Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador

Study region: Quito, Ecuador Study focus: The study region faces two water-related challenges, which, to date, have only been studied to a minimal extent: extreme precipitation events and water shortage in the dry season. This study investigates the current conditions and future changes in short-dur...

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Main Authors: Santiago X. Núñez Mejía, Santiago Mendoza Paz, Hossein Tabari, Patrick Willems
Format: Article
Language:English
Published: Elsevier 2023-10-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581823002094
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author Santiago X. Núñez Mejía
Santiago Mendoza Paz
Hossein Tabari
Patrick Willems
author_facet Santiago X. Núñez Mejía
Santiago Mendoza Paz
Hossein Tabari
Patrick Willems
author_sort Santiago X. Núñez Mejía
collection DOAJ
description Study region: Quito, Ecuador Study focus: The study region faces two water-related challenges, which, to date, have only been studied to a minimal extent: extreme precipitation events and water shortage in the dry season. This study investigates the current conditions and future changes in short-duration events, low river discharges and associated uncertainties. Daily precipitation and temperature projections from 19 state-of-the-art global climate models (CMIP6) and four future scenarios (SSP1–2.6, SSP2–4.5, SSP3–7.0 and SSP5–8.5) are downscaled with delta change and more advanced quantile perturbation methodologies. Temporal disaggregation is applied to obtain sub-daily precipitation with five extreme value distributions (EVDs). Three conceptual hydrological models are implemented to quantify the impacts on river flows. Variance decomposition is applied to estimate the uncertainty share of climate models, hydrological models, and EVDs in the results. New hydrological insights: The results indicate an intensification of extreme precipitation events, with short-duration events expected to be more intense by up to 30% in the near future (2021–2050) and up to 60% in the far future (2070–2099). The river peak discharges are projected to increase by 5–20% and 10–50% in the near and far future, respectively. On the contrary, the low river flows are projected to decrease by 0–13% and 0–30% for the respective time horizons. Overall, climate models are the dominant source of uncertainty.
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spelling doaj.art-c00b0ca0e1954e6999023450b14b2d772023-09-11T04:17:17ZengElsevierJournal of Hydrology: Regional Studies2214-58182023-10-0149101522Climate change impacts on hydrometeorological and river hydrological extremes in Quito, EcuadorSantiago X. Núñez Mejía0Santiago Mendoza Paz1Hossein Tabari2Patrick Willems3Universidad del Azuay, TRACES & Faculty of Science and Technology, Cuenca, Ecuador; Department of Water Resources and Environmental Sciences, University of Cuenca, Ecuador; Correspondence to: Av.24 de Mayo 7-77, Cuenca, Ecuador.Hydraulics and Geotechnics Section, Department of Civil Engineering, KU Leuven, Leuven 3001, BelgiumFaculty of Applied Engineering - IDLab, University of Antwerp, Antwerp, Belgium; Department of Meteorological and Climate Research, Royal Meteorological Institute of Belgium, Uccle, BelgiumHydraulics and Geotechnics Section, Department of Civil Engineering, KU Leuven, Leuven 3001, BelgiumStudy region: Quito, Ecuador Study focus: The study region faces two water-related challenges, which, to date, have only been studied to a minimal extent: extreme precipitation events and water shortage in the dry season. This study investigates the current conditions and future changes in short-duration events, low river discharges and associated uncertainties. Daily precipitation and temperature projections from 19 state-of-the-art global climate models (CMIP6) and four future scenarios (SSP1–2.6, SSP2–4.5, SSP3–7.0 and SSP5–8.5) are downscaled with delta change and more advanced quantile perturbation methodologies. Temporal disaggregation is applied to obtain sub-daily precipitation with five extreme value distributions (EVDs). Three conceptual hydrological models are implemented to quantify the impacts on river flows. Variance decomposition is applied to estimate the uncertainty share of climate models, hydrological models, and EVDs in the results. New hydrological insights: The results indicate an intensification of extreme precipitation events, with short-duration events expected to be more intense by up to 30% in the near future (2021–2050) and up to 60% in the far future (2070–2099). The river peak discharges are projected to increase by 5–20% and 10–50% in the near and far future, respectively. On the contrary, the low river flows are projected to decrease by 0–13% and 0–30% for the respective time horizons. Overall, climate models are the dominant source of uncertainty.http://www.sciencedirect.com/science/article/pii/S2214581823002094Climate changeStatistical downscalingTemporal downscalingIDF curvesSub-daily precipitation extremesConceptual hydrological models
spellingShingle Santiago X. Núñez Mejía
Santiago Mendoza Paz
Hossein Tabari
Patrick Willems
Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
Journal of Hydrology: Regional Studies
Climate change
Statistical downscaling
Temporal downscaling
IDF curves
Sub-daily precipitation extremes
Conceptual hydrological models
title Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
title_full Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
title_fullStr Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
title_full_unstemmed Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
title_short Climate change impacts on hydrometeorological and river hydrological extremes in Quito, Ecuador
title_sort climate change impacts on hydrometeorological and river hydrological extremes in quito ecuador
topic Climate change
Statistical downscaling
Temporal downscaling
IDF curves
Sub-daily precipitation extremes
Conceptual hydrological models
url http://www.sciencedirect.com/science/article/pii/S2214581823002094
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