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Statements

Subject Item
n2:RIV%2F60460709%3A41310%2F12%3A55524%21RIV13-MSM-41310___
rdf:type
skos:Concept n9:Vysledek
dcterms:description
The aim of this paper is to set up the model describing the depletion runoff process when a catchment is supplied only from subsurface water resources and also to describe a transpiration effect when depleted mostly by riparian vegetation considering it as a dirunal process in hot and rainless period. This model is conceived as a simple linear description of all forms of subsurface runoff supplying the stream flow in fully forested the Teply Brook small catchment (district Zdar nad Sazavou, the Czech Republic) for the dry seasons of 2003 to 2007 when the discharges were continuously recorded at the outlet. There are three interconnected soil water zones, represented by the corresponding subsurface storages in the model. Actual evapotranspiration from the riparian part of the catchment is approximated by a special form of the Fouries series. The model simulates a runoff process using seven independent parameters, evapotranspiration is simulated through another four parameters. The paper points out how The aim of this paper is to set up the model describing the depletion runoff process when a catchment is supplied only from subsurface water resources and also to describe a transpiration effect when depleted mostly by riparian vegetation considering it as a dirunal process in hot and rainless period. This model is conceived as a simple linear description of all forms of subsurface runoff supplying the stream flow in fully forested the Teply Brook small catchment (district Zdar nad Sazavou, the Czech Republic) for the dry seasons of 2003 to 2007 when the discharges were continuously recorded at the outlet. There are three interconnected soil water zones, represented by the corresponding subsurface storages in the model. Actual evapotranspiration from the riparian part of the catchment is approximated by a special form of the Fouries series. The model simulates a runoff process using seven independent parameters, evapotranspiration is simulated through another four parameters. The paper points out how
dcterms:title
Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods
skos:prefLabel
Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods
skos:notation
RIV/60460709:41310/12:55524!RIV13-MSM-41310___
n9:predkladatel
n10:orjk%3A41310
n3:aktivita
n13:S n13:Z
n3:aktivity
S, Z(MSM6046070905)
n3:cisloPeriodika
4
n3:dodaniDat
n11:2013
n3:domaciTvurceVysledku
n17:5660572 n17:5941822
n3:druhVysledku
n14:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n7:predkladatel
n3:idSjednocenehoVysledku
140814
n3:idVysledku
RIV/60460709:41310/12:55524
n3:jazykVysledku
n19:eng
n3:klicovaSlova
linear runoff model, most upper soil layer, unsaturated and saturated zone, hot and dry rainless period, transpiration of riparian vegetation
n3:klicoveSlovo
n16:transpiration%20of%20riparian%20vegetation n16:hot%20and%20dry%20rainless%20period n16:linear%20runoff%20model n16:most%20upper%20soil%20layer n16:unsaturated%20and%20saturated%20zone
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[8BE62AD767D4]
n3:nazevZdroje
Journal of Hydrology and Hydromechanics
n3:obor
n4:DA
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n11:2012
n3:svazekPeriodika
60
n3:tvurceVysledku
Kovář, Pavel Dvořáková, Šárka Zeman, Josef
n3:wos
000312915300001
n3:zamer
n6:MSM6046070905
s:issn
0042-790X
s:numberOfPages
10
n12:organizacniJednotka
41310