Current and future water availability in the context of water insecurity in the Parón catchment, Santa River basin, Peru

Descripción del Articulo

Water security in Andean watersheds depends on adaptive water management in the face of glaciohydrological and socioeconomic impacts. The Parón sub-basin in the Santa River basin (Ancash, Peru) is a suitable case in this respect. Water is regulated by a floodgate in the Parón lake, which has become...

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Detalles Bibliográficos
Autores: Izaguirre Liviac, Marcos Fabio, Drenkhan, Fabian, Timaná, Martín
Formato: artículo
Fecha de Publicación:2024
Institución:Pontificia Universidad Católica del Perú
Repositorio:Revistas - Pontificia Universidad Católica del Perú
Lenguaje:español
OAI Identifier:oai:ojs.pkp.sfu.ca:article/26692
Enlace del recurso:http://revistas.pucp.edu.pe/index.php/Kawsaypacha/article/view/26692
Nivel de acceso:acceso abierto
Materia:Glacier retreat
Future scenarios
Water balance
Water security
Cordillera Blanca
Hydrological model
Peru
Retroceso glaciar
Escenarios futuros
Balance hídrico
Seguridad hídrica
Cordillera blanca
Modelo hidrológico
Perú
Descripción
Sumario:Water security in Andean watersheds depends on adaptive water management in the face of glaciohydrological and socioeconomic impacts. The Parón sub-basin in the Santa River basin (Ancash, Peru) is a suitable case in this respect. Water is regulated by a floodgate in the Parón lake, which has become a focal point of social conflict. This study analyzes the water balance of this sub-basin using a semi-distributed hydrological model for the present (2006-2016) and future (2030-2050), considering different scenarios of precipitation variation, glacial melting, and increased water demand. Without regulation of the lake, the sub-basin would enter into a strong water deficit in the dry months (June-August). Until 2030 (2050), assuming a maximum regulation of 2.6 m³/s, a 15% (35%) increase in precipitation, and a 10% (26%) decrease in the glacier contribution to the annual flow, water availability would be reduced by 37% (35%). In a pessimistic scenario with a 15% (35%) decrease in precipitation, water availability would still be reduced by 47% (56%) annually. These results highlight the need to keep a socially acceptable minimum water flow (>2 m³/s) to avoid critical levels of water scarcity in the dry months and to address the needs of local water users.
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