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Title: Response of a Strongly Eddying Global Ocean to North Atlantic Freshwater Perturbations

Abstract

The strongly eddying version of the Parallel Ocean Program (POP) is used in two 45-yr simulations to investigate the response of the Atlantic meridional overturning circulation (AMOC) to strongly enhanced freshwater input due to Greenland melting, with an integrated flux of 0.5 Sverdrups (Sv; 1 Sv ≡ 106 m3 s-1). For comparison, a similar set of experiments is performed using a noneddying version of POP. The aim is to identify the signature of the salt advection feedback in the two configurations. For this reason, surface salinity is not restored in these experiments. The freshwater input leads to a quantitatively comparable reduction of the overturning strength in the two models. To examine the importance of transient effects in the relation between AMOC strength and density distribution, the results of the eddy-resolving model are related to water mass transformation theory. The freshwater forcing leads to a reduction of the rate of light to dense water conversion in the North Atlantic, but there is no change in dense to light transformation elsewhere, implying that high density layers are continuously deflating. The main focus of the paper is on the effect of the AMOC reduction on the basinwide advection of freshwater. The low-resolution modelmore » results show a change of the net freshwater advection that is consistent with the salt advection feedback. However, for the eddy-resolving model, the net freshwater advection into the Atlantic basin appears to be unaffected, despite the significant change in the large-scale velocity structure.« less

Authors:
 [1];  [1];  [2];  [2];  [2];  [3]
  1. Univ. of Utrecht (Netherlands). Dept. of Physics and Astronomy, and Inst. for Marine and Atmospheric Research Utrecht
  2. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  3. Univ. of New South Wales, Sydney, NSW (Australia). Climate Change Research Centre, and ARC Centre of Excellence for Climate System Science
Publication Date:
Research Org.:
Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF); Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1565242
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Physical Oceanography
Additional Journal Information:
Journal Volume: 44; Journal Issue: 2; Journal ID: ISSN 0022-3670
Publisher:
American Meteorological Society
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Oceanography

Citation Formats

Toom, Matthijs den, Dijkstra, Henk A., Weijer, Wilbert, Hecht, Matthew W., Maltrud, Mathew E., and van Sebille, Erik. Response of a Strongly Eddying Global Ocean to North Atlantic Freshwater Perturbations. United States: N. p., 2014. Web. doi:10.1175/jpo-d-12-0155.1.
Toom, Matthijs den, Dijkstra, Henk A., Weijer, Wilbert, Hecht, Matthew W., Maltrud, Mathew E., & van Sebille, Erik. Response of a Strongly Eddying Global Ocean to North Atlantic Freshwater Perturbations. United States. https://doi.org/10.1175/jpo-d-12-0155.1
Toom, Matthijs den, Dijkstra, Henk A., Weijer, Wilbert, Hecht, Matthew W., Maltrud, Mathew E., and van Sebille, Erik. Wed . "Response of a Strongly Eddying Global Ocean to North Atlantic Freshwater Perturbations". United States. https://doi.org/10.1175/jpo-d-12-0155.1. https://www.osti.gov/servlets/purl/1565242.
@article{osti_1565242,
title = {Response of a Strongly Eddying Global Ocean to North Atlantic Freshwater Perturbations},
author = {Toom, Matthijs den and Dijkstra, Henk A. and Weijer, Wilbert and Hecht, Matthew W. and Maltrud, Mathew E. and van Sebille, Erik},
abstractNote = {The strongly eddying version of the Parallel Ocean Program (POP) is used in two 45-yr simulations to investigate the response of the Atlantic meridional overturning circulation (AMOC) to strongly enhanced freshwater input due to Greenland melting, with an integrated flux of 0.5 Sverdrups (Sv; 1 Sv ≡ 106 m3 s-1). For comparison, a similar set of experiments is performed using a noneddying version of POP. The aim is to identify the signature of the salt advection feedback in the two configurations. For this reason, surface salinity is not restored in these experiments. The freshwater input leads to a quantitatively comparable reduction of the overturning strength in the two models. To examine the importance of transient effects in the relation between AMOC strength and density distribution, the results of the eddy-resolving model are related to water mass transformation theory. The freshwater forcing leads to a reduction of the rate of light to dense water conversion in the North Atlantic, but there is no change in dense to light transformation elsewhere, implying that high density layers are continuously deflating. The main focus of the paper is on the effect of the AMOC reduction on the basinwide advection of freshwater. The low-resolution model results show a change of the net freshwater advection that is consistent with the salt advection feedback. However, for the eddy-resolving model, the net freshwater advection into the Atlantic basin appears to be unaffected, despite the significant change in the large-scale velocity structure.},
doi = {10.1175/jpo-d-12-0155.1},
journal = {Journal of Physical Oceanography},
number = 2,
volume = 44,
place = {United States},
year = {Wed Feb 12 00:00:00 EST 2014},
month = {Wed Feb 12 00:00:00 EST 2014}
}

Journal Article:
Free Publicly Available Full Text
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Cited by: 25 works
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Figures / Tables:

FIG. 1 FIG. 1: Annual-mean fields of the seasonally varying virtual salt flux for the $R$0.1 configuration, converted to units of mm day -1 with positive values indicating evaporation. (a) Reference flux consisting of climatological evaporation, precipitation, and runoff, plus the diagnosed flux implied by the restoring condition in the spinup integration.more » Apart from minor changes due to evaporation depending on SST, this flux is constant throughout the years and the same in both simulations studied. This plot shows the field for year 76 in REF. (b) Runoff from Greenland as applied in PERT.« less

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