Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective

The Cauca River rises in the Colombian Andes and is the main tributary of the Magdalena River, which drains to the Caribbean Sea. The La Balsa station monitors the Upper Cauca basin and is located just downstream of La Salvajina hydroelectric facility. At this station, the discharge time series for...

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Autores principales: Wilmar L. Cerón, Mary T. Kayano, Camilo Ocampo-Marulanda, Teresita Canchala, Irma Ayes Rivera, Alvaro Avila-Diaz, Rita V. Andreoli, Itamara Parente de Souza
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/38d7984a18eb431e8a960b99aec5d063
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spelling oai:doaj.org-article:38d7984a18eb431e8a960b99aec5d0632021-11-25T16:45:53ZSpatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective10.3390/atmos121115272073-4433https://doaj.org/article/38d7984a18eb431e8a960b99aec5d0632021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1527https://doaj.org/toc/2073-4433The Cauca River rises in the Colombian Andes and is the main tributary of the Magdalena River, which drains to the Caribbean Sea. The La Balsa station monitors the Upper Cauca basin and is located just downstream of La Salvajina hydroelectric facility. At this station, the discharge time series for November–January during 1950–2019 shows a statistically significant downward break, and change of distribution after 1986 has been documented after La Salvajina started operation. We assessed the spatio-temporal variability of hydroclimatology in the upper Cauca River basin during the pre- and post-Salvajina dam periods to better understand this break. Post-Salvajina, low (high) discharge events are linked to negative (positive) precipitation and soil moisture anomalies that are greater in magnitude and extension than those recorded in the pre-Salvajina period in response to the more intense El Niño events (more intense and frequent central La Niña events) after 1986. Therefore, it is necessary to consider possible future rainfall scenarios and non-infrastructure measures (i.e., reforestation, territorial planning, integrated watershed management, etc.) to mitigate floods and droughts impacts. The contribution of this study is to provide evidence for the need for foresight in the design of any structural or non-structural flood measures.Wilmar L. CerónMary T. KayanoCamilo Ocampo-MarulandaTeresita CanchalaIrma Ayes RiveraAlvaro Avila-DiazRita V. AndreoliItamara Parente de SouzaMDPI AGarticleCauca river basinLa Salvajinaclimate variabilitywater dischargeMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1527, p 1527 (2021)
institution DOAJ
collection DOAJ
language EN
topic Cauca river basin
La Salvajina
climate variability
water discharge
Meteorology. Climatology
QC851-999
spellingShingle Cauca river basin
La Salvajina
climate variability
water discharge
Meteorology. Climatology
QC851-999
Wilmar L. Cerón
Mary T. Kayano
Camilo Ocampo-Marulanda
Teresita Canchala
Irma Ayes Rivera
Alvaro Avila-Diaz
Rita V. Andreoli
Itamara Parente de Souza
Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
description The Cauca River rises in the Colombian Andes and is the main tributary of the Magdalena River, which drains to the Caribbean Sea. The La Balsa station monitors the Upper Cauca basin and is located just downstream of La Salvajina hydroelectric facility. At this station, the discharge time series for November–January during 1950–2019 shows a statistically significant downward break, and change of distribution after 1986 has been documented after La Salvajina started operation. We assessed the spatio-temporal variability of hydroclimatology in the upper Cauca River basin during the pre- and post-Salvajina dam periods to better understand this break. Post-Salvajina, low (high) discharge events are linked to negative (positive) precipitation and soil moisture anomalies that are greater in magnitude and extension than those recorded in the pre-Salvajina period in response to the more intense El Niño events (more intense and frequent central La Niña events) after 1986. Therefore, it is necessary to consider possible future rainfall scenarios and non-infrastructure measures (i.e., reforestation, territorial planning, integrated watershed management, etc.) to mitigate floods and droughts impacts. The contribution of this study is to provide evidence for the need for foresight in the design of any structural or non-structural flood measures.
format article
author Wilmar L. Cerón
Mary T. Kayano
Camilo Ocampo-Marulanda
Teresita Canchala
Irma Ayes Rivera
Alvaro Avila-Diaz
Rita V. Andreoli
Itamara Parente de Souza
author_facet Wilmar L. Cerón
Mary T. Kayano
Camilo Ocampo-Marulanda
Teresita Canchala
Irma Ayes Rivera
Alvaro Avila-Diaz
Rita V. Andreoli
Itamara Parente de Souza
author_sort Wilmar L. Cerón
title Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
title_short Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
title_full Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
title_fullStr Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
title_full_unstemmed Spatio-Temporal Variability of Hydroclimatology in the Upper Cauca River Basin in Southwestern Colombia: Pre- and Post-Salvajina Dam Perspective
title_sort spatio-temporal variability of hydroclimatology in the upper cauca river basin in southwestern colombia: pre- and post-salvajina dam perspective
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/38d7984a18eb431e8a960b99aec5d063
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