The mean rate at which mass is transported by ocean currents is believed to depend primarily on the mean wind stress on the ocean surface (Munk, 1950). In...
Algorithms for computation of fundamental properties of seawater, based on the practical salinity scale (PSS-78) and the international equation of state for...
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), Stompel (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...
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...
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...
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...
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