Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin

The effects of climate change projected for 2050 to 2079 relative to the 1968–2014 reference period were evaluated using 39 CMIP5 models under the RCP8.5 emissions scenario in the Guayas River basin. The monthly normalized precipitation index (SPI) was used in this study to assess the impact of clim...

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Autores principales: Mercy Ilbay-Yupa, Franklin Ilbay, Ricardo Zubieta, Mario García-Mora, Paolo Chasi
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/5d8e0e5526ca43b49cd700de24fe8055
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spelling oai:doaj.org-article:5d8e0e5526ca43b49cd700de24fe80552021-11-11T19:58:26ZImpacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin10.3390/w132131382073-4441https://doaj.org/article/5d8e0e5526ca43b49cd700de24fe80552021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3138https://doaj.org/toc/2073-4441The effects of climate change projected for 2050 to 2079 relative to the 1968–2014 reference period were evaluated using 39 CMIP5 models under the RCP8.5 emissions scenario in the Guayas River basin. The monthly normalized precipitation index (SPI) was used in this study to assess the impact of climate change for wet events and droughts from a meteorological perspective. The GR2M model was used to project changes in the streamflow of the Daule River. The climate projection was based on the four rigorously selected models to represent the climate of the study area. On average, an increase in temperature (~2 °C) and precipitation (~6%) is expected. A 7% increase in precipitation would result in a 10% increase in streamflow for flood periods, while an 8% decrease in precipitation could result in approximately a 60% reduction in flow for dry periods. The analysis of droughts shows that they will be more frequent and prolonged in the highlands (Andes) and the middle part of the basin. In the future, wet periods will be less frequent but of greater duration and intensity on the Ecuadorian coast. These results point to future problems such as water deficit in the dry season but also increased streamflow for floods during the wet season. This information should be taken into account in designing strategies for adaptation to climate change.Mercy Ilbay-YupaFranklin IlbayRicardo ZubietaMario García-MoraPaolo ChasiMDPI AGarticleclimate changedroughtsGuayasEcuadorimpactsHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3138, p 3138 (2021)
institution DOAJ
collection DOAJ
language EN
topic climate change
droughts
Guayas
Ecuador
impacts
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle climate change
droughts
Guayas
Ecuador
impacts
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Mercy Ilbay-Yupa
Franklin Ilbay
Ricardo Zubieta
Mario García-Mora
Paolo Chasi
Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
description The effects of climate change projected for 2050 to 2079 relative to the 1968–2014 reference period were evaluated using 39 CMIP5 models under the RCP8.5 emissions scenario in the Guayas River basin. The monthly normalized precipitation index (SPI) was used in this study to assess the impact of climate change for wet events and droughts from a meteorological perspective. The GR2M model was used to project changes in the streamflow of the Daule River. The climate projection was based on the four rigorously selected models to represent the climate of the study area. On average, an increase in temperature (~2 °C) and precipitation (~6%) is expected. A 7% increase in precipitation would result in a 10% increase in streamflow for flood periods, while an 8% decrease in precipitation could result in approximately a 60% reduction in flow for dry periods. The analysis of droughts shows that they will be more frequent and prolonged in the highlands (Andes) and the middle part of the basin. In the future, wet periods will be less frequent but of greater duration and intensity on the Ecuadorian coast. These results point to future problems such as water deficit in the dry season but also increased streamflow for floods during the wet season. This information should be taken into account in designing strategies for adaptation to climate change.
format article
author Mercy Ilbay-Yupa
Franklin Ilbay
Ricardo Zubieta
Mario García-Mora
Paolo Chasi
author_facet Mercy Ilbay-Yupa
Franklin Ilbay
Ricardo Zubieta
Mario García-Mora
Paolo Chasi
author_sort Mercy Ilbay-Yupa
title Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
title_short Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
title_full Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
title_fullStr Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
title_full_unstemmed Impacts of Climate Change on the Precipitation and Streamflow Regimes in Equatorial Regions: Guayas River Basin
title_sort impacts of climate change on the precipitation and streamflow regimes in equatorial regions: guayas river basin
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/5d8e0e5526ca43b49cd700de24fe8055
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