Translations:Einzugsgebietsfenster/23/en: Unterschied zwischen den Versionen
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In the extended method, not only the direct surface runoff is determined, but also a [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation|soil moisture simulation]] is carried out for the infiltrated | In the extended method, not only the direct surface runoff is determined, but also a [[Special:MyLanguage/Einzugsgebiet#Bodenfeuchtesimulation|soil moisture simulation]] is carried out for the infiltrated amount, and the components interflow and base flow are determined. For this purpose, the [[Special:MyLanguage/Elementarflächenfenster|hydrological response units]] must be created using the corresponding button. The retention coefficients for interflow and base flow, which are used for the calculation of the [[Special:MyLanguage/Einzugsgebiet#Abflusskonzentration|discharge concentration]], are also defined. Moreover, the initial soil moisture can be set (default setting: 100%). | ||
If the checkbox ''Use original soil | If the checkbox ''Use original soil layer'' is activated, the [[Special:MyLanguage/Bodentypenfenster|soil layers]] are used as provided by the user. By default, the soil layers are grouped into three [[Special:MyLanguage/Einzugsgebiet#Bodentyp/ Bodenart|internal calculation layers]] (infiltration layer, root layer, and transport layer). |
Version vom 15. Dezember 2020, 13:28 Uhr
In the extended method, not only the direct surface runoff is determined, but also a soil moisture simulation is carried out for the infiltrated amount, and the components interflow and base flow are determined. For this purpose, the hydrological response units must be created using the corresponding button. The retention coefficients for interflow and base flow, which are used for the calculation of the discharge concentration, are also defined. Moreover, the initial soil moisture can be set (default setting: 100%). If the checkbox Use original soil layer is activated, the soil layers are used as provided by the user. By default, the soil layers are grouped into three internal calculation layers (infiltration layer, root layer, and transport layer).