球变暖每升高一度对降水的高敏感性在任何季节都得到了证实。与此相反,在高排放情景下,降水增加受到的抑制最大,而空气污染物的减缓作用较弱。因此,与全球变暖水平相比,日本各地未来的降水变化更受气溶胶排放变化的制约,尤其是在 21 世纪中期。这表明,在日本实施影响评估和适应战略时,需要考虑对空气污染物减缓的气候响应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Sola
Sola 地学-气象与大气科学
CiteScore
3.50
自引率
21.10%
发文量
41
审稿时长
>12 weeks
期刊介绍: SOLA (Scientific Online Letters on the Atmosphere) is a peer-reviewed, Open Access, online-only journal. It publishes scientific discoveries and advances in understanding in meteorology, climatology, the atmospheric sciences and related interdisciplinary areas. SOLA focuses on presenting new and scientifically rigorous observations, experiments, data analyses, numerical modeling, data assimilation, and technical developments as quickly as possible. It achieves this via rapid peer review and publication of research letters, published as Regular Articles. Published and supported by the Meteorological Society of Japan, the journal follows strong research and publication ethics principles. Most manuscripts receive a first decision within one month and a decision upon resubmission within a further month. Accepted articles are then quickly published on the journal’s website, where they are easily accessible to our broad audience.
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