Partitioning of Kinetic Energy in the Arctic Ocean's Beaufort Gyre

Kinetic energy (KE) in the Arctic Ocean's Beaufort Gyre is dominated by the mesoscale eddy field that plays a central role in the transport of freshwater, heat, and biogeochemical tracers. Understanding Beaufort Gyre KE variability sheds light on how this freshwater reservoir responds to wind f...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Zhao, Mengnan, Timmermans, Mary-Louise, Krishfield, Richard, Manucharyan, Georgy
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2018
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Online Access:https://doi.org/10.1029/2018JC014037
Description
Summary:Kinetic energy (KE) in the Arctic Ocean's Beaufort Gyre is dominated by the mesoscale eddy field that plays a central role in the transport of freshwater, heat, and biogeochemical tracers. Understanding Beaufort Gyre KE variability sheds light on how this freshwater reservoir responds to wind forcing and sea ice and ocean changes. The evolution and fate of mesoscale eddies relate to energy pathways in the ocean (e.g., the exchange of energy between barotropic and baroclinic modes). Mooring measurements of horizontal velocities in the Beaufort Gyre are analyzed to partition KE into barotropic and baroclinic modes and explore their evolution. We find that a significant fraction of water column KE is in the barotropic and the first two baroclinic modes. We explain this energy partitioning by quantifying the energy transfer coefficients between the vertical modes using the quasiâ€geostrophic potential vorticity conservation equations with a specific background stratification observed in the Beaufort Gyre. We find that the quasiâ€geostrophic vertical mode interactions uphold the persistence of KE in the first two baroclinic modes, consistent with observations. Our results explain the specific role of halocline structure on KE evolution in the gyre and suggest depressed transfer to the barotropic mode. This limits the capacity for frictional dissipation at the sea floor and suggests that energy dissipation via sea iceâ€ocean drag may be prominent. © 2018 American Geophysical Union. Received 2 APR 2018; Accepted 31 MAY 2018; Accepted article online 20 JUN 2018; Published online 10 JUL 2018. This article also appears in: Forum for Arctic Modeling and Observational Synthesis (FAMOS) 2: Beaufort Gyre phenomenon. Mooring data were collected and made available by the Beaufort Gyre Exploration Program based at the Woods Hole Oceanographic Institution (http://www.whoi.edu/beaufortgyre) in collaboration with researchers from Fisheries and Oceans Canada at the Institute of Ocean Sciences. Funding was provided by the National ...