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Artificial Intelligence for the Earth Systems
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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
Advanced Search
Help
Journal of Physical Oceanography
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Issue
Journal
Volume 13 (1983): Issue 10 (Oct 1983)
Print ISSN:
0022-3670
Online ISSN:
1520-0485
ARTICLES
Can the Western Boundary Layer Affect the Potential Vorticity Distribution in the Sverdrup interior of a Wind Gyre?
The Formation of Labrador Sea Water. Part I: Large-Scale Processes
The Formation of Labrador Sea Water. Part II. Mesoscale and Smaller-Scale Processes
Some Two-Layer Models of the Shelf-Slope Front: Geostrophic Adjustment and its Maintenance
Turbulent Dissipation Over the Continental Slope Off Vancouver Island
Laboratory Models of Bay-Type Continental Shelves in the Winter
Richardson Number Profiles over the Continental Shelf
Measurements of Gulf Stream Meandering and Evidence of Seasonal Thermocline Development Using Long-Range Acoustic Transmissions
Annual and Interannual Variability in the Kuroshio Current System
Estimates of Mass, Momentum and Kinetic Energy Fluxes of the Gulf Stream
On Equatorial Waves and El Niño. II: Effects of Air-Sea Thermal Coupling
Upper Ocean Heat Budget During the Hawaii-to-Tahiti Shuttle Experiment
Generation of Annual Rossby Waves in the North Pacific
A Simulation of Bomb Tritium Entry into the Atlantic Ocean
On the Flow Through Broad Gaps with Application to the Windward Passage
NOTES AND CORRESPONDENCE
The Principal Nonseasonal Modes of Variation of Global Sea Surface Temperature
On the Depth of Wave Influence
A Further Assessment of the Association between Sea Surface Temperature Gradient and the Overlying Mid-Tropospheric Circulation
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