Isoneutral Diffusion in a z-Coordinate Ocean ModelSource: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 005::page 805Author:Griffies, Stephen M.
,
Gnanadesikan, Anand
,
Pacanowski, Ronald C.
,
Larichev, Vitaly D.
,
Dukowicz, John K.
,
Smith, Richard D.
DOI: 10.1175/1520-0485(1998)028<0805:IDIAZC>2.0.CO;2Publisher: American Meteorological Society
Abstract: This paper considers the requirements that must be satisfied in order to provide a stable and physically based isoneutral tracer diffusion scheme in a z-coordinate ocean model. Two properties are emphasized: 1) downgradient orientation of the diffusive fluxes along the neutral directions and 2) zero isoneutral diffusive flux of locally referenced potential density. It is shown that the Cox diffusion scheme does not respect either of these properties, which provides an explanation for the necessity to add a nontrivial background horizontal diffusion to that scheme. A new isoneutral diffusion scheme is proposed that aims to satisfy the stated properties and is found to require no horizontal background diffusion.
|
Collections
Show full item record
contributor author | Griffies, Stephen M. | |
contributor author | Gnanadesikan, Anand | |
contributor author | Pacanowski, Ronald C. | |
contributor author | Larichev, Vitaly D. | |
contributor author | Dukowicz, John K. | |
contributor author | Smith, Richard D. | |
date accessioned | 2017-06-09T14:52:59Z | |
date available | 2017-06-09T14:52:59Z | |
date copyright | 1998/05/01 | |
date issued | 1998 | |
identifier issn | 0022-3670 | |
identifier other | ams-28861.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4166024 | |
description abstract | This paper considers the requirements that must be satisfied in order to provide a stable and physically based isoneutral tracer diffusion scheme in a z-coordinate ocean model. Two properties are emphasized: 1) downgradient orientation of the diffusive fluxes along the neutral directions and 2) zero isoneutral diffusive flux of locally referenced potential density. It is shown that the Cox diffusion scheme does not respect either of these properties, which provides an explanation for the necessity to add a nontrivial background horizontal diffusion to that scheme. A new isoneutral diffusion scheme is proposed that aims to satisfy the stated properties and is found to require no horizontal background diffusion. | |
publisher | American Meteorological Society | |
title | Isoneutral Diffusion in a z-Coordinate Ocean Model | |
type | Journal Paper | |
journal volume | 28 | |
journal issue | 5 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1998)028<0805:IDIAZC>2.0.CO;2 | |
journal fristpage | 805 | |
journal lastpage | 830 | |
tree | Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 005 | |
contenttype | Fulltext |