Analysis of changes in the occurrence of ice phenomena in upland and mountain rivers of Poland.


Journal

PloS one
ISSN: 1932-6203
Titre abrégé: PLoS One
Pays: United States
ID NLM: 101285081

Informations de publication

Date de publication:
2024
Historique:
received: 15 02 2024
accepted: 12 07 2024
medline: 26 7 2024
pubmed: 26 7 2024
entrez: 26 7 2024
Statut: epublish

Résumé

The ice phenomena are an inherent component of rivers in temperate, continental, and polar climate zones. Evident progress in global warming leads to a decrease in snow cover on land and ice phenomena in water bodies, disrupting the stability of the hydrological cycle and aquatic ecosystems. Although common observations indicate the disappearance of ice phenomena in rivers over recent decades, detailed quantitative research is lacking in many regions, especially in the temperate zone. In this paper, ice phenomena were analyzed on the rivers of southern Poland, located in the upland and mountain areas of the country, as no such studies have been conducted so far. The temporal changes in the annual number of days with ice (NDI) phenomena were studied in locations where ice phenomena were observed every year for at least 30 years between 1951 and 2021. Using straightforward but commonly accepted procedures, such as the Mann-Kendall test, statistically significant decreasing trends in the annual NDI were revealed for the majority of gauging stations. The Theil-Sen (TS) slope mean values were -1.66 (ranging from -3.72 to -0.56), -1.41 (from -3.22 to -0.29), and -1.33 (from -2.85 to -0.29) for the datasets representing the periods 1992-2020, 1987-2020, and 1982-2020, respectively. The results for the annual NDI were additionally presented within the context of meteorological characteristics such as annual and winter (Nov-Apr) air temperature, precipitation, and water temperature. Correlation and regression analyses revealed that the main factor triggering the decrease in NDI is the increase in the average winter air temperature. An increase in temperature by 1°C results in a decrease in NDI by up to twenty days. If these negative trends continue, ice phenomena may disappear completely from southern Polish rivers within few decades.

Identifiants

pubmed: 39058710
doi: 10.1371/journal.pone.0307842
pii: PONE-D-24-05921
doi:

Substances chimiques

Ice 0

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

e0307842

Informations de copyright

Copyright: © 2024 Kochanek et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

Déclaration de conflit d'intérêts

The authors have declared that no competing interests exist.

Auteurs

Krzysztof Kochanek (K)

Faculty of Building Services, Hydro and Environmental Engineering, Warsaw University of Technology, Warsaw, Poland.

Agnieszka Rutkowska (A)

Faculty of Environmental Engineering and Land Surveying, Department of Applied Mathematics, University of Agriculture in Cracow, Cracow, Poland.

Katarzyna Baran-Gurgul (K)

Faculty of Environmental Engineering and Energy, Department of Geoengineering and Water Resources Management, Cracow University of Technology, Cracow, Poland.

Iwona Kuptel-Markiewicz (I)

Department of Hydrology and Hydrodynamics, Institute of Geophysics Polish Academy of Sciences, Warsaw, Poland.

Dorota Mirosław-Świątek (D)

Department of Hydrology, Institute of Environmental Engineering, Meteorology and Water Management, Warsaw University of Life Sciences-SGGW, Warsaw, Poland.

Mateusz Grygoruk (M)

Department of Hydrology, Institute of Environmental Engineering, Meteorology and Water Management, Warsaw University of Life Sciences-SGGW, Warsaw, Poland.

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