skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Eddy-Driven Buoyancy Gradients on Eastern Boundaries and Their Role in the Thermocline

Journal Article · · Journal of Physical Oceanography
 [1];  [1]
  1. Univ. of California, San Diego, CA (United States)

It is demonstrated that eddy fluxes of buoyancy at the eastern and western boundaries maintain alongshore buoyancy gradients along the coast. Eddy fluxes arise near the eastern and western boundaries because on both coasts buoyancy gradients normal to the boundary are strong. The eddy fluxes are accompanied by mean vertical flows that take place in narrow boundary layers next to the coast where the geostrophic constraint is broken. These ageostrophic cells have a velocity component normal to the coast that balances the geostrophic mean velocity. It is shown that the dynamics in these thin ageostrophic boundary layers can be replaced by effective boundary conditions for the interior flow, relating the eddy flux of buoyancy at the seaward edge of the boundary layers to the buoyancy gradient along the coast. These effective boundary conditions are applied to a model of the thermocline linearized around a mean stratification and a state of rest. The linear model parameterizes the eddy fluxes of buoyancy as isopycnal diffusion. Furthermore, the linear model produces horizontal gradients of buoyancy along the eastern coast on a vertical scale that depends on both the vertical diffusivity and the eddy diffusivity. The buoyancy field of the linear model agrees positively with the mean state of an eddy-resolving computation. Because the east–west difference in buoyancy is related to the zonally integrated meridional velocity, the linear model successfully predicts the meridional overturning circulation.

Research Organization:
Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF); Univ. of California, San Diego, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
FG02-01ER63252
OSTI ID:
1564671
Journal Information:
Journal of Physical Oceanography, Vol. 39, Issue 7; ISSN 0022-3670
Publisher:
American Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 21 works
Citation information provided by
Web of Science

References (22)

A unified linear theory of homogeneous and stratified rotating fluids journal September 1967
Buoyancy driven planetary flows journal May 1988
On the interaction of wind and buoyancy driven gyres journal August 1989
Isopycnal Mixing in Ocean Circulation Models journal January 1990
An explicit solution of the linear thermocline equations journal May 1985
Reconstructing the Meridional Overturning Circulation from Boundary Densities and the Zonal Wind Stress journal March 2007
Diffusivity and viscosity dependence in the linear thermocline journal November 2004
The Ventilated Thermocline journal February 1983
Equilibrium Structure and Dynamics of the California Current System journal April 2003
Boundary Mixing and the Dynamics of Three-Dimensional Thermohaline Circulations journal August 1997
Abyssal recipes II: energetics of tidal and wind mixing journal December 1998
Linear theory of the circulation of a stratified ocean journal January 1969
Eastern Boundary Ventilation and the Structure of the Thermocline journal November 1983
Geophysical Fluid Dynamics book January 1987
Boundary Intensification of Vertical Velocity in a β-Plane Basin journal December 2005
A simplified linear ocean circulation theory journal November 1986
The thermocline as an "internal boundary layer" journal August 1990
Large-scale circulation with small diapycnal diffusion: The two-thermocline limit journal March 1997
Global Characteristics of Ocean Variability Estimated from Regional TOPEX/POSEIDON Altimeter Measurements journal August 1997
Large-Scale Circulation and Production of Stratification: Effects of Wind, Geometry, and Diffusion journal May 2000
Overturning Circulation in an Eddy-Resolving Model: The Effect of the Pole-to-Pole Temperature Gradient journal January 2009
Eastern Boundary Conditions and Weak Solutions of the Ideal Thermocline Equations journal November 1986

Cited By (6)

Role of Surface-Layer Coherent Eddies in Potential Vorticity Transport in Quasigeostrophic Turbulence Driven by Eastward Shear journal December 2019
Transport by deep convection in basin-scale geostrophic circulation: turbulence-resolving simulations journal February 2019
Transport by deep convection in basin-scale geostrophic circulation: Turbulence-resolving simulations text January 2019
Dynamics of the Atlantic meridional overturning circulation. Part 2: Forcing by winds and buoyancy journal January 2014
Interannual to decadal variability within and across the major Eastern Boundary Upwelling Systems journal December 2019
Meridional overturning circulation: stability and ocean feedbacks in a box model text January 2012

Similar Records

Eastern-Boundary Contribution to the Residual and Meridional Overturning Circulations
Journal Article · Wed Sep 01 00:00:00 EDT 2010 · Journal of Physical Oceanography · OSTI ID:1564671

A reduced-gravity, primitive equation, isopycnal ocean GCM: Formulation and simulations
Journal Article · Fri Sep 01 00:00:00 EDT 1995 · Monthly Weather Review · OSTI ID:1564671

Circulation in the Peruvian Upwelling system near 15/sup 0/S
Journal Article · Sun Jul 20 00:00:00 EDT 1980 · J. Geophys. Res.; (United States) · OSTI ID:1564671