Co-occurrence probability of water balance elements in a mountain catchment on the example of the upper Nysa Kłodzka River

Perz, Adam; Sobkowiak, Leszek; Wrzesiński, Dariusz

doi:10.1007/s11600-022-00765-z

Artykuł - szczegóły

Tytuł artykułu

Co-occurrence probability of water balance elements in a mountain catchment on the example of the upper Nysa Kłodzka River

Autorzy

Perz Adam , Sobkowiak Leszek , Wrzesiński Dariusz

Wybrane pełne teksty z tego czasopisma

https://www.springer.com/journal/11600

Identyfikatory

DOI

10.1007/s11600-022-00765-z

Warianty tytułu

Języki publikacji

Abstrakty

Conditions of the formation of key elements of the water balance, such as precipitation and runoff, and relations between them in the mountain catchment area are very complicated, conditioned both by the climatic factor and the physiographic characteristics of the catchment area. The aim of the study is to determine relations between precipitation and runoff in the Kłodzka Valley (KV) located in mountain areas of south-western Poland. Analyzes were based on precipitation in KV and discharges of the Nysa Kłodzka River and its tributaries, recorded in hydrological years 1974–2013. The bivariate Archimedean copulas were used to describe the degree of synchronicity between these variables. The study area shows a considerable variability in the conditions of transformation of precipitation into runoff. It is conditioned both by the pluvial regime and the physical-geographical characteristics of the catchment area. As a result, sub-catchments with diversified hydrological activity and their role in the formation of water resources of the entire KV were identified. Among them, the Biała Lądecka River sub-catchment was found to be the most hydrologically active, and the sub-catchment of Bystrzyca Dusznicka River the most inert, despite e.g. quite similar synchronicity of precipitation compared to the average precipitation in KV. At the same time, the KV rivers are characterized by different types of runoff regime and characteristic of the water balance structure. The methodology presented can be useful in determining dependencies between selected elements of the water balance and evaluation of water resources availability in source areas of mountain rivers.

Słowa kluczowe

precipitation runoff synchronicity rainfall-runoff modelling runoff coefficient bivariate copula functions

opad atmosferyczny spływ synchroniczność modelowanie relacji opad–odpływ współczynnik spływu

Wydawca

Instytut Geofizyki PAN
Springer

Czasopismo

Acta Geophysica

Rocznik

2022

Tom

Vol. 70, no 3

Strony

1301--1315

Opis fizyczny

Bibliogr. 52 poz.

Twórcy

autor

Perz Adam

adam.perz@amu.edu.pl

Department of Hydrology and Water Management, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Bogumiła Krygowskiego str. 10, 61-680 Poznań, Poland

https://orcid.org/0000-0002-2497-4390

autor

Sobkowiak Leszek

lesob@amu.edu.pl

Department of Hydrology and Water Management, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Bogumiła Krygowskiego str. 10, 61-680 Poznań, Poland

https://orcid.org/0000-0002-7921-1454

autor

Wrzesiński Dariusz

darwrze@amu.edu.pl

Department of Hydrology and Water Management, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Bogumiła Krygowskiego str. 10, 61-680 Poznań, Poland

https://orcid.org/0000-0001-5025-1447

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Uwagi

Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-ae5653a2-d61c-4c66-a13b-0276c205b4c2