Record‐High Precipitation Over Eastern Europe Induced by Tropical‐Subtropical North Atlantic Warming in Late Fall 2023

Abstract Eastern Europe experienced record‐high precipitation in late fall (October–November) 2023, with an area‐weighted anomaly reaching up to 86 mm, >80% of its climatological precipitation. This study examines the drivers of this anomalous event using observations‐based statistical analyses, and atmospheric model experiments. Our results reveal that exceptional warming in the tropical‐subtropical North Atlantic (TSNA), characterized by a warm blob off North Africa reaching 1.2 K, played a crucial role. The TSNA warming induced a low‐pressure anomaly over the mid‐latitude North Atlantic and Europe, facilitating moisture transport and convergence toward Eastern Europe, leading to heavy rainfall. While the concurrent El Niño event and positive Indian Ocean Dipole may contribute to this process, their impacts were relatively modest compared to TSNA warming. These findings highlight the importance of monitoring and predicting TSNA SST anomaly to improve seasonal precipitation forecasts and develop effective adaptation strategies for Europe in the context of climate change.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-04-24
DOI
https://doi.org/10.1029/2024gl114309
Citations
1
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
1.11

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article

Record‐High Precipitation Over Eastern Europe Induced by Tropical‐Subtropical North Atlantic Warming in Late Fall 2023

Yurong Hou, Kai Man, Xichen Li, Shun Yu
1 citations
Geophysical Research Letters
Climate variability and models
1.11
article

Record‐High Precipitation Over Eastern Europe Induced by Tropical‐Subtropical North Atlantic Warming in Late Fall 2023

Yurong Hou, Kai Man, Xichen Li, Shun Yu
article en
1 citations

Abstract

Abstract Eastern Europe experienced record‐high precipitation in late fall (October–November) 2023, with an area‐weighted anomaly reaching up to 86 mm, >80% of its climatological precipitation. This study examines the drivers of this anomalous event using observations‐based statistical analyses, and atmospheric model experiments. Our results reveal that exceptional warming in the tropical‐subtropical North Atlantic (TSNA), characterized by a warm blob off North Africa reaching 1.2 K, played a crucial role. The TSNA warming induced a low‐pressure anomaly over the mid‐latitude North Atlantic and Europe, facilitating moisture transport and convergence toward Eastern Europe, leading to heavy rainfall. While the concurrent El Niño event and positive Indian Ocean Dipole may contribute to this process, their impacts were relatively modest compared to TSNA warming. These findings highlight the importance of monitoring and predicting TSNA SST anomaly to improve seasonal precipitation forecasts and develop effective adaptation strategies for Europe in the context of climate change.

Geophysical Research LettersVol. 52(8)
Chinese Academy of Sciences (CN), Institute of Atmospheric Physics (CN), University of Chinese Academy of Sciences (CN), China Agricultural University (CN)
National Science Fund for Distinguished Young Scholars
Openalex Percentile: Top 25%
Climate variability and models
1.11
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Record‐High Precipitation Over Eastern Europe Induced by Tropical‐Subtropical North Atlantic Warming in Late Fall 2023 — Yurong Hou, Kai Man, et al. · Geophysical Research Letters (2025) | TGRS Research Map | TGRS