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Volume 44 Issue 9
Sep.  2026
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LIU Kanglong, CAO Qing, HUANG Xiao, LIU Junjiang. Characteristics of rapid temperature flip events based on hybrid regionalization and spatiotemporal composite index clustering[J]. ENVIRONMENTAL ENGINEERING , 2026, 44(9): 161-170. doi: 10.13205/j.hjgc.202609017
Citation: LIU Kanglong, CAO Qing, HUANG Xiao, LIU Junjiang. Characteristics of rapid temperature flip events based on hybrid regionalization and spatiotemporal composite index clustering[J]. ENVIRONMENTAL ENGINEERING , 2026, 44(9): 161-170. doi: 10.13205/j.hjgc.202609017

Characteristics of rapid temperature flip events based on hybrid regionalization and spatiotemporal composite index clustering

doi: 10.13205/j.hjgc.202609017
  • Received Date: 2025-12-23
    Available Online: 2026-11-05
  • Rapid temperature flips, characterized by abrupt transitions between warm and cold extremes within a short period, pose substantial challenges to regional climate variability, ecosystem stability, and socio-economic systems. Based on the CN05.1 High-Resolution Daily Gridded Temperature Dataset over China for 1979—2021 and concurrent reanalysis atmospheric circulation data, a regional-scale identification framework for rapid temperature flip events was developed by explicitly accounting for their temporal evolution and spatial continuity. By integrating rotated empirical orthogonal function (REOF) analysis with K-means clustering, China was divided into 14 homogeneous temperature regions. Within representative regions, rapid temperature flip events were further classified using a set of composite indices, including event duration, spatial coverage, transition time, and transition intensity. Composite analyses were then conducted to examine the evolution of atmospheric dynamical and thermodynamical variables before and after different types of events. The results reveal pronounced regional differences in both the frequency and structural characteristics of rapid temperature flips across China. Overall, cold-related flips occur more frequently than warm-related flips, with higher event frequency observed over the Pearl River Basin, the middle and lower reaches of the Yangtze River, and the Hetao region (the Great Bend of the Yellow River). Distinct event types exhibit clear separations in spatial scale, persistence, and intensity. Despite these differences, the lifecycle evolution of precipitation, vertical motion, geopotential height, surface pressure, and specific humidity anomalies shows strong consistency across event types, indicating that rapid temperature flips can be understood within a unified large-scale circulation adjustment framework. These findings advance the understanding of rapid temperature reversals at the regional scale and provide a scientific basis for mechanism studies, monitoring strategies, and impact assessments of rapid temperature flip events.
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