Preprints
https://doi.org/10.5194/egusphere-2025-2982
https://doi.org/10.5194/egusphere-2025-2982
07 Nov 2025
 | 07 Nov 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

No longer on schedule, the pattern Is breaking apart: The Loss of Seasonal Synchrony in a Sub-Arctic River System Under Warming Climate

Abolfazl Jalali Shahrood, Amirhossein Ahrari, and Ali Torabi Haghighi

Abstract. Climate warming is altering the timing and synchrony of snow and ice processes across northern river systems, yet long-term shifts in their seasonal dynamics remain insufficiently resolved. Here, we analyze a 57-year daily record (1966–2023) from the River Oulankajoki in northeastern Finland to characterize freeze-up, break-up, snow accumulation and melt, and key atmospheric temperature transition points. Using a process-based detection tool, we identify significant advances in spring-related events, including snow melt, ice break-up, and the seasonal shift from cold to warm temperatures. In contrast, autumn transitions such as freeze-up and snow onset exhibit higher year-to-year variability and no consistent trends. The durations of cold season, ice cover, and snow melt periods have shortened, while warm and open-water seasons have lengthened. Moreover, the temporal gap between atmospheric warming and surface responses has increased in spring but contracted in autumn. These findings suggest not only a shift in seasonal timing but also a growing desynchronization between atmospheric conditions and cryo-hydrological processes, with implications for Arctic river ecology, ice forecasting, and flood risk under continued climate change.

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Abolfazl Jalali Shahrood, Amirhossein Ahrari, and Ali Torabi Haghighi

Status: open (until 19 Dec 2025)

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Abolfazl Jalali Shahrood, Amirhossein Ahrari, and Ali Torabi Haghighi
Abolfazl Jalali Shahrood, Amirhossein Ahrari, and Ali Torabi Haghighi
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Short summary
We analyzed 57 years of river, snow, and temperature records from a sub-Arctic watershed in Finland to understand how seasonal freezing and thawing have changed due to climate warming. Our findings show that spring events like snowmelt and ice break-up are happening earlier, while autumn changes remain unpredictable. This loss of seasonal coordination affects river behavior, water resources, and future planning under ongoing climate change.
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