Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F12%3A55524" target="_blank" >RIV/60460709:41330/12:55524 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60460709:41310/12:55524

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods

Popis výsledku v původním jazyce

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 itas 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

Název v anglickém jazyce

Implementation of conceptual linear storage model of runoff with diurnal fluctuation in rainless periods

Popis výsledku anglicky

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 itas 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

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2012

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Hydrology and Hydromechanics

ISSN

0042-790X

e-ISSN

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Svazek periodika

60

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

10

Strana od-do

217-226

Kód UT WoS článku

000312915300001

EID výsledku v databázi Scopus

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