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JOURNALS
Artificial Intelligence for the Earth Systems
Bulletin of the American Meteorological Society
Community Science
Earth Interactions
Journal of Applied Meteorology and Climatology
Journal of Atmospheric and Oceanic Technology
Journal of Climate
Journal of Hydrometeorology
Journal of Physical Oceanography
Journal of the Atmospheric Sciences
Monthly Weather Review
Weather and Forecasting
Weather, Climate, and Society
Meteorological Monographs
BROWSE
PUBLISH
SUBSCRIBE
ABOUT
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Journal of Physical Oceanography
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Issue
Journal
Volume 50 (2020): Issue 7 (Jul 2020)
Print ISSN:
0022-3670
Online ISSN:
1520-0485
ARTICLES
Mechanisms of Mid- to Outer-Shelf Transport of Shoreline-Released Tracers
The Influence of an Eddy in the Success Rates and Distributions of Passively Advected or Actively Swimming Biological Organisms Crossing the Continental Slope
Control of Bering Strait Transport by the Meridional Overturning Circulation
Global Characterization of the Ocean’s Internal Wave Spectrum
Breaking of Internal Waves and Turbulent Dissipation in an Anticyclonic Mode Water Eddy
The Evolution of a Buoyant River Plume in Response to a Pulse of High Discharge from a Small Midlatitude River
Nongeostrophic Baroclinic Instability over Sloping Bathymetry: Buoyant Flow Regime
Unraveling the Essential Effects of Flocculation on Large-Scale Sediment Transport Patterns in a Tide-Dominated Estuary
On the Mean Flow in the Western Gulf of Mexico and a Reappraisal of Errors in Ship-Drift Data
Why Does the Deep Western Boundary Current “Leak” around Flemish Cap?
Frontal Instability and Energy Dissipation in a Submesoscale Upwelling Filament
Near-Surface Ocean Kinetic Energy Spectra and Small-Scale Intermittency from Ship-Based ADCP Data in the Bay of Bengal
Dynamics of the Diurnal Warm Layer: Surface Jet, High-Frequency Internal Waves, and Mixing
Intraseasonal Variability of Cross-Slope Flow in the Northern South China Sea
CORRESPONDENCE
Comments on the Recent Discussion Concerning the Article “Diathermal Heat Transport in a Global Ocean Model”
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