The Distribution of Ocean Temperatures Along the West Coast of North America Ded
The Distribution of Ocean Temperatures Along the West Coast of North America Ded
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The estimated deviations of the directions of the coast from a north and south line at stations 1, 2, 3, and 4 are respectively (35), (30), (25), and (0) to the north west, and for stations 1 and 2, (x 2 ) = (2x 1 ), but for stations 3 and 4, (x 1 ) = 0. From this data, and the values of ( x i ~f" "sT**) obtained from formula (22) the corresponding distances (xi-J-Xo) were found to be 1670, 1120, 910, and 525 kilometers. An estimate based upon the isothermes of Thorade's charts, of the distance...s out from the coast to where the cooling effect was negligible gave the following series of values: 2150, 1450, 710, and 600 kilo- meters. In (Fig. 14, curves 3 and 1) these results are shown graphi- cally. These curves 1 and 3 would coincide if the theory and the ob- servations were correct. And the observed increase in width of the cold-water area agrees well with the results deduced from the observed winds. In (Fig. 15) are shown the contours of the ocean bottom perpen- dicular to the coast at each station.
What to read after The Distribution of Ocean Temperatures Along the West Coast of North America Ded?
You can find similar books in the "Read Also" column, or choose other free books by George F George Francis Mcewen to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The estimated deviations of the directions of the coast from a north and south line at stations 1, 2, 3, and 4 are respectively (35), (30), (25), and (0) to the north west, and for stations 1 and 2, (x 2 ) = (2x 1 ), but for stations 3 and 4, (x 1 ) = 0. From this data, and the values of ( x i ~f" "sT**) obtained from formula (22) the corresponding distances (xi-J-Xo) were found to be 1670, 1120, 910, and 525 kilometers. An estimate based upon the isothermes of Thorade's charts, of the distance...s out from the coast to where the cooling effect was negligible gave the following series of values: 2150, 1450, 710, and 600 kilo- meters. In (Fig. 14, curves 3 and 1) these results are shown graphi- cally. These curves 1 and 3 would coincide if the theory and the ob- servations were correct. And the observed increase in width of the cold-water area agrees well with the results deduced from the observed winds. In (Fig. 15) are shown the contours of the ocean bottom perpen- dicular to the coast at each station.
What to read after The Distribution of Ocean Temperatures Along the West Coast of North America Ded?
You can find similar books in the "Read Also" column, or choose other free books by George F George Francis Mcewen to read onlineMoreLess
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