日本地球惑星科学連合2019年大会

講演情報

[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] 衛星による地球環境観測

2019年5月30日(木) 09:00 〜 10:30 302 (3F)

コンビーナ:沖 理子(宇宙航空研究開発機構)、本多 嘉明(千葉大学環境リモートセンシング研究センター)、高薮 縁(東京大学 大気海洋研究所)、松永 恒雄(国立環境研究所地球環境研究センター/衛星観測センター)、座長:鈴木 健太郎

10:00 〜 10:15

[ACG34-11] Issues in aerosol-cloud-climate interaction: Needs for future satellite mission

★Invited Papers

*鈴木 健太郎1 (1.東京大学大気海洋研究所)

キーワード:エアロゾル、雲・降水、気候モデリング、衛星観測

The aerosol forcing is the largest source of uncertainty in determining climate forcing that drives global climate change. The aerosol forcing consists of the so-called direct (aerosol-radiation interaction) and indirect (aerosol-cloud interaction) effects, both of which are subject to significant uncertainty. This uncertainty arises from our lack of understanding on key processes that govern interactions between aerosol, cloud and climate. Precipitation, among those processes, is central to the aerosol-cloud-climate interaction through its effect of depleting both clouds and aerosols. The aerosol-induced precipitation change influences the cloud lifetime and amount, whereas the precipitation change also modulates the wet removal of aerosols. This underscores a fundamental role of precipitation in shaping the aerosol-cloud-climate interaction. Recent advance in satellite observations by multiple sensors and platforms enabled us to observationally diagnose the precipitation processes on the global scale particularly, which also offers a process-level constraint on model representation of the processes. Such a “bottom-up” model constraint, however, turned out to be inconsistent with “top-down” energy balance requirement on model performance, exposing error compensations in state-of-the-art climate models at a fundamental level. This proposes that there is still a gap in our understanding of the aerosol-cloud-climate processes that hampers their reliable modeling. This presentation discusses what is required to observe in future satellite missions for filling the gap in understanding and modeling the aerosol-cloud-climate interaction. In particular, observational needs for aerosol, cloud and precipitation will be argued to better quantify aerosol-induced climate forcing in the context of recent Aerosol-Cloud-Convection-Precipitation (A-CCP) discussion emerging from the US Decadal Survey and multiple community efforts for process-oriented model diagnostics in an attempt to advance climate modeling.