Abstract
Records of Nile flood discharge from AD 930 to 1450 reveal pronounced variability in the frequency of extreme floods due to differential influence of global climatic forcing mechanisms on the two main catchment areas of the Nile tributaries, namely Equatorial Africa and the Ethiopian Highlands.
Cite
CITATION STYLE
APA
Hassan, F. A. (2011). Nile flood discharge during the Medieval Climate Anomaly. PAGES News, 19(1), 30–31. https://doi.org/10.22498/pages.19.1.30
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