Acceleration of northern ice sheet melt induces AMOC slowdown and northern cooling in simulations of the early last deglaciation

• Published in: Paleoceanography and Paleoclimatology
• Main Authors: Ivanovic, Ruza, Gregoire, Lauren, Burke, Andrea, Wickert, A. D., Valdes, P. J., Ng, H. C., Robinson, L. F., McManus, J. F., Mitrovica, J. X., Lee, L., Dentith, J. E.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2018
• Subjects: Heinrich Stadial 1; Meltwater; AMOC; Freshwater forcing; Deglaciation; Stadial; Greenland; Ice Sheet
• Online Access: https://risweb.st-andrews.ac.uk/portal/en/researchoutput/acceleration-of-northern-ice-sheet-melt-induces-amoc-slowdown-and-northern-cooling-in-simulations-of-the-early-last-deglaciation(8efb5fd5-4218-40c6-a809-8febbabb0bb1).html; https://doi.org/10.1029/2017PA003308; https://research-repository.st-andrews.ac.uk/bitstream/10023/15798/1/Ivanovic_2018_PP_Northernicesheetmelt_CC.pdf

The cause of a rapid change in Atlantic Ocean circulation and northern cooling at the onset of Heinrich Stadial 1 ~18.5 ka is unclear. Previous studies have simulated the event using ice sheet and/or iceberg meltwater forcing, but these idealized freshwater fluxes have been unrealistically large. Here, we use a different approach, driving a high‐resolution drainage network model with a recent time‐resolved global paleo ice sheet reconstruction to generate a realistic meltwater forcing. We input this flux to the HadCM3 climate model without adjusting the timing or amplitude and find that an acceleration in northern ice sheet melting (up to ~7.5 m kyr ‐1 global mean sea level rise equivalent) triggers a 20% reduction in the Atlantic Meridional Overturning Circulation. The simulated pattern of ocean circulation and climate change matches an array of palaeoclimate and ocean circulation reconstructions for the onset of Heinrich Stadial 1, both in terms of rates and magnitude of change. This is achieved with a meltwater flux that matches constraints on sea level changes and ice sheet evolution around 19‐18 ka. Since the rates of melting are similar to those projected for Greenland by 2200, constraining the melt rates and magnitude of climate change during Heinrich Stadial 1 would provide an important test of climate model sensitivity to future ice sheet melt.