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Runoff changes in areas differing in land-use in the blanice river basin - application of the deterministic model

Identifieur interne : 001597 ( Istex/Curation ); précédent : 001596; suivant : 001598

Runoff changes in areas differing in land-use in the blanice river basin - application of the deterministic model

Auteurs : Michal Jení Ek [République tchèque]

Source :

RBID : ISTEX:DE5D3ADC89E0EC16AEDA6421301A10F031957E05

English descriptors

Abstract

The aim of this article is to present partial results of more extensive research which is focused on using different methods for runoff computation in areas differing in land use. With the help of the deterministic lumped model HEC-HMS (Hydrologic Engineering Center - Hydrologic Modelling System) several simulations of r noff changes by different basin conditions were carried out. The Blanice River basin in the Šumava Mts. was chosen as an experimental catchment in its closure profile in Podedvory (gauge station, area 209.6 km2). For assessment of land cover changes impact on hydrological regime four scenarios were carried out - 10, 20, 50 and 100-year 1-day probability precipitation in combination with different initial conditions (soil saturation). These scenarios were applied to the stage of the land cover in the year 1992 and 2000 (based on the CORINE Landcover database). The method SCS CN (Soil Conservation Service Curve Number) was applied as the main model technique.

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DOI: 10.2478/v10098-009-0014-0

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ISTEX:DE5D3ADC89E0EC16AEDA6421301A10F031957E05

Le document en format XML

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<div type="abstract" xml:lang="en">The aim of this article is to present partial results of more extensive research which is focused on using different methods for runoff computation in areas differing in land use. With the help of the deterministic lumped model HEC-HMS (Hydrologic Engineering Center - Hydrologic Modelling System) several simulations of r noff changes by different basin conditions were carried out. The Blanice River basin in the Šumava Mts. was chosen as an experimental catchment in its closure profile in Podedvory (gauge station, area 209.6 km2). For assessment of land cover changes impact on hydrological regime four scenarios were carried out - 10, 20, 50 and 100-year 1-day probability precipitation in combination with different initial conditions (soil saturation). These scenarios were applied to the stage of the land cover in the year 1992 and 2000 (based on the CORINE Landcover database). The method SCS CN (Soil Conservation Service Curve Number) was applied as the main model technique.</div>
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