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Przestrzenne generowanie dobowych danych meteorologicznych

100%

Iwanski S. , Kuchar L.

tom 02

nr 1

113-121

A modeling framework to assess the impact of climate change on a river runoff

80%

Kuchar L. , Iwanski S. , Jelonek L. , Szalinska W.

nr 2

Global climate change is anticipated to have consequences on water resources and the envi-ronment both at global and local/regional levels. Efforts towards proper management of future water resources and resolving potential water-related conflicts require the formulation of appropriate techniques to downscale the output of global climate models (GCM) to local conditions for hydrologic prediction. The paper presents an integrated framework for modeling the impact of climate change on river runoff that combines methodology for downscaling climate change scenarios for a basin scale with a hydrological model to estimate the impact of climate change on a river runoff. The modeling framework uses long-term observations of meteorological and hydrological variables together with a climate change scenario to provide a projection of future flows for the specified time horizon. The framework is based on a spatial weather generator and a distributed rainfall-runoff model. Such a configuration enables a reflection of the uncertainty of future conditions by running multiple realizations of future conditions, and also take into account the spatial variability of hydrological properties in the catchment by maintaining the physical details at a given grid size. The performance of the framework was presented for the Kaczawa basin that is one of the main left bank tributaries of the Odra River – the second biggest river in Poland. The results show simulated changes of the future river flow regime caused by climatic changes for two time horizons: 2040 and 2080.

Porównanie wybranych modeli do szacowania parowania potencjalnego w okresie zimowym dla potrzeb modelowania hydrologicznego

80%

Bac S. , Iwanski S. , Kuchar L.

nr 2[162]

Modelowanie przepływów w rzece Kaczawa w perspektywie lat 2030 i 2050 (półrocze letnie)

80%

Kuchar L. , Iwanski S. , Jelonek L. , Szalinska W.

nr 2[38]