. Carnegie Institution of Washington publication. 92 DYNAMIC METEOROLOGY AND HYDROGRAPHY. The vector-addition will be performed according to the simplest law, that of scalar addition or subtraction, in all points where the two given vectors have either the same or opposite directions, , in the points of the curves (a) (b) a. i* j8-o o 32. « (i-a-o ,e p. Fig. 77.—Easily accessible data on the field of the vector-sum. A. First given vector (A, a). B. Second given vector (B, 0). C. Curves 0 —a = 0 and 0 —a =32, and their points of intersection with the required curves <p =12, 8, 4. D. Curv


. Carnegie Institution of Washington publication. 92 DYNAMIC METEOROLOGY AND HYDROGRAPHY. The vector-addition will be performed according to the simplest law, that of scalar addition or subtraction, in all points where the two given vectors have either the same or opposite directions, , in the points of the curves (a) (b) a. i* j8-o o 32. « (i-a-o ,e p. Fig. 77.—Easily accessible data on the field of the vector-sum. A. First given vector (A, a). B. Second given vector (B, 0). C. Curves 0 —a = 0 and 0 —a =32, and their points of intersection with the required curves <p =12, 8, 4. D. Curves 0 —o =0 and 0 —a =32 and their points of intersection with the required curves F = 11, 10, 9, . . In all points of the first curve the vector-sum F will have the same direction as both A and B,and a numerical value equal to their scalar sum. In all points of the second curve the vector-sum F will have the same direction as the greater of the vectors A and B, and a numerical value equal to their scalar difference. We can therefore. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Carnegie Institution of Washington. Washington, Carnegie Institution of Washington


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