Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

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

Wed. May 28, 2025 10:45 AM - 12:15 PM 101 (International Conference Hall, Makuhari Messe)

convener:Takahito Kataoka(JAMSTEC Japan Agency for Marine-Earth Science and Technology), Hiroyuki Murakami(Geophysical Fluid Dynamics Laboratory), Yushi Morioka(Japan Agency for Marine-Earth Science and Technology), Nathaniel C Johnson(NOAA Geophysical Fluid Dynamics Laboratory), Chairperson:Yushi Morioka(Japan Agency for Marine-Earth Science and Technology), Nathaniel C Johnson(NOAA Geophysical Fluid Dynamics Laboratory), Takahito Kataoka(JAMSTEC Japan Agency for Marine-Earth Science and Technology)

11:15 AM - 11:30 AM

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

*Ko Tsuchida1, Yu Kosaka1, Shoshiro Minobe2 (1.Research Center for Advanced Science and Technology, the University of Tokyo, 2.Faculty of Science, Hokkaido University)

Keywords:Earth's Energy Imbalance, Radiative budgets, Internal variability, ENSO

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.