Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]

Descripción del Articulo

Este trabajo fue financiado por el CONCYTECFONDECYT en el marco de la convocatoria Proyecto Investigaci?n B?sica y Aplicada, 2017-02 [Convenio N? 157-2017-FONDECYT].
Detalles Bibliográficos
Autores: Saldaña D.M., Ramos-Fernández L., Bejarano T.V., Gutiérrez L.A.
Formato: artículo
Fecha de Publicación:2021
Institución:Consejo Nacional de Ciencia Tecnología e Innovación
Repositorio:CONCYTEC-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.concytec.gob.pe:20.500.12390/3054
Enlace del recurso:https://hdl.handle.net/20.500.12390/3054
https://doi.org/10.4067/S0718-34292021000100017
Nivel de acceso:acceso abierto
Materia:Validation
Calibration
Lurin
Simulation
TETIS
https://purl.org/pe-repo/ocde/ford#1.05.11
id CONC_f86ccf9797f0420c28626f0977892dfc
oai_identifier_str oai:repositorio.concytec.gob.pe:20.500.12390/3054
network_acronym_str CONC
network_name_str CONCYTEC-Institucional
repository_id_str 4689
dc.title.none.fl_str_mv Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
title Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
spellingShingle Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
Saldaña D.M.
Validation
Calibration
Calibration
Lurin
Simulation
TETIS
TETIS
https://purl.org/pe-repo/ocde/ford#1.05.11
title_short Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
title_full Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
title_fullStr Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
title_full_unstemmed Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
title_sort Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]
author Saldaña D.M.
author_facet Saldaña D.M.
Ramos-Fernández L.
Bejarano T.V.
Gutiérrez L.A.
author_role author
author2 Ramos-Fernández L.
Bejarano T.V.
Gutiérrez L.A.
author2_role author
author
author
dc.contributor.author.fl_str_mv Saldaña D.M.
Ramos-Fernández L.
Bejarano T.V.
Gutiérrez L.A.
dc.subject.none.fl_str_mv Validation
topic Validation
Calibration
Calibration
Lurin
Simulation
TETIS
TETIS
https://purl.org/pe-repo/ocde/ford#1.05.11
dc.subject.es_PE.fl_str_mv Calibration
Calibration
Lurin
Simulation
TETIS
TETIS
dc.subject.ocde.none.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.05.11
description Este trabajo fue financiado por el CONCYTECFONDECYT en el marco de la convocatoria Proyecto Investigaci?n B?sica y Aplicada, 2017-02 [Convenio N? 157-2017-FONDECYT].
publishDate 2021
dc.date.accessioned.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.available.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.issued.fl_str_mv 2021
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12390/3054
dc.identifier.doi.none.fl_str_mv https://doi.org/10.4067/S0718-34292021000100017
dc.identifier.scopus.none.fl_str_mv 2-s2.0-85112784623
url https://hdl.handle.net/20.500.12390/3054
https://doi.org/10.4067/S0718-34292021000100017
identifier_str_mv 2-s2.0-85112784623
dc.language.iso.none.fl_str_mv spa
language spa
dc.relation.ispartof.none.fl_str_mv Idesia
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.uri.none.fl_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.publisher.none.fl_str_mv Universidad de Tarapaca
publisher.none.fl_str_mv Universidad de Tarapaca
dc.source.none.fl_str_mv reponame:CONCYTEC-Institucional
instname:Consejo Nacional de Ciencia Tecnología e Innovación
instacron:CONCYTEC
instname_str Consejo Nacional de Ciencia Tecnología e Innovación
instacron_str CONCYTEC
institution CONCYTEC
reponame_str CONCYTEC-Institucional
collection CONCYTEC-Institucional
repository.name.fl_str_mv Repositorio Institucional CONCYTEC
repository.mail.fl_str_mv repositorio@concytec.gob.pe
_version_ 1844883056524001280
spelling Publicationrp08780600rp08779600rp08778600rp08781600Saldaña D.M.Ramos-Fernández L.Bejarano T.V.Gutiérrez L.A.2024-05-30T23:13:38Z2024-05-30T23:13:38Z2021https://hdl.handle.net/20.500.12390/3054https://doi.org/10.4067/S0718-342920210001000172-s2.0-85112784623Este trabajo fue financiado por el CONCYTECFONDECYT en el marco de la convocatoria Proyecto Investigaci?n B?sica y Aplicada, 2017-02 [Convenio N? 157-2017-FONDECYT].The Lurin river is located in the coastal part of Peru. Although, in general the climate is arid, in some month of the year in possible to have some precipitation. This situation is the main cause of deficits in water resources management, inefficient growth of agriculture and livestock, lack of climatic and hydrometric information in the Basin. The TETIS Model which is a spatially distributed hydrological has been applied to modeling the Lurín river basin, for which information on precipitation, evapotranspiration and flow, geomorphological maps (MED, accumulated cells, flow direction, slope, speed), maps of hydrological parameters of static storage (Hu) and hydraulic conductivity of the soil (Ks) and the map of hydraulic conductivity of the aquifer (Kp), the map of vegetation cover and the information referred to the index of vegetation (?) by type of cover. In the hydrometric station of Antapucro and San Damian, the daily calibration and validation of