Water dynamics over a Western Patagonian watershed: Land surface changes and human factors

Indexado

WoS: WOS:000704389800012

Scopus: SCOPUS_ID:85114690810

Año

2022

Tipo

artículo de investigación

0
Citas Totales
0
Autores Afiliación Chile
0
Instituciones Chile
0
% Participación Internacional
0
Autores Afiliación Extranjera
0
Instituciones Extranjeras

Abstract

Warming trends in Patagonia and severe droughts in recent decades are still poorly understood in terms of their hydrological effects. The effects of climate change on water dynamics in addition to human water management could generate a future water scarcity scenario in one of the regions with the most abundant water resources of Chile. The aim of this work is to focus on assessing the impacts of warming trends on water dynamics in the Patagonian Simpson River watershed during the last two decades. We estimated anomalies in the main components of water balance such as precipitation (P), snow cover (SC), evapotranspiration (ET) and streamflows (Q) as well as surface variables and meteorological forcing (i.e. air temperature - Ta, solar radiation -RS, land surface temperature - LST). The processed data were obtained from remote sensing, reanalysis and in-situ data. We implemented a trend analysis for each variable in the period 2000-2019 at monthly, seasonal and annual scale. Results showed a warming trend in Ta and LST of about 1.2 degrees C and 2.1 degrees C, respectively, concentrated mainly in the autumn and winter seasons. Although P showed non-significant trends, Q diminished significantly at rates of more than 9.1 m3/s/decade, representing 36% of its historical mean. However, the decreases in Q are seen only in the maximum (spring) and minimum (summer) seasonal flows. These decreases are explained by significant increases in ET, led by a positive feedback of its drivers (LST, Ta and RS), which is directly linked to the impact of warming and an associated vegetation greenness in the watershed, as well as a decrease in SC during winter that feeds the Simpson River during spring and summer. The decrease in Q is reinforced by the intensifi-cation of water withdrawals in recent decades, as shown by an accelerated increase in water rights for agricultural and drinking uses. In a context of water scarcity and increasing and extreme droughts, this work contributes to further understanding water dynamics in western Patagonia, providing support for policy and decision-making when defining sustainable productive practices at watershed scale. (C) 2021 Published by Elsevier B.V.

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Disciplinas de Investigación

WOS
Environmental Sciences
Scopus
Waste Management And Disposal
Pollution
Environmental Engineering
Environmental Chemistry
SciELO
Sin Disciplinas
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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

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Financiamiento

Fuente
Fondo Nacional de Desarrollo Científico y Tecnológico
Comisión Nacional de Investigación Científica y Tecnológica
Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias
ANID
MODIS
ECMWF
FONDECYT Regular (CONICYT)
Research and Education Foundation, Sligo General Hospital
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Agradecimientos

Agradecimiento
The authors would like to thank the ECMWF for the ERA-Interimproducts and the MODIS team for the land surface products. This work was supported in part by the FONDECYT Regular (CONICYT/ref-1181155). C.Z.E. would like to thank ANID/FONDAP/15110009 program.
The authors would like to thank the ECMWF for the ERA-Interim products and the MODIS team for the land surface products. This work was supported in part by the FONDECYT Regular ( CONICYT/ref-1181155 ). C.Z.E. would like to thank ANID/FONDAP/ 15110009 program.
The authors would like to thank the ECMWF for the ERA-Interim products and the MODIS team for the land surface products. This work was supported in part by the FONDECYT Regular ( CONICYT/ref-1181155 ). C.Z.E. would like to thank ANID/FONDAP/ 15110009 program.
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