日本地球惑星科学連合2014年大会

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

[A-CG37_28AM2] 熱帯におけるマルチスケール大気海洋相互作用現象

2014年4月28日(月) 11:00 〜 12:31 423 (4F)

コンビーナ:*名倉 元樹((独) 海洋研究開発機構)、長谷川 拓也(独立行政法人海洋研究開発機構)、清木 亜矢子(海洋研究開発機構)、東塚 知己(東京大学大学院理学系研究科地球惑星科学専攻)、時長 宏樹(ハワイ大学国際太平洋研究センター)、大庭 雅道(電力中央研究所 環境科学研究所 大気海洋環境領域)、今田 由紀子(東京大学大気海洋研究所)、座長:名倉 元樹((独) 海洋研究開発機構)、清木 亜矢子(海洋研究開発機構)

11:40 〜 11:55

[ACG37-03] Observed moisture variations associated with shallow convection

*BELLENGER Hugo1KATSUMATA Masaki1YONEYAMA Kunio1NISHIZAWA Tomoaki2YASUNAGA Kazuaki3SHIROOKA Ryuichi1 (1.JAMSTEC、2.NIES、3.University of Toyama)

キーワード:Convection, moisture, MJO, CINDY/DYNAMO, preconditionning, observation

The variability of tropospheric moisture is a key feature of tropical climate. In particular, the importanceof moisture variations due to convective transport is still to be quantified on a variety of spatial andtemporal scales. For instance, there is a debate on the importance of moisture convective transport inpreconditioning the atmosphere prior to deep convection development associated with the Madden--Julian Oscillation (MJO). We use here high frequency observations of humidity and convection in theIndian Ocean by lidars and radars on board the R/V Mirai during the CINDY/DYNAMO campaign.Significant moisture variations on the scale of few hours are observed within the first first kilometers ofthe atmosphere in association with shallow convective and congestus clouds. We then compare theselocal tendencies with large--scale ones and discuss the potential importance of convective transport byconvection in the moisture budget during the transition from convectively suppressed to convectivelyactive periods.