the model were carried out. Obtaining the Nash indices (NSE), normalized mean square error (RSR) and volume error (Ev) of (0.7551, 0.4949, 0.701%) for calibration and (0.7611, 0.4888, –14.629%) for validation, respectively; the parameters with the highest sensitivity in the model being the evapotranspiration correction factor (FC2) and the rain interpolation factor (?). The daily flows were simulated from 1969 to 2019, the annual water balance an offer of 121.36 hm3 and demand of 111.59 hm3 were obtained, which corresponds mainly to agricultural use. In the water balance there is a surplus from January to May of 58.44 hm3, which is discharged to the sea due to the inexistent reservoir infrastructure in the basin. In the others months, June to December, there is a deficit of 48.67 hm3 due to the lack of rain. © 2021, Universidad de Tarapaca. All rights reserved.Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - ConcytecspaUniversidad de TarapacaIdesiainfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/4.0/ValidationCalibration-1Calibration-1Lurin-1Simulation-1TETIS-1TETIS-1https://purl.org/pe-repo/ocde/ford#1.05.11-1Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]info:eu-repo/semantics/articlereponame:CONCYTEC-Institucionalinstname:Consejo Nacional de Ciencia Tecnología e Innovacióninstacron:CONCYTEC20.500.12390/3054oai:repositorio.concytec.gob.pe:20.500.12390/30542024-05-30 16:13:33.634https://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_14cbinfo:eu-repo/semantics/closedAccessmetadata only accesshttps://repositorio.concytec.gob.peRepositorio Institucional CONCYTECrepositorio@concytec.gob.pe#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#<Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="1532b3a1-ffa5-444c-a62a-807663b468f9"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>spa</Language> <Title>Simulation with a conceptual distributed hydrological model on a daily scale in a semi-arid basin of the lurin river, Peru [Simulación con un modelo hidrológico distribuido de tipo conceptual a escala diaria en una cuenca semiárida del río Lurín, Perú]</Title> <PublishedIn> <Publication> <Title>Idesia</Title> </Publication> </PublishedIn> <PublicationDate>2021</PublicationDate> <DOI>https://doi.org/10.4067/S0718-34292021000100017</DOI> <SCP-Number>2-s2.0-85112784623</SCP-Number> <Authors> <Author> <DisplayName>Saldaña D.M.</DisplayName> <Person id="rp08780" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Ramos-Fernández L.</DisplayName> <Person id="rp08779" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Bejarano T.V.</DisplayName> <Person id="rp08778" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Gutiérrez L.A.</DisplayName> <Person id="rp08781" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Universidad de Tarapaca</DisplayName> <OrgUnit /> </Publisher> </Publishers> <License>https://creativecommons.org/licenses/by-nc-nd/4.0/</License> <Keyword>Validation</Keyword> <Keyword>Calibration</Keyword> <Keyword>Calibration</Keyword> <Keyword>Lurin</Keyword> <Keyword>Simulation</Keyword> <Keyword>TETIS</Keyword> <Keyword>TETIS</Keyword> <Abstract>The Lurin river is located in the coastal part of Peru. Although, in general the climate is arid, in some month of the year in possible to have some precipitation. This situation is the main cause of deficits in water resources management, inefficient growth of agriculture and livestock, lack of climatic and hydrometric information in the Basin. The TETIS Model which is a spatially distributed hydrological has been applied to modeling the Lurín river basin, for which information on precipitation, evapotranspiration and flow, geomorphological maps (MED, accumulated cells, flow direction, slope, speed), maps of hydrological parameters of static storage (Hu) and hydraulic conductivity of the soil (Ks) and the map of hydraulic conductivity of the aquifer (Kp), the map of vegetation cover and the information referred to the index of vegetation (?) by type of cover. In the hydrometric station of Antapucro and San Damian, the daily calibration and validation of the model were carried out. Obtaining the Nash indices (NSE), normalized mean square error (RSR) and volume error (Ev) of (0.7551, 0.4949, 0.701%) for calibration and (0.7611, 0.4888, –14.629%) for validation, respectively; the parameters with the highest sensitivity in the model being the evapotranspiration correction factor (FC2) and the rain interpolation factor (?). The daily flows were simulated from 1969 to 2019, the annual water balance an offer of 121.36 hm3 and demand of 111.59 hm3 were obtained, which corresponds mainly to agricultural use. In the water balance there is a surplus from January to May of 58.44 hm3, which is discharged to the sea due to the inexistent reservoir infrastructure in the basin. In the others months, June to December, there is a deficit of 48.67 hm3 due to the lack of rain. © 2021, Universidad de Tarapaca. All rights reserved.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication> -1
score 13.413352
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