Role of the Bering Strait on the hysteresis of the ocean conveyor belt circulation and glacial climate stability
Aixue Hua,1, Gerald A. Meehla, Weiqing Hanb, Axel Timmermannc, Bette Otto-Bliesnera, Zhengyu Liud, Warren M. Washingtona, William Largea, Ayako Abe-Ouchie, Masahide Kimotoe, Kurt Lambeckf, and Bingyi Wug
Edited by Isaac M. Held, Geophysical Fluid Dynamics Laboratory/NOAA, Princeton, NJ, and approved March 8, 2012 (received for review September 28, 2011)
AbstractAuthors & InfoSIMetricsPDFPDF + SI
Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open.
abrupt climate transitions Atlantic Meridional Overturning Circulation