Runoff from tropical alpine grasslands increases with areal extent of wetlands

Tropical alpine grasslands of the northern Andes, commonly known as the páramo, provide abundant high-quality water for downstream populations as well as a variety of other environmental services. Yet, very little is known about the role that landscape characteristics play in the hydrologic function...

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1. autor: Mosquera Rojas, Giovanny Mauricio (author)
Kolejni autorzy: Célleri Alvear, Rolando Enrique (author), Crespo Sánchez, Patricio Javier (author), Lazo Jara, Patricio Xavier (author)
Format: article
Wydane: 2015
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Dostęp online:https://www.scopus.com/inward/record.uri?eid=2-s2.0-84910087177&doi=10.1016%2fj.catena.2014.10.010&partnerID=40&md5=6892afce2b7dfe0d67bab1f4e3064f8a
http://dspace.ucuenca.edu.ec/handle/123456789/21989
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author Mosquera Rojas, Giovanny Mauricio
author2 Célleri Alvear, Rolando Enrique
Crespo Sánchez, Patricio Javier
Lazo Jara, Patricio Xavier
author2_role author
author
author
author_facet Mosquera Rojas, Giovanny Mauricio
Célleri Alvear, Rolando Enrique
Crespo Sánchez, Patricio Javier
Lazo Jara, Patricio Xavier
author_role author
collection Repositorio Universidad de Cuenca
dc.creator.none.fl_str_mv Mosquera Rojas, Giovanny Mauricio
Célleri Alvear, Rolando Enrique
Crespo Sánchez, Patricio Javier
Lazo Jara, Patricio Xavier
dc.date.none.fl_str_mv 2015-02-01
2018-01-11T21:21:51Z
2018-01-11T21:21:51Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv 3418162
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84910087177&doi=10.1016%2fj.catena.2014.10.010&partnerID=40&md5=6892afce2b7dfe0d67bab1f4e3064f8a
http://dspace.ucuenca.edu.ec/handle/123456789/21989
10.1016/j.catena.2014.10.010
dc.language.none.fl_str_mv en_US
dc.publisher.none.fl_str_mv ELSEVIER
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.source.none.fl_str_mv Catena
reponame:Repositorio Universidad de Cuenca
instname:Universidad de Cuenca
instacron:UCUENCA
dc.subject.none.fl_str_mv Andean Páramo Wetlands
Andes
Andosol And Histosol
Ecuador
Hydrologic Processes
Topography
dc.title.none.fl_str_mv Runoff from tropical alpine grasslands increases with areal extent of wetlands
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/article
description Tropical alpine grasslands of the northern Andes, commonly known as the páramo, provide abundant high-quality water for downstream populations as well as a variety of other environmental services. Yet, very little is known about the role that landscape characteristics play in the hydrologic functioning of these ecosystems. To help fill this knowledge gap, we investigated the relationships between various landscape attributes and hydrology in a wet páramo ecosystem of southern Ecuador. Using linear regression analysis, we examined the influence of soil type, vegetation cover, catchment area, geology, and topography on runoff coefficient, streamflow rates, and evapotranspiration. Our study site is located at the Zhurucay River experimental catchment, which is composed of seven nested microcatchments ranging in size from 0.20 to 7.53km2 and in elevation from 3200 to 3900ma.s.l. We found that (1) water yield accounts for a high percentage of the water budget; (2) runoff coefficient and specific discharge are strongly correlated with the extent of Andean páramo wetlands (Histosol soils and cushion plants), and also increase with catchment size; (3) conversely, inferred evapotranspiration is the highest in catchments having the greatest percentages of upland terrain (Andosol soils and tussock grasses); and (4) low flows are highly positively correlated with steep slopes. These results suggest that in the high-elevation tropical grasslands of the Andes, runoff coefficient and specific discharge increase with catchment size because as catchment size increases, so does the relative area of permanently near-saturation zones (Andean páramo wetlands); likely because of reduced available storage capacity of the Andean páramo wetlands, and their hydrologic connectivity to the stream network.
