日本地球惑星科学連合2023年大会

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セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS07] 大気化学

2023年5月22日(月) 09:00 〜 10:15 展示場特設会場 (2) (幕張メッセ国際展示場)

コンビーナ:坂本 陽介(京都大学大学院地球環境学堂)、内田 里沙(一般財団法人 日本自動車研究所)、石戸谷 重之(産業技術総合研究所)、岩本 洋子(広島大学大学院統合生命科学研究科)、座長:入江 仁士(千葉大学環境リモートセンシング研究センター)、石戸谷 重之(産業技術総合研究所)、内田 里沙(一般財団法人 日本自動車研究所)

09:45 〜 10:00

[AAS07-04] 2010年代の中国SLCFs排出量変動が東アジア・全球気候に与える影響

*須藤 健悟1,2、王 靖凌1 (1.名古屋大学大学院環境学研究科地球環境科学専攻、2.海洋研究開発機構)

キーワード:短寿命気候影響物質、二酸化硫黄、気候変動、化学気候モデル、中国排出量

This study investigates the temperature and precipitation changes (especially in East Asia) from 2012 to 2019 under the scenario of emission reduction due to China's emission reduction policies using the chemistry-climate model CHASER (MIROC) with the Chinese emission inventory MEIC. Our model simulation reveals that influences of the rapid SO2 emission reduction and increases in well-mixed greenhouse gases (WMGHG) cause regionally different changes in temperature and precipitation in East Asia exhibiting almost opposite change patterns for SO2 and WMGHG influences. The model calculates a significant increase in temperature in eastern China and its eastern seas, Japan, and other regions with also a large precipitation increase near Japan, but a decrease in precipitation in eastern China and adjacent seas. For both surface temperature and precipitation, the decrease in Chinese SO2 emission has the same magnitude of impact as the increase in WMGHGs, suggesting the important role of Chinese SO2 reduction in the decadal climate change in the 2010s. The simulation shows that the precipitation changes due to a decrease in SO2 and an increase in WMGHG are both attributed to the induced large-scale changes in atmospheric circulation and cloud distribution in East Asia. Our additional simulation shows that the solo impact of SO2 reduction on surface temperature may be confined within South Asia and China, but this may be largely amplified by the coinciding NOx reduction in China to give very significant warming in North China to Mongolia and Russia. Furthermore, we also found that the global pattern of surface temperature changes during the 2010s can be also well attributed to the reduction in SO2 emissions in China, indicating a potentially large contribution of regional SO2 and aerosol emissions to global climate change. Interannual variation in biomass burning emissions and other anthropogenic emission changes (for BC/OC/NH3) which are not treated in this study should be examined as well as for SO2/NOx.
By investigating the impact of China's emission reduction policies like in this study, we can detect that while the policy has effectively curbed the deterioration of air quality, it has indeed brought about significant changes in precipitation in the surrounding region and contributed to climate change in East Asia and the globe, which may further lead to extreme weather events such as droughts and high temperatures. In addition, this modeling exercise can be good training for chemistry-climate models that target SLCFs impacts.