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A Theory of the Wind-Driven Beaufort Gyre Variability

Manucharyan, Georgy E. and Spall, Michael A. and Thompson, Andrew F. (2016) A Theory of the Wind-Driven Beaufort Gyre Variability. Journal of Physical Oceanography, 46 (11). pp. 3263-3278. ISSN 0022-3670. http://resolver.caltech.edu/CaltechAUTHORS:20161222-091517006

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Abstract

The halocline of the Beaufort Gyre varies significantly on interannual to decadal time scales, affecting the freshwater content (FWC) of the Arctic Ocean. This study explores the role of eddies in the Ekman-driven gyre variability. Following the transformed Eulerian-mean paradigm, the authors develop a theory that links the FWC variability to the stability of the large-scale gyre, defined as the inverse of its equilibration time. The theory, verified with eddy-resolving numerical simulations, demonstrates that the gyre stability is explicitly controlled by the mesoscale eddy diffusivity. An accurate representation of the halocline dynamics requires the eddy diffusivity of 300 ± 200 m^2 s^(−1), which is lower than what is used in most low-resolution climate models. In particular, on interannual and longer time scales the eddy fluxes and the Ekman pumping provide equally important contributions to the FWC variability. However, only large-scale Ekman pumping patterns can significantly alter the FWC, with spatially localized perturbations being an order of magnitude less efficient. Lastly, the authors introduce a novel FWC tendency diagnostic—the Gyre Index—that can be conveniently calculated using observations located only along the gyre boundaries. Its strong predictive capabilities, assessed in the eddy-resolving model forced by stochastic winds, suggest that the Gyre Index would be of use in interpreting FWC evolution in observations as well as in numerical models.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1175/JPO-D-16-0091.1DOIArticle
http://journals.ametsoc.org/doi/10.1175/JPO-D-16-0091.1PublisherArticle
Additional Information:© 2016 American Meteorological Society. Manuscript received 11 April 2016, in final form 22 July 2016, Published online 20 October 2016. The authors acknowledge the high-performance computing support from Yellowstone provided by NCAR’s CIS Laboratory, sponsored by the NSF. GEM acknowledges the support from the Howland Postdoctoral Program Fund at WHOI and the Stanback Fellowship Fund at Caltech. MAS was supported by NSF Grants PLR-1415489 and OCE-1232389. AFT acknowledges support from NASA Award NNN12AA01C. The authors thank Prof. John Marshall and an anonymous reviewer for helpful comments and suggestions. The manuscript also benefited from discussions at the annual Forum for Arctic Modeling and Observing Synthesis (FAMOS) funded by the NSF OPP Awards PLR-1313614 and PLR-1203720.
Funders:
Funding AgencyGrant Number
Woods Hole Oceanographic InstitutionUNSPECIFIED
Coco and Foster Stanback Postdoctoral Fellowship in Global Environmental ScienceUNSPECIFIED
NSFPLR-1415489
NSFOCE-1232389
NASANNN12AA01C
NSFPLR-1313614
NSFPLR-1203720
Subject Keywords:Arctic; Eddies; Ekman pumping/transport; Large-scale motions; Ocean circulation; Stability
Record Number:CaltechAUTHORS:20161222-091517006
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20161222-091517006
Official Citation:Manucharyan, G., M. Spall, and A. Thompson, 2016: A Theory of the Wind-Driven Beaufort Gyre Variability. J. Phys. Oceanogr., 46, 3263–3278, doi: 10.1175/JPO-D-16-0091.1.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:73130
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:22 Dec 2016 17:23
Last Modified:22 Dec 2016 17:23

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