Spatio‐temporal patterns of rainfall trends and the 2015–2017 drought over the winter rainfall region of South Africa. (19th August 2020)

• Record Type: Journal Article
• Authors: Wolski, Piotr; Conradie, Stefaan; Jack, Christopher; Tadross, Mark
• Is Part Of: International journal of climatology. Volume 41(2021)Supplement 1
• Page Start: E1303
• Page End: E1319
• Publication Date: 2020-08-19
• Subjects: drought -- Mediterranean climate -- rainfall trend; Climatology -- Periodicals; Climat -- Périodiques; Climatologie -- Périodiques; 551.605
• DOI: 10.1002/joc.6768
• Languages: English
• ISSNs: 0899-8418

Abstract

Abstract: We analyse long‐term (1900–2017) rainfall data in the southern part of the winter rainfall region of southern Africa to understand the spatial patterns of recent and long‐term trends and contextualize the 2015–2017 rainfall anomalies which led to the so‐called "Day Zero" drought in Cape Town. Our analyses reveal cohesive spatial patterns and seasonal differences in rainfall trends across a range of timescales. These suggest that rainfall is subject to regional driving mechanisms, predominantly manifested at the 20–50 year timescale, but the influence of these mechanisms is modified by subregional and seasonally specific processes, frequently resulting in trends of different magnitudes and even sign. Trend patterns are consistent with multidecadal‐scale quasi‐periodicity, with only the most recent phase (post‐1981 drying) corresponding to the expected regional response to hemispheric processes linked to anthropogenic climate change. The spatial and seasonal patterns of drying observed since 1981 alone do not explain the pattern of 2015–2017 drought anomalies, although they share a strong autumn and weak mid‐winter signal. These results have implications to the interpretation of drought in the context of observed rainfall trends. Furthermore, we identify directions for improvement of the conceptual understanding of drivers of rainfall variability and the role of anthropogenic climate change in the winter rainfall region of South Africa. Abstract : We reveal robust but divergent spatial and seasonal patterns in rainfall trends in the Cape Town region. These reflect influence of common regional forcing modified by subregional and seasonally specific processes. Trends are embedded within a multidecadal quasiperiodicity, but in recent period are consistent with hemispheric forcing reflecting anthropogenic climate change. Results have implications for interpretation of rainfall trends in the context of drought, and to understanding of climate drivers of rainfall variability this and similar regions.