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Ice jams and spring flooding across Ostrobothnia

Observations and prospects

Bibliographic Data

ID8238057
AuthorsMarek Kasprzak (0000-0002-8265-8441), Alun Hubbard (0000-0002-0503-3915)
Year2025
Volume54
Issue2
Pages95-106
Publication date2025-07-25
Open AccessYes
TypeARTICLE
VenueNordia Geographical Publications (BOOK_SERIES)
Journal identifiersISSN: 1238-2086 • E-ISSN: 2736-9722
PublisherNordia Geographical Publications (PUBLISHER)
DOI10.30671/nordia.156579
OpenAlexW4412673163
LanguageEN

Seasonal snow and ice play a key role in the hydrological regimes of Arctic and sub-Arctic river catchments that differentiate them from their lower latitude counterparts. Against a backdrop of assumed reduced spring flooding due to ongoing Arctic warming resulting in shorter winters with less snowfall, we examine the prevailing conditions that led to spring-melt flooding, its impact and mitigation management strategies across Northern Ostrobothnia in April 2024. We find that sustained freezing temperatures in early 2024, combined with thicker than average snowpack in March, preconditioned the region’s catchments to two episodes of flooding driven by abrupt warm events and widespread snowmelt in early March and April. Due to their predominantly shallow, east to west long-profiles, the region’s rivers received large fluxes of snowmelt runoff simultaneously along their entire courses, responding rapidly with rising levels and discharge. Thick river ice formed during the colder than average winter, causing ice jams at constricting pinch-points including bridges, dams and where rivers naturally shallowed or narrowed, leading to backup and flooding. Numerous effective civil interventions – including the release of discharge into managed agricultural areas – prevented extensive flood damage and major disruption to infrastructure other than temporary closure of some roads. We conclude that the event was pragmatically managed, precluding significant material damage and disruption. However, projected long-term climate scenarios indicating increased temperature fluctuations and extreme precipitation – including snowfall – events associated with intense warm air intrusions, coupled with potential meter-scale relative sea- and base-level rise could act in consort to increase the region’s winter and spring flood risk, rather than mitigate it

Flooding (psychology · Geography · Geotechnical engineering · Hydrology (agriculture · JAMS · Physical geography · Political science · Spring (device · Arctic and Antarctic ice dynamics · Arctic and Russian Policy Studies · Engineering · Environmental Science · Marine and environmental studies · Geology

Highly citedNo

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