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Title: Meltwater routing and the Younger Dryas

Journal Article · · Proceedings of the National Academy of Sciences of the United States of America
 [1];  [2]
  1. Univ. of Massachusetts, Amherst, MA (United States). Dept. of Geosciences, Climate System Research Center
  2. Univ. of Alaska, Fairbanks, AK (United States). Inst. of Marine Science, School of Fisheries and Ocean Sciences

The Younger Dryas -- the last major cold episode on Earth -- is generally considered to have been triggered by a meltwater flood into the North Atlantic. The prevailing hypothesis, proposed by Broecker et al. [1989 Nature 341:318–321] more than two decades ago, suggests that an abrupt rerouting of Lake Agassiz overflow through the Great Lakes and St. Lawrence Valley inhibited deep water formation in the subpolar North Atlantic and weakened the strength of the Atlantic Meridional Overturning Circulation (AMOC).More recently, Tarasov and Peltier [2005 Nature 435:662–665] showed that meltwater could have discharged into the Arctic Ocean via the Mackenzie Valley ~4,000 km northwest of the St. Lawrence outlet. Here we use a sophisticated, high-resolution, ocean sea-ice model to study the delivery of meltwater from the two drainage outlets to the deep water formation regions in the North Atlantic. Unlike the hypothesis of Broecker et al., freshwater from the St. Lawrence Valley advects into the subtropical gyre ~3,000 km south of the North Atlantic deep water formation regions and weakens the AMOC by <15%. In contrast, narrow coastal boundary currents efficiently deliver meltwater from the Mackenzie Valley to the deep water formation regions of the subpolar North Atlantic and weaken the AMOC by >30%. We conclude that meltwater discharge from the Arctic, rather than the St. Lawrence Valley, was more likely to have triggered the Younger Dryas cooling.

Research Organization:
Univ. of Alaska, Fairbanks, AK (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
FG02-09ER64725
OSTI ID:
1105906
Journal Information:
Proceedings of the National Academy of Sciences of the United States of America, Vol. 109, Issue 49; ISSN 0027-8424
Publisher:
National Academy of Sciences, Washington, DC (United States)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 109 works
Citation information provided by
Web of Science

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Cited By (18)

Optically stimulated luminescence ages from the Lake Agassiz basin in Manitoba journal March 2018
Subtropical iceberg scours and meltwater routing in the deglacial western North Atlantic journal October 2014
Early Holocene sea level in the Canadian Beaufort Sea constrained by radiocarbon dates from a deep borehole in the Mackenzie Trough, Arctic Canada journal July 2018
North Atlantic forcing of tropical Indian Ocean climate journal April 2014
Water mass evolution of the Greenland Sea since late glacial times journal January 2014
Inferring surface water equilibrium calcite δ 18 O during the last deglacial period from benthic foraminiferal records: Implications for ocean circulation journal November 2015
A multi-proxy study of changing environmental conditions in a Younger Dryas sequence in southwestern Manitoba, Canada, and evidence for an extraterrestrial event journal October 2019
LakeCC: a tool for efficiently identifying lake basins with application to palaeogeographic reconstructions of North America journal April 2020
Origin and provenance of spherules and magnetic grains at the Younger Dryas boundary journal September 2013
Sediment Provenance Changes in the Western Arctic Ocean in Response to Ice Rafting, Sea Level, and Oceanic Circulation Variations Since the Last Deglaciation journal July 2018
Acceleration of Northern Ice Sheet Melt Induces AMOC Slowdown and Northern Cooling in Simulations of the Early Last Deglaciation journal July 2018
Reconstruction of North American drainage basins and river discharge since the Last Glacial Maximum journal January 2016
Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling journal July 2018
LakeCC: a tool for efficiently identifying lake basins with application to palaeogeographic reconstructions of North America text January 2019
Climate response to the meltwater runoff from Greenland ice sheet: evolving sensitivity to discharging locations journal November 2017
Transient climate simulations of the deglaciation 21–9 thousand years before present (version 1) – PMIP4 Core experiment design and boundary conditions journal January 2016
Offset timing of climate oscillations during the last two glacial‐interglacial transitions connected with large‐scale freshwater perturbation journal June 2015
Collapse of a marine-based ice stream during the early Younger Dryas chronozone, western Canadian Arctic journal January 2018

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