Decadal and multidecadal natural variability of African rainfall

• Published in: Journal of Hydrology: Regional Studies
• Main Authors: Horst-Joachim Lüdecke, Gisela Müller-Plath, Michael G. Wallace, Sebastian Lüning
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2021
• Subjects: Precipitation; Natural variability; Modes of variability; Sahel; Atlantic Multidecadal Oscillation; North Atlantic Oscillation; Physical geography; GB3-5030; Geology; QE1-996.5; Pacific; Indian; North Atlantic; North Atlantic oscillation
• Online Access: https://doi.org/10.1016/j.ejrh.2021.100795; https://doaj.org/article/8ec5b56cacfa4e079dd64aa1d3398e27

Study region: Africa Study focus: African rainfall shows significant year-to-year natural fluctuations that in part are linked to teleconnections associated with modes of variability in the Atlantic, Pacific and Indian oceans. A better understanding of African rainfall variability and potential drivers would help to better prepare African societies for anticipated droughts and floods by taking early precautionary action. Here we are presenting the first continent-wide analysis of African rainfall variability on a month-by-month and country-by-country basis. We have calculated Pearson r values for smoothed monthly rainfall data of 49 African countries over the period 1901–2017 which we compared to six potential climatic drivers of natural variability, namely AMO, NAO, ENSO (El Niño Southern Oscillation), Pacific Decadal Oscillation (PDO), Indian Ocean Dipole (IOD) and solar activity changes. We allowed time lags of up to 11 months for each potential driver (66 months for solar activity). New hydrological insights for the region: The dynamic temporal-spatial evolution of the seasonal Pearson correlations was mapped out across the continent, tracking the gradual or abrupt expansion, displacement and subsequent waning of the various effects over the course of the year. Relationships are complicated by characteristic time lags, non-stationary correlations and occasional phase shifts. Our empirical results may help to further improve short- to midterm rainfall prognoses in Africa and provide important calibration data for the further improvement of climate models.