[1] Zhou et al. (Science, May 2024)
Heinrich event ice discharge and the fate of the Atlantic Meridional Overturning Circulation
https://www.science.org/doi/10.1126/science.adh8369
Editor’s summary
Will ice mass loss from the Greenland Ice Sheet caused by climate warming disrupt large-scale ocean circulation? Zhou et al. reconstructed iceberg production rates during the massive calving episodes of the last glacial period, called Heinrich events, when icebergs did affect ocean circulation. The authors found that present-day Greenland Ice Sheet calving rates are as high as during some of those events. However, because melting is causing the Greenland Ice Sheet to recede from the coasts of Greenland, where icebergs originate, its iceberg discharge should not persist long enough to cause major disruption of the Atlantic overturning circulation by itself. —Jesse Smith
Abstract
During Heinrich events, great armadas of icebergs episodically flooded the North Atlantic Ocean and weakened overturning circulation. The ice discharges of these episodes constrain the sensitivity of overturning circulation to iceberg melting. We reconstructed these ice discharges to be as high as 0.13 Sverdrup (Sv) (1 Sv = 1 million cubic meters per second) during Heinrich event 4 and to average 0.029 Sv over all episodes. The present-day Greenland Ice Sheet calving of icebergs is comparable to that of a mid-range Heinrich event. As the future Greenland Ice Sheet recedes from marine-terminating outlets, its iceberg calving likely will not persist long enough for icebergs alone to cause catastrophic disruption to the Atlantic overturning circulation, although the accelerating Greenland runoff and continued global warming remain threats to the circulation stability.