Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
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...
Fisheries Research Board of Canada, Pacific Oceanographic Group, 1957
Input routines and subroutines for the ALWAC III-E computer program, generating oceanographic data for sound velocity, observed depths, temperature and...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
Sverdrup (1947), Stommel (1948), and Munk (1950) have shown that the total steady-state transport of the mass in the ocean depends primarily on the curl of the...
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