A recent Climatic Change paper suggests a relationship between climatic change in the 7th century BCE and the fall of the Assyrian Empire. However, available archaeological and textual evidence does not support the hypothesis that Assyria was overpopulated during this time and for that reason susceptible to outbreaks of drought. Besides long-term climatic variation, inter-annual variability in crops has always been very high in the dry farming areas of Upper Mesopotamia. To cope with this uncertainty, the local population developed several strategies (e.g. storage of agricultural surpluses in granaries and artificial irrigation in river valleys). Finally, slave prices, known to have declined during times of famine, were relatively stable during the entire century suggesting absence of prolonged periods of food shortage.In a recent volume of Climatic Change, Schneider and Adalı (2014) published a paper suggesting some sort of relationship between climatic change in the 7th century BCE and the fall of the Assyrian Empire. The authors hypothesize that prolonged drought decreased the volume of available crops and that the carrying capacity was exceeded in the core area of Assyria, which was overpopulated at this time. The authors use paleoclimatic proxies from distant parts of the Near East, most of which have relatively low temporal resolution, and one letter dated 15 May 657 BCE reporting on drought and the lack of harvests, as evidence for the deterioration of climatic conditions. Inferred overpopulation was deduced based on the size of Nineveh, which covered c. 750 ha during this time.The article by Schneider and Adalı (2014) is written in a very cautious manner, but the authors nonetheless seem convinced that both their model and their data are sufficient for identifying the proposed climatic change as the possible cause of the rapid collapse of the Assyrian state in the last quarter of the 7th century BCE. However, the amount of textual and Climatic Change (2016) 136:389-394