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Model Sensitivity to North Atlantic Freshwater Forcing at 8.2 Ka : Volume 9, Issue 2 (10/04/2013)

By Morrill, C.

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Book Id: WPLBN0004006634
Format Type: PDF Article :
File Size: Pages 14
Reproduction Date: 2015

Title: Model Sensitivity to North Atlantic Freshwater Forcing at 8.2 Ka : Volume 9, Issue 2 (10/04/2013)  
Author: Morrill, C.
Volume: Vol. 9, Issue 2
Language: English
Subject: Science, Climate, Past
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2013
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

Citation

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Bakker, P., Otto-Bliesner, B. L., Renssen, H., Morrill, C., & Legrande, A. N. (2013). Model Sensitivity to North Atlantic Freshwater Forcing at 8.2 Ka : Volume 9, Issue 2 (10/04/2013). Retrieved from http://www.ebooklibrary.org/


Description
Description: Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA. We compared four simulations of the 8.2 ka event to assess climate model sensitivity and skill in responding to North Atlantic freshwater perturbations. All of the simulations used the same freshwater forcing, 2.5 Sv for one year, applied to either the Hudson Bay (northeastern Canada) or Labrador Sea (between Canada's Labrador coast and Greenland). This freshwater pulse induced a decadal-mean slowdown of 10–25% in the Atlantic Meridional Overturning Circulation (AMOC) of the models and caused a large-scale pattern of climate anomalies that matched proxy evidence for cooling in the Northern Hemisphere and a southward shift of the Intertropical Convergence Zone. The multi-model ensemble generated temperature anomalies that were just half as large as those from quantitative proxy reconstructions, however. Also, the duration of AMOC and climate anomalies in three of the simulations was only several decades, significantly shorter than the duration of ~150 yr in the paleoclimate record. Possible reasons for these discrepancies include incorrect representation of the early Holocene climate and ocean state in the North Atlantic and uncertainties in the freshwater forcing estimates.

Summary
Model sensitivity to North Atlantic freshwater forcing at 8.2 ka

Excerpt
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