Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components

<p>Although water balance components at the catchment scale are strongly related to annual rainfall, the availability of water resources in Mediterranean catchments also depends on rainfall seasonality. Observed seasonal anomalies in historical records are fairly episodic, but an increase in t...

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Main Authors: P. Nasta, C. Allocca, R. Deidda, N. Romano
Format: Article
Language:English
Published: Copernicus Publications 2020-06-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/24/3211/2020/hess-24-3211-2020.pdf
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spelling doaj-9c6ad25c2e144b318efe983043858e532020-11-25T03:03:40ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-06-01243211322710.5194/hess-24-3211-2020Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance componentsP. Nasta0C. Allocca1R. Deidda2N. Romano3N. Romano4Department of Agricultural Sciences, AFBE Division, University of Naples Federico II, Portici (Naples), ItalyDepartment of Agricultural Sciences, AFBE Division, University of Naples Federico II, Portici (Naples), ItalyDepartment of Civil and Environmental Engineering and Architecture, University of Cagliari, Cagliari, ItalyDepartment of Agricultural Sciences, AFBE Division, University of Naples Federico II, Portici (Naples), ItalyThe Interdepartmental Research Center for Environmental Research (C.I.R.AM.), University of Naples Federico II, Naples, Italy<p>Although water balance components at the catchment scale are strongly related to annual rainfall, the availability of water resources in Mediterranean catchments also depends on rainfall seasonality. Observed seasonal anomalies in historical records are fairly episodic, but an increase in their frequency might exacerbate water deficit or water excess if the rainy season shortens or extends its duration, e.g., due to climate change. This study evaluates the sensitivity of water yield, evapotranspiration, and groundwater recharge to changes in rainfall seasonality by using the Soil Water Assessment Tool (SWAT) model applied to the upper Alento River catchment (UARC) in southern Italy, where a long time series of daily rainfall is available from 1920 to 2018. We compare two distinct approaches: (i) a “static” approach, where three seasonal features (namely rainy, dry, and transition fixed-duration 4-month seasons) are identified through the standardized precipitation index (SPI) and (ii) a “dynamic” approach based on a stochastic framework, where the duration of two seasons (rainy and dry seasons) varies from year to year according to a probability distribution. Seasonal anomalies occur when the transition season is replaced by the rainy or dry season in the first approach and when season duration occurs in the tails of its normal distribution in the second approach. Results are presented within a probabilistic framework. We also show that the Budyko curve is sensitive to the rainfall seasonality regime in UARC by questioning the implicit assumption of a temporal steady state between annual average dryness and the evaporative index. Although the duration of the rainy season does not exert a major control on water balance, we were able to identify season-dependent regression equations linking water yield to the dryness index in the rainy season.</p>https://www.hydrol-earth-syst-sci.net/24/3211/2020/hess-24-3211-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Nasta
C. Allocca
R. Deidda
N. Romano
N. Romano
spellingShingle P. Nasta
C. Allocca
R. Deidda
N. Romano
N. Romano
Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
Hydrology and Earth System Sciences
author_facet P. Nasta
C. Allocca
R. Deidda
N. Romano
N. Romano
author_sort P. Nasta
title Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
title_short Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
title_full Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
title_fullStr Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
title_full_unstemmed Assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
title_sort assessing the impact of seasonal-rainfall anomalies on catchment-scale water balance components
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2020-06-01
description <p>Although water balance components at the catchment scale are strongly related to annual rainfall, the availability of water resources in Mediterranean catchments also depends on rainfall seasonality. Observed seasonal anomalies in historical records are fairly episodic, but an increase in their frequency might exacerbate water deficit or water excess if the rainy season shortens or extends its duration, e.g., due to climate change. This study evaluates the sensitivity of water yield, evapotranspiration, and groundwater recharge to changes in rainfall seasonality by using the Soil Water Assessment Tool (SWAT) model applied to the upper Alento River catchment (UARC) in southern Italy, where a long time series of daily rainfall is available from 1920 to 2018. We compare two distinct approaches: (i) a “static” approach, where three seasonal features (namely rainy, dry, and transition fixed-duration 4-month seasons) are identified through the standardized precipitation index (SPI) and (ii) a “dynamic” approach based on a stochastic framework, where the duration of two seasons (rainy and dry seasons) varies from year to year according to a probability distribution. Seasonal anomalies occur when the transition season is replaced by the rainy or dry season in the first approach and when season duration occurs in the tails of its normal distribution in the second approach. Results are presented within a probabilistic framework. We also show that the Budyko curve is sensitive to the rainfall seasonality regime in UARC by questioning the implicit assumption of a temporal steady state between annual average dryness and the evaporative index. Although the duration of the rainy season does not exert a major control on water balance, we were able to identify season-dependent regression equations linking water yield to the dryness index in the rainy season.</p>
url https://www.hydrol-earth-syst-sci.net/24/3211/2020/hess-24-3211-2020.pdf
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