Influence of climate changes on the state of water resources in Poland and their usage
K Kubiak-Wójcicka, S Machula - Geosciences, 2020 - mdpi.com
The study aims to estimate the amount of available renewable water resources in Poland in
the years 1999–2018 and the extent of their use by various sectors of the national economy …
the years 1999–2018 and the extent of their use by various sectors of the national economy …
Assessment of water resources in Poland
K Kubiak-Wójcicka - Quality of Water Resources in Poland, 2021 - Springer
The paper analyzes the size of water resources in Poland, which are among the lowest in
Europe. Water resources are very variable, both temporally and spatially, which results from …
Europe. Water resources are very variable, both temporally and spatially, which results from …
[PDF][PDF] Regionalization methods for low flow estimation in ungauged catchments-a review
A Cupak - Acta Scientiarum Polonorum. Formatio Circumiectus, 2020 - acta.urk.edu.pl
The described regional regression approach for low flow estimation in ungauged
catchments, which correlates low flow indices and catchment characteristics, is the most …
catchments, which correlates low flow indices and catchment characteristics, is the most …
Determination of Seasonal Indices for the Regionalization of Low Flows in the Upper Vistula River Basin
A Cupak, G Kaczor - Water, 2023 - mdpi.com
Low flow is a parameter that is used for many purposes in water management. It is
particularly important in terms of the needs of small water supply systems, which usually are …
particularly important in terms of the needs of small water supply systems, which usually are …
[图书][B] Hydromorfologiczne uwarunkowania funkcjonowania geoekosystemu Zbiornika Włocławskiego= Hydromorphological conditions of the functioning of the …
P Gierszewski - 2018 - books.google.com
Pierwsze zapory wodne pojawiły się najprawdopodobniej przed 3000 lat pne w
nadrzecznych cywilizacjach Mezopotamii i Egiptu (Mays 2010; Tamburrino 2010). Jednak to …
nadrzecznych cywilizacjach Mezopotamii i Egiptu (Mays 2010; Tamburrino 2010). Jednak to …
[图书][B] Prawidłowości obiegu wody na obszarze beskidzko-pogórskim Karpat Zachodnich na przykładzie zlewni Bystrzanki w świetle zmian klimatu i działalności …
W Bochenek - 2020 - books.google.com
Obieg wody na kuli ziemskiej jest procesem ciągłym, zapewniającym prawidłowe
funkcjonowanie przyrody ożywionej, w tym człowieka. Jest to proces niezwykle złożony …
funkcjonowanie przyrody ożywionej, w tym człowieka. Jest to proces niezwykle złożony …
Sezonowość odpływu z wybranych zlewni karpackich= Seasonality of outflow in selected Carpathian catchments
P Jokiel, P Tomalski - Przegląd Geograficzny, 2017 - rcin.org.pl
Opracowanie zawiera analizę sezonowości odpływu w 12 zlewniach karpackich. Do badań
wykorzystano szeregi dobowych przepływów z lat 1951-2010. Dla badanych przekrojów …
wykorzystano szeregi dobowych przepływów z lat 1951-2010. Dla badanych przekrojów …
[PDF][PDF] Flow characteristics of intermittent rivers in Slovakia
Flow characteristics of intermittent rivers in Slovakia. Intermittent rivers are rivers that cease
to flow, ie temporary, ephemeral, seasonal, and episodic rivers. Analysis of hydrological …
to flow, ie temporary, ephemeral, seasonal, and episodic rivers. Analysis of hydrological …
Flow seasonality in two big Polish rivers–the Vistula and the Oder
P Jokiel, P Tomalski - Management of Water Resources in Poland, 2021 - Springer
The aim of the chapter is to identify the flow seasonality of Vistula river (14 water gauges)
and the Oder river (11 water gauges) located along the river's course. For this purpose …
and the Oder river (11 water gauges) located along the river's course. For this purpose …
Earlier emergence of winter-spring maximum streamflow across Poland, 1981–2020
U Somorowska - Acta Geographica Lodziensia, 2024 - journals.ltn.lodz.pl
Rivers in Poland present nival, nivo-pluvial and pluvio-nival water regimes with
considerable peak flows occurring at the winter-spring turn in March, April or May. As climate …
considerable peak flows occurring at the winter-spring turn in March, April or May. As climate …