Análisis de variabilidad espacial y temporal de los caudales del río Cauca - Colombia

Studying the spatial and temporal variations of flow rates in Colombian rivers is an important step to guarantee water availability and to carry out adequate plans to prevent possible environmental or socioeconomic impacts that such variations may generate. This research aims to analyze the trends i...

Full description

Autores:
Peláez Baldovino, Aldair Abad
Barros Núñez, Samantha del Mar
Tipo de recurso:
Trabajo de grado de pregrado
Fecha de publicación:
2020
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
spa
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/6375
Acceso en línea:
https://hdl.handle.net/11323/6375
https://repositorio.cuc.edu.co/
Palabra clave:
Flows
Trends
Stationary
Mann Kendall
Sen slope
Cauca river
Río Cauca
Caudales
Tendencias
Estacionaria
Mann Kendall
Rights
openAccess
License
Attribution-NonCommercial-ShareAlike 4.0 International
Description
Summary:Studying the spatial and temporal variations of flow rates in Colombian rivers is an important step to guarantee water availability and to carry out adequate plans to prevent possible environmental or socioeconomic impacts that such variations may generate. This research aims to analyze the trends in the series of annual maximum and minimum flows of the Cauca River. Eight (8) stations of the main section of the river selected according to their location and the time window of data available in them (1970 - 2018) were selected for this investigation. The methods used to find the trends were the non-parametric Mann-Kendall and Sen's Slope tests, from which significant trends (with a confidence level of 95%) were detected in the series of annual maximums of 6 stations and in the series of annual minimums of 2 of them. The stations Las Varas and Tres Cruces presented significant increasing trends for the series of maximums and the series of minimums, which suggests an increase in the variability of the annual data. The trend detected in the upper part of the basin was decreasing (-0.57 to -2.17 m3 / year), while the trends detected in the lower basin were increasing (0.49 to 8.93 m3 / year). be related to the anthropic interventions carried out in the basin and to the variations of macro climatic phenomena such as the ENSO and the PDO.