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contributor authorPolzin, Kurt
contributor authorFerrari, Raffaele
date accessioned2017-06-09T14:56:12Z
date available2017-06-09T14:56:12Z
date copyright2004/01/01
date issued2004
identifier issn0022-3670
identifier otherams-30006.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167298
description abstractFinescale velocity and density fluctuations consist of both internal waves and vorticity-containing perturbations (vortical modes). A recent decomposition of observations obtained as part of the North Atlantic Tracer Release Experiment (NATRE) permits one to investigate isopycnal stirring associated with vortical modes. This stirring is treated here as a relative dispersion problem in the context of 2D turbulence. Isopycnal diffusivities attain values on the order of 1 m2 s?1 after an initial transient of 5?10 days. After 2 weeks, a patch of tracer with initial radius of 25 m is predicted to have evolved into a convoluted web having an rms radius of 2?4 km. These estimates agree with observations of the evolution of an anthropogenic tracer in NATRE.
publisherAmerican Meteorological Society
titleIsopycnal Dispersion in NATRE
typeJournal Paper
journal volume34
journal issue1
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(2004)034<0247:IDIN>2.0.CO;2
journal fristpage247
journal lastpage257
treeJournal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 001
contenttypeFulltext


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