Abstract
The climate during the Caucasian Bronze Age was similar to that of today: basically continental with warm to hot summers and cold winters and varying with altitude, with pronounced diurnal variations particularly during summer months at the higher elevations. There is a general decrease in precipitation from west to east with the greatest rainfall in the subtropical Colchidean depression of western Georgia. Given shifts in settlement location and the abandonment of drier areas, such as the Mil-Karabagh steppes, at the beginning of the Caucasian Bronze Age, some researchers have postulated increased aridization; similarly, others have postulated another such shift at the end of the Early Bronze Age as reflected in the abandonment of numerous Kura-Araxes culture sites. Both theories need more primary empirical substantiation.
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Kohl, P. (2001). Caucasian Bronze Age. In: Peregrine, P.N., Ember, M. (eds) Encyclopedia of Prehistory. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1187-8_4
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DOI: https://doi.org/10.1007/978-1-4615-1187-8_4
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