On the eddy transfer of tracers: Advective or diffusive?

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ID: 294680
1997
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Abstract
Geostrophic eddies have traditionally been viewed within oceanography as diffusing water masses and tracers in a down-gradient manner. However, eddies also have an advective role that may lead to an up-gradient transfer of tracers, as has been recognized in atmospheric tracer studies and recent eddy parameterizations developed for the ocean. Eddies provide an advective transfer or “bolus” velocity through the secondary circulation formed by the slumping of density surfaces in baroclinic instability. Here we use an eddy-resolving isopycnal ocean model to investigate the meridional transfer across a zonal jet. The jet undergoes baroclinic instability, forming a vibrant eddy field and inducing a meridional bolus velocity. The bolus velocity is found to be correlated with gradients of potential
Reference Key
openalex_W2163299562 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Mei-Man Lee, David P. Marshall, Richard G. Williams
Journal journal of marine research
Year 1997
DOI
10.1357/0022240973224346
URL
Keywords Keywords not found

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