Preprints
https://doi.org/10.5194/egusphere-2026-1017
https://doi.org/10.5194/egusphere-2026-1017
11 Mar 2026
 | 11 Mar 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Teleconnection processes linking snow cover variability over western Siberia to enhanced early-winter cold waves in South Korea

Sangwoo Kim and Eungul Lee

Abstract. This study examines thermodynamic teleconnection processes to identify the drivers of the increasing frequency of December cold waves in South Korea over the past 46 years. The identified teleconnection is associated with land–atmosphere interactions triggered by reduced October snow cover (SC) over western Siberia. By refining the cold wave advisory criteria of Korea Meteorological Administration, we calculated cold day frequencies. We applied k-means clustering and principal component analysis to extract dominant time series representing nationwide cold day variability. Analyses based on automated synoptic observing system and ERA5 reanalysis data revealed that October SC reduction over western Siberia initiates a positive snow–ice albedo feedback, leading to enhanced surface solar radiation absorption and increased turbulent heat fluxes. These thermodynamic anomalies lead to atmospheric thermal expansion during October through December, thereby strengthening a December anticyclonic anomaly centered over western Siberia. The intensified northerly winds along the eastern flank of this anomaly established a teleconnection pattern that amplifies early-winter cold waves in South Korea. Overall, these results indicate that October SC may serve as a critical precursor to the recent intensification of early-winter cold waves, providing a scientific foundation for policies to adapt and mitigate the socioeconomic impacts of climate change.

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Sangwoo Kim and Eungul Lee

Status: open (until 22 Apr 2026)

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Sangwoo Kim and Eungul Lee
Sangwoo Kim and Eungul Lee

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Short summary
December cold waves in South Korea have become more frequent over the last 46 years. We found that reduced October snow cover in western Siberia lets the land absorb more sunlight and release more heat into the air. This extra heat can alter the wind pattern during December, strengthening northerly winds that could push cold air to East Asia. Using October snow cover in western Siberia as a precursor may support earlier warnings and help reduce socioeconomic damage from early-winter cold waves.
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