JpGU-AGU Joint Meeting 2017

講演情報

[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-AS03] [EE] 最新の大気科学:海大陸研究強化年-YMC

2017年5月21日(日) 10:45 〜 12:15 301A (国際会議場 3F)

コンビーナ:米山 邦夫(海洋研究開発機構 基幹研究領域 大気海洋相互作用研究分野)、Chidong Zhang(NOAA Pacific Marine Environmental Laboratory)、竹見 哲也(京都大学防災研究所)、座長:竹見 哲也(京都大学防災研究所)

11:15 〜 11:30

[AAS03-09] Observational study of diurnal offshore migration of precipitation area over the Indonesian Maritime Continent

*横井 覚1森 修一1勝俣 昌己1耿 驃1安永 数明1,2ファドリ シャムスディン3ヌルハヤティ ヌルハヤティ4米山 邦夫1 (1.海洋研究開発機構、2.富山大学、3.インドネシア技術評価応用庁、4.インドネシア気象気候地球物理庁)

キーワード:precipitation diurnal cycle, the Indonesian Maritime Continent, gravity waves

The Pre-YMC (Years of the Maritime Continent) field campaign conducted in the western coastal area of Sumatra Island during November and December of 2015 successfully observed typical diurnal cycle of precipitation over coastal waters characterized by nighttime offshore migration of heavy precipitation zone, with 3-hourly radiosonde soundings and weather radar at the research vessel Mirai deployed at about 50 km off the coast. Through analysis of these observational data, this study examines mechanisms responsible for the offshore migration. We find that the static stability of the offshore atmosphere decreases a couple of hours before the arrival of the precipitation zone, which is due mainly to cooling in the lower free troposphere. We further find that the cooling is due mainly to ascent motion, which is presumably a component of shallow gravity waves excited by convective systems over land. As the cooling rate is significantly correlated with offshore precipitation amount during nighttime, we can conclude that these gravity waves and the resultant destabilization play significant roles in the offshore migration of the precipitation zone via enhancement of the convective activity.