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-OS 海洋科学・海洋環境

[A-OS10] Atlantic climate variability, and its global impacts and predictability

2019年5月30日(木) 10:45 〜 12:15 105 (1F)

コンビーナ:Ingo Richter(JAMSTEC Japan Agency for Marine-Earth Science and Technology)、時長 宏樹(九州大学応用力学研究所)、Noel S Keenlyside(Geophysical Institute Bergen)、Carlos R Mechoso(University of California Los Angeles)、座長:Ingo Richter時長 宏樹(京都大学白眉センター)

11:45 〜 12:00

[AOS10-11] Generation mechanisms of the Benguela Nino with a focus on local amplification

*東塚 知己1小林 諒1 (1.東京大学大学院理学系研究科地球惑星科学専攻)

キーワード:沿岸ニーニョ、南大西洋、経年変動、セントヘレナ高気圧、アンゴラ低気圧

Benguela Nino is associated with positive sea surface temperature (SST) anomalies off the west coast of Angola and Namibia in the South Atlantic. Although both local and remote forcing have been indicated to contribute to the development of Benguela Nino, the reason why their relative contribution varies among the events has not been clarified. Thus, the generation mechanisms of the Benguela Nino are investigated in this study by categorizing the events into locally amplified and non-locally amplified events depending on whether alongshore wind anomalies contribute to the development of the Benguela Nino. It is found that the locally events are associated with alongshore northerly wind anomalies related to anomalous weakening of the subtropical anticyclone in the South Atlantic known as St. Helena High and the continental low named Angola Low. On other hands, no alongshore wind anomalies that favor the development of SST anomalies exist in the non-locally amplified events. A mixed layer heat budget analysis reveals that the surface heat flux term is greater in the locally amplified events owing to smaller latent heat release associated with the weakening of the climatological southerly winds, while the anomalous warming by the advection term is stronger in the non-locally amplified events.