RefDoc
Haut

Faire une nouvelle recherche
Make a new search
Lancer la recherche


Titre du document / Document title

Comparisons of localized convection due to localized forcing and to preconditioning

Auteur(s) / Author(s)

STRANEO F. (1) ; KAWASE M. (1) ;

Affiliation(s) du ou des auteurs / Author(s) Affiliation(s)

(1) School of Oceanography, University of Washington, Seattle. Washington, ETATS-UNIS

Résumé / Abstract

Although observations indicate that localization of deep convection results from oceanic preconditioning and only to a lesser extent from the gradients in the atmospheric forcing, most laboratory and numencal simulations of oceanic deep convection localize convection via the buoyancy forcing. It is as yet unclear to what extent the localized forcing simplification is representative of realistic preconditioned convection and whether conclusions drawn from analyzing the former scenario can be applied to the latter. Comparison between these two localized convection scenarios is the focus of this study. The analysis is conducted using a high-resolution, nonhydrostatic numerical model that assumes no variations in the latitudinal direction. Although this model cannot represent baroclinic instability, it represents well the violent mixing phase of chimney formation that precedes baroclinic instability., Because of the inherently different initial and boundary conditions, there is no single comparison to be made between the two scenarios; all of the comparisons, however, show that a localized forcing tends to enhance the frontal structures at the edge of the convected water mass. The authors explain these results by means of some simple analytical calculations that indicate that convection as a result of a localized forcing induces a continuous increase in the horizontal density gradient, while convection in a surface-intensitied. cyclonic gyre results in a decrease in the horizontal gradient The authors conclude that the two scenarios are not equivalent and discuss how some of the conclusions, valid for localized forcing, do not necessarily apply to the preconditioned scenario. In particular, the equilibrium state observed in localized forcing simulations, in which the lateral fluxes due to the baroclinic eddies balance the surface buoyancy loss, may not have an analog for the case of preconditioned convection.

Revue / Journal Title

Journal of physical oceanography    ISSN  0022-3670   CODEN JPYOBT 

Source / Source

1999, vol. 29, no1, pp. 55-68 (20 ref.)

Langue / Language

Anglais

Editeur / Publisher

American Meteorological Society, Boston, MA, ETATS-UNIS  (1971) (Revue)

Mots-clés anglais / English Keywords

Ocean convection

;

Forcing

;

Ocean atmosphere interaction

;

Sea surface

;

Deep water

;

Numerical method

;

Baroclinic instability

;

Water mass

;

Vorticity

;

Mixed layer

;

Mots-clés français / French Keywords

Convection océanique

;

Forçage

;

Interaction atmosphère océan

;

Surface marine

;

Eau profonde

;

Méthode numérique

;

Instabilité barocline

;

Masse eau

;

Vorticité

;

Couche mélangée

;

Mots-clés espagnols / Spanish Keywords

Convección oceánica

;

Forzamiento

;

Interacción atmósfera océano

;

Superficie marina

;

Agua profunda

;

Método numérico

;

Inestabilidad baroclínica

;

Masa agua

;

Vorticidad

;

Capa mezclada

;

Localisation / Location

INIST-CNRS, Cote INIST : 15148, 35400007214183.0040

Nº notice refdoc (ud4) : 1654979



Faire une nouvelle recherche
Make a new search
Lancer la recherche
Bas