日本地球惑星科学連合2018年大会

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[EE] 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-AS02] 大規模な水蒸気場と組織化した雲システム

2018年5月22日(火) 13:45 〜 15:15 301B (幕張メッセ国際会議場 3F)

コンビーナ: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(富山大学都市デザイン学部)、横井 覚(海洋研究開発機構、共同)、佐藤 正樹(東京大学大気海洋研究所)、座長:三浦 裕亮

13:45 〜 14:00

[AAS02-01] Idealized simulations of convective organization and moisture buildup during South China Sea monsoon onset

★Invited Papers

*Chien-Ming Wu1Wei-Ming Tsai1Yen-Kai Huang1Wei-Ting Chen1 (1.National Taiwan University)

キーワード:cloud resolving model, organized convection, cloud tracking

The moisture development over South China Sea (SCS) plays an essential role in modulating the timing of summer monsoon onset. This moisture development is generally associated with the increasing number of organized convection over SCS. In this study, idealized simulations are designed to evaluate the causal relationship between the moisture buildup and organized convection using a vector vorticity equation cloud-resolving model (VVM). The results show that the topography surrounding SCS is important in geographical locking the coastal convection over SCS. In addition, when the diurnal convection is strong over land, strong subsidence occurs and the convection is suppressed over the ocean with random isolated deep convection. When the vertical wind shear is imposed, mimicking the change of large-scale circulation during onset, organized coastal convection develops and propagates toward the center of SCS. A critical column water vapor is therefore reached with the moisture transport of the propagating convection and possibly causes the onset of the SCS monsoon. An object-based tracking algorithm is developed to further examine the characteristics of organized convection. Preliminary results suggest that these propagating systems tend to be smaller in size with longer lifetime compared to the geographically locked coastal convection. The role of cold pool in these convective systems is also evaluated.