日本地球惑星科学連合2023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-CG 大気海洋・環境科学複合領域・一般

[A-CG33] 熱帯におけるマルチスケール大気海洋相互作用

2023年5月23日(火) 13:45 〜 15:15 104 (幕張メッセ国際会議場)

コンビーナ:堀井 孝憲(国立研究開発法人海洋研究開発機構)、釜江 陽一(筑波大学生命環境系)、清木 亜矢子(海洋研究開発機構)、時長 宏樹(九州大学応用力学研究所)、座長:堀井 孝憲(国立研究開発法人海洋研究開発機構)、時長 宏樹(九州大学応用力学研究所)

14:10 〜 14:30

[ACG33-02] Multi-year ENSO: impact, mechanisms, and predictability

★Invited Papers

*岩切 友希1,2渡部 雅浩1 (1.東京大学大気海洋研究所、2.気象研究所)

キーワード:ENSO

El Niño–Southern Oscillation (ENSO) events occasionally recur one after the other in the same polarity, called multi-year ENSO. Multi-year La Niña brings different climate impacts over Japan, and therefore understanding mechanisms and predictability are important. We found that multi-year El Niño and La Niña events are roughly symmetric. The composite multi-year ENSO reveals that anomalous ocean heat content (OHC) in the equatorial Pacific persists beyond the first peak, stimulating another event. This prolonged OHC anomaly is caused by meridional Ekman heat transport counteracting geostrophic recharge-discharge that otherwise acts to change the OHC anomaly. A meridionally wide pattern of sea surface temperature anomalies observed during multiyear ENSO is responsible for the Ekman heat transport. Furthermore, 100-member climate predictions were conducted for multi-year La Niña in 2020-2022. The ensemble-mean captures the second-year La Niña while the inter-member spread is explained by the position of the North Pacific high and negative North Pacific meridional mode. It contributes to the modulation of the apparent meridional scale of La Niña, and thus our proposed mechanisms are helpful in understanding ENSO persistence for the seasonal forecast.