日本地球惑星科学連合2025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-AS 大気科学・気象学・大気環境

[A-AS08] 湿潤大気の多様な現象

2025年5月28日(水) 10:45 〜 12:15 展示場特設会場 (6) (幕張メッセ国際展示場 7・8ホール)

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)、高須賀 大輔(東北大学大学院理学研究科)、濱田 篤(富山大学)、横井 覚(海洋研究開発機構)、座長:高須賀 大輔(東北大学大学院理学研究科)、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)

10:45 〜 11:00

[AAS08-07] The March 2023 MJO and Its Impacts on the Subsequent Coastal El Niño

★Invited Papers

*Yuntao Wei1 (1.Fudan University)

キーワード:MJO, Convective initiation, Equatorial waves, Coastal El Niño

The year 2023 has witnessed sequential geneses of a record-breaking Madden–Julian oscillation (MJO) and an unprecedented coastal El Niño in March–April, thus offering another opportunity to further understand the dynamics of MJO–El Niño interactions. Here, we show that the March 2023 MJO is quite unusual as it starts from the South China Sea due to the dry intrusion of extratropical cold northerly winds and moist preconditioning effects of equatorial Rossby waves, propagates eastward fast as a double Kelvin wave system, and expands over the entire tropical Pacific largely as a Kelvin wave response to its strong suppressed convection over the Maritime Continent. Because of these unusual features, the MJO exerts widespread westerly wind forcing to the ocean surface, with two maxima over the western and far eastern tropical Pacific. Due mainly to the depressed local Ekman upwelling under MJO westerly, the upper ocean gets warmer than normal near the coast of South America, thereby helping trigger the 2023 coastal El Niño. Using an El Niño ensemble forecasting system, we quantify that the MJO westerly over the far eastern Pacific explains approximately 30% of coastal warming signals off Peru. Although only marginally increasing the end-of-year Niño-3.4 index, the March MJO can induce small-scale oceanic westward-propagating disturbances, which significantly decrease the intermember spread of the forecasted basin-scale 2023/24 El Niño. These results highlight the pivotal importance of tropical–extratropical interactions in initiating those MJOs from outside the Indian Ocean and also point out the potential roles of MJOs in dynamical El Niño evolution and prediction.