Fisheries Research Board of Canada, Pacific Oceanographic Group, 1962
Sometimes, in the course of plotting dynamic height and potential energy anomalies, an error in temperature or salinity is detected. It is often not expedient...
The present report consists of notes prepared for a series of six lectures given as part of the Geophysical Fluid Dynamics Seminars held at the Woods Hole...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Sverdrup (1947), Stommel (1948) and Munk (1950) have shown that the total steady-state transport of mass in the ocean depends primarily on the curl of the wind...
Describes the usage of thermodynamics in studying the physical properties of sea water. Includes a history of the development of thermometers for use at sea,...
Sea water is a complex fluid. Its physical properties such as thermal expansion, compressibility, etc., exhibit highly nonlinear behavior with respect to...
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