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contributor authorWright, Corwin J.
contributor authorScott, Robert B.
contributor authorFurnival, Darran
contributor authorAilliot, Pierre
contributor authorVermet, Franck
date accessioned2017-06-09T17:19:56Z
date available2017-06-09T17:19:56Z
date copyright2013/02/01
date issued2012
identifier issn0022-3670
identifier otherams-83327.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226540
description abstractuadratic bottom boundary layer drag is a potentially significant source of energy dissipation in the deep ocean. This study presents a new estimate of the energy dissipated by this process, using results from the world?s largest archive of ocean current meter time series and focusing strongly upon the potential uncertainties in this calculation. Two methods are used, one based on a simple division of the World Ocean into a series of regular grids and the other based on a more sophisticated analysis using a hierarchical clustering mechanism assisted by estimates from the Hybrid Coordinate Ocean Model (HYCOM) model. From these analyses, the authors estimate a globally integrated bottom boundary layer dissipation of 0.65 ± 0.15 (statistical uncertainty) ± 0.15 (methodological uncertainty) TW.
publisherAmerican Meteorological Society
titleGlobal Observations of Ocean-Bottom Subinertial Current Dissipation
typeJournal Paper
journal volume43
journal issue2
journal titleJournal of Physical Oceanography
identifier doi10.1175/JPO-D-12-082.1
journal fristpage402
journal lastpage417
treeJournal of Physical Oceanography:;2012:;Volume( 043 ):;issue: 002
contenttypeFulltext


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