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Ref ID: 28646
Ref Type: Journal Article
Authors: Buckley, Brendan M.
Anchukaitis, Kevin J.
Penny, Daniel
Fletcher, Roland
Cook, Edward R.
Sano, Masaki
Nam, Le Canh
Wichienkeeo, Aroonrut
Minh, Ton That
Hong, Truong Mai
Title: Climate as a contributing factor in the demise of Angkor, Cambodia
Date: 2010
Source: PNAS
DOI: 10.1073/pnas.0910827107
Abstract: The “hydraulic city” of Angkor, the capitol of the Khmer Empire in Cambodia, experienced decades-long drought interspersed with intense monsoons in the fourteenth and fifteenth centuries that, in combination with other factors, contributed to its eventual demise. The climatic evidence comes from a seven-and-a-half century robust hydroclimate reconstruction from tropical southern Vietnamese tree rings. The Angkor droughts were of a duration and severity that would have impacted the sprawling city’s water supply and agricultural productivity, while high-magnitude monsoon years damaged its water control infrastructure. Hydroclimate variability for this region is strongly and inversely correlated with tropical Pacific sea surface temperature, indicating that a warm Pacific and El Niño events induce drought at interannual and interdecadal time scales, and that low-frequency variations of tropical Pacific climate can exert significant influence over Southeast Asian climate and society.
Date Created: 9/27/2011
Volume: 107
Number: 15
Page Start: 6748
Page End: 6752