Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia

Páramo ecosystems are located on the upper parts of the tropical mountains, below the snow line areas or in isolated areas where no glacier ecosystems occur. These ecosystems are considered important for their biodiversity, but mainly because they are permanent source of water for populations located at the upper and middle parts of the Andes. Recent studies indicate that ecosystems located at high altitudes, are more vulnerable to climate change and to changes in land use, which threatens the ecosystem services derived from them. There are very few studies in these ecosystems, within which, studies on the hydrological functioning are even scarcer, which seems to be related to their position in the top of the mountains and difficulties associated with the access to them. This implies that there is a need to create tools that allow us to study these ecosystems, overcoming the current difficulties. Hydrological TOPMODEL is used to investigate the hydrological functioning of the páramo of Chingaza, through a case study in La Chucua basin. For this, we calibrate and validate the model using two data sets of climate and the hydrology of the basin (climate and discharge from 2008 and 2009, respectively). Through the calibration procedure we obtain a high efficiency value of 0.76 model (coefficient Nash - Sutcliffe), which adequately represents the hydrological behavior of the páramo. Simulations with better adjustment between measured and predicted values of discharge, have low values of surface infiltration excess runoff, indicating high water storage capacity on the soils. This agrees with the predominance of subsurface flow in studied ecosystem, given the special characteristics of soils. Results also show the large influence of factors represented in the model (topography and soils), on water basin response to rainfall events. This is significant evidence of exceptional hydrological behavior of the páramos, mainly related to the presence of soil with high organic matter content. These results imply that TOPMODEL is a robust tool, able to represent in a precise manner the hydrological functioning of the basin La Chucua, and consequently it is expected that TOPMODEL can also represent hydrological conditions of Chingaza páramo.

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Main Authors: Gil Morales, Eydith Girleza, Tobón Marín, Conrado
Format: Digital revista
Language:eng
Published: Universidad Nacional de Colombia - Sede Medellín - Facultad de Ciencias Agrarias 2016
Online Access:https://revistas.unal.edu.co/index.php/refame/article/view/59137
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institution UNAL
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country Colombia
countrycode CO
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language eng
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author Gil Morales, Eydith Girleza
Tobón Marín, Conrado
spellingShingle Gil Morales, Eydith Girleza
Tobón Marín, Conrado
Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
author_facet Gil Morales, Eydith Girleza
Tobón Marín, Conrado
author_sort Gil Morales, Eydith Girleza
title Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
title_short Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
title_full Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
title_fullStr Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
title_full_unstemmed Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia
title_sort hydrological modelling with topmodel of chingaza páramo, colombia
description Páramo ecosystems are located on the upper parts of the tropical mountains, below the snow line areas or in isolated areas where no glacier ecosystems occur. These ecosystems are considered important for their biodiversity, but mainly because they are permanent source of water for populations located at the upper and middle parts of the Andes. Recent studies indicate that ecosystems located at high altitudes, are more vulnerable to climate change and to changes in land use, which threatens the ecosystem services derived from them. There are very few studies in these ecosystems, within which, studies on the hydrological functioning are even scarcer, which seems to be related to their position in the top of the mountains and difficulties associated with the access to them. This implies that there is a need to create tools that allow us to study these ecosystems, overcoming the current difficulties. Hydrological TOPMODEL is used to investigate the hydrological functioning of the páramo of Chingaza, through a case study in La Chucua basin. For this, we calibrate and validate the model using two data sets of climate and the hydrology of the basin (climate and discharge from 2008 and 2009, respectively). Through the calibration procedure we obtain a high efficiency value of 0.76 model (coefficient Nash - Sutcliffe), which adequately represents the hydrological behavior of the páramo. Simulations with better adjustment between measured and predicted values of discharge, have low values of surface infiltration excess runoff, indicating high water storage capacity on the soils. This agrees with the predominance of subsurface flow in studied ecosystem, given the special characteristics of soils. Results also show the large influence of factors represented in the model (topography and soils), on water basin response to rainfall events. This is significant evidence of exceptional hydrological behavior of the páramos, mainly related to the presence of soil with high organic matter content. These results imply that TOPMODEL is a robust tool, able to represent in a precise manner the hydrological functioning of the basin La Chucua, and consequently it is expected that TOPMODEL can also represent hydrological conditions of Chingaza páramo.
