Cover Journal of Physical Oceanography
Journal of Physical Oceanography

 

Volume 30 (2000): Issue 11 (Nov 2000)

Print ISSN:
0022-3670
Online ISSN:
1520-0485
Cover Journal of Physical Oceanography
ARTICLES
On the Propagation of Baroclinic Waves in the General Circulation
Does the Wind Control the Import and Export of the South Atlantic?
Bottom Boundary Layer Structure and Detachment in the Shelfbreak Jet of the Middle Atlantic Bight
Diagnosis of the Three-Dimensional Circulation in Mesoscale Features with Large Rossby Number
Marginal Thermobaric Stability in the Ice-Covered Upper Ocean over Maud Rise
Spectral Energy Balance of Breaking Waves within the Surf Zone
The Effects of Subgrid-Scale Parameterizations in a Zonally Averaged Ocean Model
Airborne Measurements of the Wavenumber Spectra of Ocean Surface Waves. Part I: Spectral Slope and Dimensionless Spectral Coefficient
Airborne Measurements of the Wavenumber Spectra of Ocean Surface Waves. Part II: Directional Distribution
Branching Mechanism of the Tsushima Current in the Korea Strait
Interdecadal Thermocline Variability in the North Pacific for 1958–97: A GCM Simulation
Equations of Motion Using Thermodynamic Coordinates
Orthobaric Density: A Thermodynamic Variable for Ocean Circulation Studies
Deep Pacific Circulation Controlled by Vertical Diffusivity at the Lower Thermocline Depths
Slope-Enhanced Fission of Salty Hetons under Sea Ice
Response of the Equatorial Thermocline to Extratropical Buoyancy Forcing
Internal Solitary Waves in the Warm Pool of the Western Equatorial Pacific
A Numerical Study of the Adjustment of a Narrow Stratified Current over a Sloping Bottom
Boundary Layer Control of Buoyant Coastal Currents and the Establishment of a Shelfbreak Front
Modeling the East Australian Current in the Western Tasman Sea
Coupled Rossby Waves in the Indian Ocean on Interannual Timescales
The Surface-Layer Heat Balance in the Equatorial Pacific Ocean. Part II: Interannual Variability
Climate Variability Induced by Anomalous Buoyancy Forcing in a Multilayer Model of the Ventilated Thermocline
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