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Abstract
This study assesses the projected trajectory of Warm Arctic-Cold Continent (WACC) events in East Asia and North America through large ensemble simulation for the upcoming decades. It analyses the evolution of the geographical boundaries of threshold cold temperatures, revealing a significant northward shift as a sign of global warming’s impact on the southward advancement of Arctic cold air. While validating the intensification of the WACC phenomenon until the 2020 s, echoing earlier studies, the findings indicate a marked decrease beginning in the 2030s. If warming is not curbed, this shift suggests a critical modification in the WACC pattern, prompting a re-evaluation of existing theories and models for extreme winter weather events. The results have major implications, spurring communities impacted by WACC to anticipate future changes and encouraging the climate forecasting community to update conceptual models for improved adaptation and mitigation approaches.
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1 Gwangju Institute of Science and Technology, School of Earth Sciences and Environmental Engineering, Gwangju, South Korea (GRID:grid.61221.36) (ISNI:0000 0001 1033 9831)
2 Utah State University, Department of Plants, Soils, and Climate, Logan, USA (GRID:grid.53857.3c) (ISNI:0000 0001 2185 8768)
3 Seoul National University, School of Earth and Environmental Sciences, Seoul, South Korea (GRID:grid.31501.36) (ISNI:0000 0004 0470 5905)
4 Chonnam National University, Faculty of Earth and Environmental Sciences, Gwangju, South Korea (GRID:grid.14005.30) (ISNI:0000 0001 0356 9399)
5 Pukyong National University, Department of Environmental Atmospheric Sciences, Busan, South Korea (GRID:grid.412576.3) (ISNI:0000 0001 0719 8994)
6 Korea Advanced Institute of Science and Technology, Moon Soul Graduate School of Future Strategy, Daejeon, South Korea (GRID:grid.37172.30) (ISNI:0000 0001 2292 0500)