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Large-scale mechanisms linked to anomalously wet summers over the southwestern Cape, South Africa

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Abstract

Although on average, the southwestern Cape (SWC) of South Africa is a winter rainfall dominated region, almost 30% of the total rainfall occurs during the extended summer (October-March). A previous study showed that anomalously wet summers may help mitigate the effects of severe winter drought. Apart from that study, very little work has been done on summer rainfall variability over the SWC or the mechanisms associated with it. Here, station data and ERA5 reanalyses are used to investigated summer rainfall day variability and associated mechanisms. Interannual variability in summer rainfall day frequencies appears related to that in the South Atlantic High Pressure (SAHP) and westerly moisture fluxes across the midlatitude South Atlantic. Increased rainfall days are associated with cyclonic anomalies over the region and enhanced westerly moisture fluxes. Some of these circulation changes are related to the Southern Annular Mode, and in late summer, also to ENSO and changes in the zonal wavenumber 3 pattern. Significant decreasing trends in rainfall days were found in the mid- and late summer for the southern part of the region where most of the population lives and the main water supply dams are located. These trends seem associated with significant trends found in the southern boundary of the SAHP and in decreasing (increasing) South Atlantic storm counts in the 35°–45° S (50°–60° S) latitude bands.

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Data availability statement

Station rainfall data used in this study are available upon request from the South African Weather Service (SAWS) (http://www.weathersa.so.za). ERA5 reanalysis was sourced from the Copernicus Climate Data Store (https://cds.climate.copernicus.eu/). The SAM and ENSO indices were obtained from the Climate Explorer portal (http://climexp.knmi.nl/ ). The Gramcianinov et al. (2020) extratropical cyclone track data is available at (https://data.mendeley.com/datasets/kwcvfr52hp/3). The OISSTv2 is available on the NOAA website (https://psl.noaa.gov/data/gridded/data.noaa.oisst.v2.highres.html) to calculate the SAOD and SIOD.

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Acknowledgements

WDK was funded by the National Research Foundation (NRF) of South Africa through the ACSyS and SANAP projects. RCB acknowledges support of the FLAIR programme, a partnership between the African Academy of Sciences and the Royal Society funded by the UK Government’s Global Challenges Research Fund. The authors thank all the listed institutions above for making the data available.

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This study was funded by National Research Foundation.

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Correspondence to W. M. De Kock.

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De Kock, W.M., Blamey, R.C. & Reason, C.J.C. Large-scale mechanisms linked to anomalously wet summers over the southwestern Cape, South Africa. Clim Dyn 59, 3503–3517 (2022). https://doi.org/10.1007/s00382-022-06280-7

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  • DOI: https://doi.org/10.1007/s00382-022-06280-7

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