Analyses of historical patterns of rainfall variability are essential for understanding long-term changes in precipitation timing and distribution. Focussing on former Natal and Zululand (now KwaZulu-Natal, South Africa), this study presents the first combined annual and seasonal reconstruction of rainfall variability over southeast Africa for the 19th century. Analyses of documentary sources, including newspapers and colonial and missionary materials, indicate that the region was affected by severe or multi-year drought on eight occasions between 1836 and 1900 (the rainy seasons of 1836-38, 1861-63, 1865-66, 1868-70, 1876-79, 1883-85, 1886-90 and 1895-1900). Six severe or multi-year wet periods are also identified (1847-49, 1854-57, 1863-65, 1879-81, 1890-91 and 1892-94). The timing of these events agrees well with independent reconstructions of 19th century rainfall for other parts of the southern African summer rainfall zone (SRZ), suggesting subcontinental scale variability. Our results indicate that the relationship between El Niño and rainfall in southeast Africa was relatively stable, at least for the latter half of the 19th century. El Niño conditions appear to have had a more consistent modulating effect upon rainfall during the 19th century than La Niña. The rainfall chronology from this study is combined with other annually-resolved palaeoclimate records from mainland southern Africa and surrounding oceans as part of a multi-proxy rainfall reconstruction for the SRZ. This reconstruction confirms (i) the long-term importance of ENSO and Indian Ocean SSTs for modulating regional rainfall; and (ii) that summer precipitation has been declining progressively over the last 200 years

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Annual rainfall reconstruction for northern (region 1), central (region 2), and southern (region 3) Malawi derived from historical documentary sources. CR indicates confidence rating from highest (3) to lowest (1); a value of 0 indicates insufficient evidence to generate a classification. Inset shows average rainfall for Blantyre and Zomba Agricultural College downloaded from the GHCN database; note that data are not available for these stations for 1893–1895. El Niño years are also indicated.

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Tropical cyclones (TCs) represent the most significant natural hazard for the economy and population of Madagascar. Planning for the impacts of future cyclone strikes requires a detailed understanding of the frequency of destructive storms in the past. In this paper, we utilise historical documentary materials to construct an initial framework of TCs making landfall on Madagascar during the latter half of the 19th century. The study focuses on 1862–1900 as this is the period of most extensive documentary records. Accounts of storm damage contained within historical sources are used to reconstruct TC tracks over land, with details of wind damage converted into Fujita (F) Scale classes to classify TC intensity. A total of 20 TCs are identified, of which only 17 are included within the IBTrACS dataset for the southwest Indian Ocean. The TCs of 13–14 March 1872 and 28 January–1 February 1893 were the most destructive of the late 19th century, with F3+ levels of wind damage identified from historical accounts. We compare our results with data for TCs within the IBTrACS dataset that made landfall on Madagascar during the period 1970–2012. This comparison suggests that (1) fewer TCs made landfall during the 19th century compared with the post-satellite era, but that of these (2) a greater proportion appear to have crossed the northeast of the island. There is no significant correlation between numbers of landfalling TCs and either mean annual SOI or DMI. We conclude with a consideration of additional archival collections that may be used in future investigations to enhance our chronology