Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica
(Figure Presented) Tropical mountain regions contain the main headwaters of important rivers in Central America. We selected 2 contrasting catchments located in a mountainous region to evaluate the precision of daily flow estimates based on the Hydrological Land Use Change (HYLUC) and Nedbør-Afstrøm...
Autores Principales: | Jiménez-Rodríguez , César, Calvo-Alvarado, Julio, Jackson, John |
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International Mountain Society
2017
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https://www.scopus.com/inward/record.url?eid=2-s2.0-84941625425&partnerID=40&md5=53cf4dc23f7d2e995bc36a48f6c432fc https://hdl.handle.net/2238/6945 |
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RepoTEC69452022-04-09T03:05:30Z Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica Jiménez-Rodríguez , César Calvo-Alvarado, Julio Jackson, John Cambio climático Hidrometeorología Precipitaciones (Figure Presented) Tropical mountain regions contain the main headwaters of important rivers in Central America. We selected 2 contrasting catchments located in a mountainous region to evaluate the precision of daily flow estimates based on the Hydrological Land Use Change (HYLUC) and Nedbør-Afstrømnings Model (NAM) hydrological models. A second objective was to simulate the impact of expected climate change for the year 2050 on stream flows and seasonal distribution of rainfall. We studied the catchments of the Tempisquito and Cucaracho streams, located in the Guanacaste volcanic mountain range of Costa Rica, from April 2008 to October 2010. Modeling of discharge using the NAM and HYLUC models suggested difficulties in their calibration due to intrinsic catchment characteristics because of their volcanic origin. The climate change scenario applied in both catchments depicted a strong reduction in discharge. However, the Cucaracho catchment, on the Caribbean slope, is predicted to experience a smaller reduction in discharge than the Tempisquito catchment, located on the Pacific slope. 2017-04-05T20:25:15Z 2017-04-05T20:25:15Z 2015 info:eu-repo/semantics/article https://www.scopus.com/inward/record.url?eid=2-s2.0-84941625425&partnerID=40&md5=53cf4dc23f7d2e995bc36a48f6c432fc 02764741 https://hdl.handle.net/2238/6945 eng Attribution-NonCommercial 3.0 Costa Rica https://creativecommons.org/licenses/by-nc/3.0/cr/ application/pdf International Mountain Society Jiménez-Rodríguez, C. D., Calvo-Alvarado, J. C., & Jackson, J. K. (2015). Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica. Mountain Research & Development, 35(3), 240-253. doi:10.1659/MRD-JOURNAL-D-14-00109.1 |
institution |
Tecnológico de Costa Rica |
collection |
Repositorio TEC |
language |
Inglés |
topic |
Cambio climático Hidrometeorología Precipitaciones |
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Cambio climático Hidrometeorología Precipitaciones Jiménez-Rodríguez , César Calvo-Alvarado, Julio Jackson, John Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
description |
(Figure Presented) Tropical mountain regions contain the main headwaters of important rivers in Central America. We selected 2 contrasting catchments located in a mountainous region to evaluate the precision of daily flow estimates based on the Hydrological Land Use Change (HYLUC) and Nedbør-Afstrømnings Model (NAM) hydrological models. A second objective was to simulate the impact of expected climate change for the year 2050 on stream flows and seasonal distribution of rainfall. We studied the catchments of the Tempisquito and Cucaracho streams, located in the Guanacaste volcanic mountain range of Costa Rica, from April 2008 to October 2010. Modeling of discharge using the NAM and HYLUC models suggested difficulties in their calibration due to intrinsic catchment characteristics because of their volcanic origin. The climate change scenario applied in both catchments depicted a strong reduction in discharge. However, the Cucaracho catchment, on the Caribbean slope, is predicted to experience a smaller reduction in discharge than the Tempisquito catchment, located on the Pacific slope. |
format |
Artículo |
author |
Jiménez-Rodríguez , César Calvo-Alvarado, Julio Jackson, John |
author_sort |
Jiménez-Rodríguez , César |
title |
Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
title_short |
Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
title_full |
Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
title_fullStr |
Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
title_full_unstemmed |
Performance of Two Hydrological Models in Predicting Daily Flow under a Climate Change Scenario for Mountainous Catchments in Northwestern Costa Rica |
title_sort |
performance of two hydrological models in predicting daily flow under a climate change scenario for mountainous catchments in northwestern costa rica |
publisher |
International Mountain Society |
publishDate |
2017 |
url |
https://www.scopus.com/inward/record.url?eid=2-s2.0-84941625425&partnerID=40&md5=53cf4dc23f7d2e995bc36a48f6c432fc https://hdl.handle.net/2238/6945 |
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1796139253697085440 |
score |
12.2319145 |