eu_rights_str_mv openAccess
format article
id UCUENCA_e74865018c2021a9fc06659566614ac0
identifier_str_mv 3418162
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network_acronym_str UCUENCA
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oai_identifier_str oai:dspace.ucuenca.edu.ec:123456789/21989
publishDate 2015
publisher.none.fl_str_mv ELSEVIER
reponame_str Repositorio Universidad de Cuenca
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repository.name.fl_str_mv Repositorio Universidad de Cuenca - Universidad de Cuenca
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spelling Runoff from tropical alpine grasslands increases with areal extent of wetlandsMosquera Rojas, Giovanny MauricioCélleri Alvear, Rolando EnriqueCrespo Sánchez, Patricio JavierLazo Jara, Patricio XavierAndean Páramo WetlandsAndesAndosol And HistosolEcuadorHydrologic ProcessesTopographyTropical alpine grasslands of the northern Andes, commonly known as the páramo, provide abundant high-quality water for downstream populations as well as a variety of other environmental services. Yet, very little is known about the role that landscape characteristics play in the hydrologic functioning of these ecosystems. To help fill this knowledge gap, we investigated the relationships between various landscape attributes and hydrology in a wet páramo ecosystem of southern Ecuador. Using linear regression analysis, we examined the influence of soil type, vegetation cover, catchment area, geology, and topography on runoff coefficient, streamflow rates, and evapotranspiration. Our study site is located at the Zhurucay River experimental catchment, which is composed of seven nested microcatchments ranging in size from 0.20 to 7.53km2 and in elevation from 3200 to 3900ma.s.l. We found that (1) water yield accounts for a high percentage of the water budget; (2) runoff coefficient and specific discharge are strongly correlated with the extent of Andean páramo wetlands (Histosol soils and cushion plants), and also increase with catchment size; (3) conversely, inferred evapotranspiration is the highest in catchments having the greatest percentages of upland terrain (Andosol soils and tussock grasses); and (4) low flows are highly positively correlated with steep slopes. These results suggest that in the high-elevation tropical grasslands of the Andes, runoff coefficient and specific discharge increase with catchment size because as catchment size increases, so does the relative area of permanently near-saturation zones (Andean páramo wetlands); likely because of reduced available storage capacity of the Andean páramo wetlands, and their hydrologic connectivity to the stream network.ELSEVIER2018-01-11T21:21:51Z2018-01-11T21:21:51Z2015-02-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdf3418162https://www.scopus.com/inward/record.uri?eid=2-s2.0-84910087177&doi=10.1016%2fj.catena.2014.10.010&partnerID=40&md5=6892afce2b7dfe0d67bab1f4e3064f8ahttp://dspace.ucuenca.edu.ec/handle/123456789/2198910.1016/j.catena.2014.10.010Catenareponame:Repositorio Universidad de Cuencainstname:Universidad de Cuencainstacron:UCUENCAen_USinfo:eu-repo/semantics/openAccess2025-03-27T16:46:15Zoai:dspace.ucuenca.edu.ec:123456789/21989Institucionalhttp://dspace.ucuenca.edu.ec/Universidad públicahttps://www.ucuenca.edu.ec/http://dspace.ucuenca.edu.ec/oai.Ecuador...opendoar:41862025-08-09T06:54:45.173480Repositorio Universidad de Cuenca - Universidad de Cuencatrue
spellingShingle Runoff from tropical alpine grasslands increases with areal extent of wetlands
Mosquera Rojas, Giovanny Mauricio
Andean Páramo Wetlands
Andes
Andosol And Histosol
Ecuador
Hydrologic Processes
Topography
status_str publishedVersion
title Runoff from tropical alpine grasslands increases with areal extent of wetlands
title_full Runoff from tropical alpine grasslands increases with areal extent of wetlands
title_fullStr Runoff from tropical alpine grasslands increases with areal extent of wetlands
title_full_unstemmed Runoff from tropical alpine grasslands increases with areal extent of wetlands
title_short Runoff from tropical alpine grasslands increases with areal extent of wetlands
title_sort Runoff from tropical alpine grasslands increases with areal extent of wetlands
topic Andean Páramo Wetlands
Andes
Andosol And Histosol
Ecuador
Hydrologic Processes
Topography
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-84910087177&doi=10.1016%2fj.catena.2014.10.010&partnerID=40&md5=6892afce2b7dfe0d67bab1f4e3064f8a
http://dspace.ucuenca.edu.ec/handle/123456789/21989