Projected changes in drought characteristics over the Western Cape, South Africa

Abstract The devastating socioeconomic impacts of recent droughts in the Western Cape have intensified the quest for future drought mitigation measures. While ongoing global warming may increase atmospheric evaporative demand and worsen drought conditions, most studies on drought in the Western Cape...

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Published in:Meteorological Applications
Main Authors: Myra Naik, Babatunde J. Abiodun
Format: Article
Language:English
Published: Wiley 2020-01-01
Subjects:
Online Access:https://doi.org/10.1002/met.1802
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author Myra Naik
Babatunde J. Abiodun
author_facet Myra Naik
Babatunde J. Abiodun
author_sort Myra Naik
collection DOAJ
container_title Meteorological Applications
description Abstract The devastating socioeconomic impacts of recent droughts in the Western Cape have intensified the quest for future drought mitigation measures. While ongoing global warming may increase atmospheric evaporative demand and worsen drought conditions, most studies on drought in the Western Cape have overlooked the role of potential evapotranspiration (PET). The present study examines the role of PET on future drought characteristics, focusing on four river catchments. Two drought indices, the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI), were analysed. The capability of the Co‐ordinated Regional Downscaling Experiment simulations to reproduce the drought characteristics was evaluated by comparing present‐day climate simulations with observations. The impacts of different global warming levels (GWLs) on the SPI and SPEI projections were assessed using self‐organizing map (SOM) classifications. The results project that a robust drying signal across the Western Cape, but the magnitudes of the projections, which vary across the river catchments, increase with the GWLs. The changes in the drought intensity and frequency are weaker when using the SPI than the SPEI, suggesting that SPI projections may underestimate the influence of global warming on drought because they do not account for the influence of PET. The SOM classification confirms the differences between the two drought indices reveals the drought patterns that are not seen in the drought ensemble means. Nevertheless, the study underscores the need to mitigate future drought impacts over the Western Cape, but with careful consideration on the drought index used in characterizing the droughts.
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spelling doaj-art-1dbcaee7cb9b425aa8795b69c3f1d7602025-08-19T20:16:49ZengWileyMeteorological Applications1350-48271469-80802020-01-01271n/an/a10.1002/met.1802Projected changes in drought characteristics over the Western Cape, South AfricaMyra Naik0Babatunde J. Abiodun1Department of Environmental and Geographical Science, Climate System Analysis Group University of Cape Town Cape Town South AfricaDepartment of Environmental and Geographical Science, Climate System Analysis Group University of Cape Town Cape Town South AfricaAbstract The devastating socioeconomic impacts of recent droughts in the Western Cape have intensified the quest for future drought mitigation measures. While ongoing global warming may increase atmospheric evaporative demand and worsen drought conditions, most studies on drought in the Western Cape have overlooked the role of potential evapotranspiration (PET). The present study examines the role of PET on future drought characteristics, focusing on four river catchments. Two drought indices, the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI), were analysed. The capability of the Co‐ordinated Regional Downscaling Experiment simulations to reproduce the drought characteristics was evaluated by comparing present‐day climate simulations with observations. The impacts of different global warming levels (GWLs) on the SPI and SPEI projections were assessed using self‐organizing map (SOM) classifications. The results project that a robust drying signal across the Western Cape, but the magnitudes of the projections, which vary across the river catchments, increase with the GWLs. The changes in the drought intensity and frequency are weaker when using the SPI than the SPEI, suggesting that SPI projections may underestimate the influence of global warming on drought because they do not account for the influence of PET. The SOM classification confirms the differences between the two drought indices reveals the drought patterns that are not seen in the drought ensemble means. Nevertheless, the study underscores the need to mitigate future drought impacts over the Western Cape, but with careful consideration on the drought index used in characterizing the droughts.https://doi.org/10.1002/met.1802climate changedroughtevapotranspirationriver catchmentsSouth AfricaWestern Cape
spellingShingle Myra Naik
Babatunde J. Abiodun
Projected changes in drought characteristics over the Western Cape, South Africa
climate change
drought
evapotranspiration
river catchments
South Africa
Western Cape
title Projected changes in drought characteristics over the Western Cape, South Africa
title_full Projected changes in drought characteristics over the Western Cape, South Africa
title_fullStr Projected changes in drought characteristics over the Western Cape, South Africa
title_full_unstemmed Projected changes in drought characteristics over the Western Cape, South Africa
title_short Projected changes in drought characteristics over the Western Cape, South Africa
title_sort projected changes in drought characteristics over the western cape south africa
topic climate change
drought
evapotranspiration
river catchments
South Africa
Western Cape
url https://doi.org/10.1002/met.1802
work_keys_str_mv AT myranaik projectedchangesindroughtcharacteristicsoverthewesterncapesouthafrica
AT babatundejabiodun projectedchangesindroughtcharacteristicsoverthewesterncapesouthafrica