日本地球惑星科学連合2025年大会

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[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-CG38] Climate Variability and Predictability on Subseasonal to Centennial Timescales

2025年5月28日(水) 10:45 〜 12:15 101 (幕張メッセ国際会議場)

コンビーナ:片岡 崇人(国立研究開発法人 海洋研究開発機構)、Murakami Hiroyuki(Geophysical Fluid Dynamics Laboratory/University Corporation for Atmospheric Research)、森岡 優志(海洋研究開発機構)、Johnson Nathaniel C(NOAA Geophysical Fluid Dynamics Laboratory)、座長:森岡 優志(海洋研究開発機構)、Nathaniel C Johnson(NOAA Geophysical Fluid Dynamics Laboratory)、片岡 崇人(国立研究開発法人 海洋研究開発機構)

11:15 〜 11:30

[ACG38-09] The triple-dip La Niña was key to Earth’s extreme heat uptake in 2022-2023

*土田 耕1小坂 優1見延 庄士郎2 (1.東京大学先端科学技術研究センター、2.北海道大学大学院理学研究院)

キーワード:地球エネルギー非平衡、放射収支、内部変動、エルニーニョ・南方振動

Recent observations reveal a surge in Earth's energy uptake in 2022/23, reaching 1.94 W/m2 (yearly average from October 2022 to September 2023). This increase played a pivotal role in the record-high global surface temperatures and widespread climate extremes observed by early 2024. However, its attribution remains challenging due to limited understanding of internal climate variability’s influence on Earth’s energy imbalance. Here, using multi-model climate simulations, we show that the transition from a three-year La Niña to a strong 2023/24 El Niño was a key driver of the extreme 2022/23 energy uptake, superimposed on the ongoing positive trend of Earth’s energy imbalance (EEI) due to anthropogenic forcing. We find that simulation samples with extreme global energy uptake systematically accompany preceding multi-year La Niña and subsequent El Niño, consistent with observations. These samples also replicate the dominant contribution of the shortwave radiation anomaly to the net energy imbalance and spatial distributions of radiation and atmospheric circulation anomalies organized by El Niño-Southern Oscillation (ENSO). Further analyses using targeted sampling of ENSO transitions reveal that the La Niña-to-El Niño sequence contributed 0.58 (±0.04) W/m² to the enhanced energy uptake, with the multi-year persistence of La Niña alone accounting for an additional 0.23 W/m².When combined with the external forcing component (~1.1 W/m²) estimated from large ensemble simulations, the enhancement of EEI associated with internal variability can closely account for the extreme EEI observed in 2022/23.Our finding illustrates the striking influence of internal climate variability, in addition to anthropogenic forcing, on Earth's energy budget and underscores their significance in past and future global climate extremes.