publisher Universidad Nacional de Colombia - Sede Medellín - Facultad de Ciencias Agrarias
publishDate 2016
url https://revistas.unal.edu.co/index.php/refame/article/view/59137
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spelling oai:www.revistas.unal.edu.co:article-591372019-04-29T17:25:20Z Hydrological modelling with TOPMODEL of Chingaza páramo, Colombia Modelación hidrológica con TOPMODEL en el páramo de Chingaza, Colombia Gil Morales, Eydith Girleza Tobón Marín, Conrado Ecohydrology Modelling Páramos The Chucua basin Topmodel Ecohidrología Modelación Páramos Cuenca La Chucua Topmodel Páramo ecosystems are located on the upper parts of the tropical mountains, below the snow line areas or in isolated areas where no glacier ecosystems occur. These ecosystems are considered important for their biodiversity, but mainly because they are permanent source of water for populations located at the upper and middle parts of the Andes. Recent studies indicate that ecosystems located at high altitudes, are more vulnerable to climate change and to changes in land use, which threatens the ecosystem services derived from them. There are very few studies in these ecosystems, within which, studies on the hydrological functioning are even scarcer, which seems to be related to their position in the top of the mountains and difficulties associated with the access to them. This implies that there is a need to create tools that allow us to study these ecosystems, overcoming the current difficulties. Hydrological TOPMODEL is used to investigate the hydrological functioning of the páramo of Chingaza, through a case study in La Chucua basin. For this, we calibrate and validate the model using two data sets of climate and the hydrology of the basin (climate and discharge from 2008 and 2009, respectively). Through the calibration procedure we obtain a high efficiency value of 0.76 model (coefficient Nash - Sutcliffe), which adequately represents the hydrological behavior of the páramo. Simulations with better adjustment between measured and predicted values of discharge, have low values of surface infiltration excess runoff, indicating high water storage capacity on the soils. This agrees with the predominance of subsurface flow in studied ecosystem, given the special characteristics of soils. Results also show the large influence of factors represented in the model (topography and soils), on water basin response to rainfall events. This is significant evidence of exceptional hydrological behavior of the páramos, mainly related to the presence of soil with high organic matter content. These results imply that TOPMODEL is a robust tool, able to represent in a precise manner the hydrological functioning of the basin La Chucua, and consequently it is expected that TOPMODEL can also represent hydrological conditions of Chingaza páramo. Los páramos son ecosistemas localizados hacia las partes altas de las montañas, por debajo de las zonas de nieves perpetuas o en áreas aisladas, donde no hay glaciar. Estos ecosistemas son considerados importantes, tanto por su biodiversidad, como por ser fuente permanente de agua para poblaciones ubicadas hacia las partes medias y altas de las montañas andinas. Estudios recientes indican que ecosistemas localizados en altitudes altas, son más vulnerable al cambio climático y cambios en el uso del suelo, lo que pone en peligro los servicios ecosistémicos que se derivan desde estos. Son muy pocos los estudios realizados en estos ecosistemas, dentro de los cuales, estudios sobre su funcionamiento hidrológico son aún más escasos, lo que parece estar relacionado con las dificultades asociadas con el acceso a los mismos. Esto implica que existe una necesidad de generar herramientas que nos permitan estudiar estos ecosistemas, sobreponiéndose a las dificultades actuales. En este sentido en la presente investigación, se utilizó el modelo hidrológico TOPMODEL con el fin de investigar el funcionamiento hidrológico del páramo de Chingaza, a través de un estudio de caso en la cuenca La Chucua. Para esto se calibró y validó el modelo, mediante dos series de datos del clima y la hidrología de la cuenca (clima y caudales de los años 2008 y 2009, respectivamente), obteniéndose un valor alto de eficiencia del modelo de 0.76 (coeficiente Nash-Sutcliffe), el cual representa adecuadamente el comportamiento hidrológico del páramo. Las simulaciones de mayor ajuste presentaron bajos valores de escorrentía superficial por exceso de infiltración, lo que indica alta capacidad de almacenamiento de agua en el suelo, y coincide con la predominancia de la escorrentía subsuperficial, dadas las características especiales de los suelos allí presentes. Se comprobó la influencia que tienen los factores representados en el modelo (topografía y suelos), sobre la respuesta hídrica de la cuenca. Esto constituye evidencia significativa del comportamiento hídrico excepcional de los páramos, debido a sus suelos. Estos resultados implican que TOPMODEL es una herramienta robusta, capaz de representar de una manera precisa el funcionamiento hidrológico de la cuenca La Chucua, y por ende se espera que pueda representar igualmente las condiciones del páramo de Chingaza. Universidad Nacional de Colombia - Sede Medellín - Facultad de Ciencias Agrarias 2016-07-01 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion application/pdf text/html https://revistas.unal.edu.co/index.php/refame/article/view/59137 10.15446/rfna.v69n2.59137 Revista Facultad Nacional de Agronomía Medellín; Vol. 69 No. 2 (2016); 7919-7933 Revista Facultad Nacional de Agronomía Medellín; Vol. 69 Núm. 2 (2016); 7919-7933 Revista Facultad Nacional de Agronomía Medellín; v. 69 n. 2 (2016); 7919-7933 2248-7026 0304-2847 eng https://revistas.unal.edu.co/index.php/refame/article/view/59137/56791 https://revistas.unal.edu.co/index.php/refame/article/view/59137/57045 Copyright (c) 2016 Revista Facultad Nacional de Agronomía Medellín https://creativecommons.org/licenses/by-nc-nd/4.0/