Did recent sea surface temperature warming reinforce the extreme East Asian summer monsoon precipitation in 2020?
Abstract
We analyzed the possible effects of recent sea surface temperature (SST) warming on the extraordinary East Asian summer monsoon (EASM) precipitation in 2020 summer. The dynamic and thermodynamic impacts of SST are examined by conducting regional climate model experiments with observed SST and cold SST where the 22-year SST trend is removed. In the presence of warm SST, precipitation increases in low latitudes but decreases in the EASM region. This dipolar precipitation change pattern opposes the precipitation anomalies in 2020 summer, indicating that the extraordinary 2020 EASM precipitation is not likely driven by recent SST warming. The warm SST suppresses the western North Pacific subtropical high expansion and weakens the southwesterly from the South China Sea toward the EASM region. In terms of large-scale atmospheric circulations, SST-induced wind changes strengthen the local Walker circulation in the South China Sea and the Philippines and the local Hadley circulation across the EASM region. These support the reduced EASM rainfall in the control experiment compared to the cold SST experiment and imply that the precipitation reduction by dynamical effects could exceed the precipitation increase by thermodynamic effects in the EASM region under warm SST.
Versions
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BibTeX
@misc{mun2026recent,
title = {{Did recent sea surface temperature warming reinforce the extreme East Asian summer monsoon precipitation in 2020?}},
author = {Taeho Mun and Haerin Park and Dong-Hyun Cha and Chang-Keun Song and Seung-Ki Min and Seok-Woo Son},
howpublished = {arXiv},
year = {2026},
month = sep,
doi = {10.48550/arxiv.2609.02545},
eprint = {2609.02545},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2609.02545},
note = {CC BY-NC-ND 4.0},
}
RIS
TY - UNPB
TI - Did recent sea surface temperature warming reinforce the extreme East Asian summer monsoon precipitation in 2020?
AU - Taeho Mun
AU - Haerin Park
AU - Dong-Hyun Cha
AU - Chang-Keun Song
AU - Seung-Ki Min
AU - Seok-Woo Son
PY - 2026
DA - 2026/09/02
PB - arXiv
DO - 10.48550/arxiv.2609.02545
UR - https://arxiv.org/abs/2609.02545
AB - We analyzed the possible effects of recent sea surface temperature (SST) warming on the extraordinary East Asian summer monsoon (EASM) precipitation in 2020 summer. The dynamic and thermodynamic impacts of SST are examined by conducting regional climate model experiments with observed SST and cold SST where the 22-year SST trend is removed. In the presence of warm SST, precipitation increases in low latitudes but decreases in the EASM region. This dipolar precipitation change pattern opposes the precipitation anomalies in 2020 summer, indicating that the extraordinary 2020 EASM precipitation is not likely driven by recent SST warming. The warm SST suppresses the western North Pacific subtropical high expansion and weakens the southwesterly from the South China Sea toward the EASM region. In terms of large-scale atmospheric circulations, SST-induced wind changes strengthen the local Walker circulation in the South China Sea and the Philippines and the local Hadley circulation across the EASM region. These support the reduced EASM rainfall in the control experiment compared to the cold SST experiment and imply that the precipitation reduction by dynamical effects could exceed the precipitation increase by thermodynamic effects in the EASM region under warm SST.
ER -