日本地球惑星科学連合2021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-AS 大気科学・気象学・大気環境

[A-AS01] 大規模な水蒸気場と組織化した雲システム

2021年6月4日(金) 15:30 〜 17:00 Ch.07 (Zoom会場07)

コンビーナ:横井 覚(海洋研究開発機構)、三浦 裕亮(国立大学法人 東京大学大学院 理学系研究科 地球惑星科学専攻)、濱田 篤(富山大学)、佐藤 正樹(東京大学大気海洋研究所)、座長:濱田 篤(富山大学)、横井 覚(海洋研究開発機構)

15:30 〜 15:45

[AAS01-07] A numerical study on precipitation over the western coastal area of Sumatra Island

★Invited Papers

*安永 数明1、奥川 椋介1、濱田 篤1 (1.富山大学)

キーワード:海洋大陸

It has been documented that significant amounts of tropical precipitation are concentrated in coastal areas, which is especially prominent over the western coast of Sumatra Island. We conducted 14-day-long numerical simulations, focusing on precipitation patterns around Sumatra Island. In the control experiment, the rainfall concentration was obscure, and dry biases were found. Based on the budget equation of the column-integrated frozen moist static energy (which is nearly equivalent to the column-integrated moisture under the weak temperature gradient assumption), we formulated 9 sensitivity experiments. When the terminal velocity and effective radius of ice clouds were reduced in addition to incorporating the warmer sea surface temperature (SST) around the coast, the model showed better rainfall peak fidelity. On the other hand, similar diurnal cycles of precipitation were simulated in the sensitivity tests without any conspicuous peaks in the coastal region, which indicated that the precipitation concentration fidelity was irrelevant to that of the diurnal cycle. An analysis in the time-mean fields demonstrated that inhibition of radiative cooling (associated with the upper-level ice clouds) and warmer SSTs induced anomalous updrafts, and thus, more moisture and precipitation were brought to the coast by enhancement of the vertical moisture advection. Comparing the simulation results with in situ observations, we speculated that together with the climatologically warmer SSTs, the SST diurnal cycle and lateral transport of ice clouds from inland convection, which was strictly regulated by solar insolation, significantly contributed to the precipitation concentration around the coastal region.