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].
| Autores: | , , , |
|---|---|
| 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 |
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| 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 |
Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).