日本地球惑星科学連合2022年大会

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[E] 口頭発表

セッション記号 A (大気水圏科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG34] Climate Variability and Predictability on Subseasonal to Multidecadal Timescales

2022年5月25日(水) 09:00 〜 10:30 201A (幕張メッセ国際会議場)

コンビーナ:森岡 優志(海洋研究開発機構)、コンビーナ:Murakami Hiroyuki(Geophysical Fluid Dynamics Laboratory/University Corporation for Atmospheric Research)、那須野 智江(国立研究開発法人 海洋研究開発機構)、コンビーナ:Zhang Liping(NOAA GFDL Princeton)、Chairperson:Hiroyuki Murakami(Geophysical Fluid Dynamics Laboratory/University Corporation for Atmospheric Research)、那須野 智江(国立研究開発法人 海洋研究開発機構)


09:30 〜 09:45

[ACG34-03] Substantial Global Influence of Anthropogenic Aerosols on Tropical Cyclones over the Last 40 Years

*Hiroyuki Murakami1 (1.Geophysical Fluid Dynamics Laboratory/University Corporation for Atmospheric Research)

キーワード:Anthropogenic aerosols, Tropical cyclone, Climate modeling

Several studies to date have demonstrated a substantial impact of aerosols on regional tropical cyclone (TC) activity. However, it is not yet clear how changes in anthropogenic aerosols, such as sulfate, have altered and will change global TC activity. Indeed, over the last 40 years, anthropogenic aerosols have been significantly decreasing over Europe and the United States owing to pollution control measures, whereas they have increased in South and East Asia because of the economic and industrial growth in these regions. In this study, we applied climate model simulations by imposing the changes in global anthropogenic aerosols over the last 40 years and uncovered a substantial global impact of anthropogenic aerosols on the spatial distributions of TCs. Specifically, the decreases in aerosols over Europe and the United States have contributed to significant decreases in TCs over the Southern Hemisphere as well as increases in TCs over the North Atlantic, whereas the increases in aerosols in South and East Asia have exerted substantial decreases in TCs over the western North Pacific. These global-scale simulated changes in TCs are a result of the global changes in large-scale circulations imposed by the changes in anthropogenic aerosols. These results highlight that how we control emissions of anthrophonic aerosols in the future, as well as greenhouse gases, will exert a substantial impact on the world’s TC activity.