By L. Marton (ed.), Claire Marton (ed.)

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From this fact we deduce: (a) after the emission of each photon of 5577 the oxygen atom must either emit a photon of 6300 or leave the lD state by collisional deexcitati~n~; (b) the lack of covariance between 6300 and 5577 shows that the second alternative is followed; (c) therefore, the 6300 emission that we do observe must be due to some mechanism not associated with 5577 and must be emitted at a n atmospheric height where collisional deexcitation is less than it is in the 100-km region where 5577 occurs.

W ...... ..... ..... .. . . t .... LATITUDE 20° 40° 55O 65' FIG. 19. Idealized representation of magnetic tubes corresponding to different magnetic latitudes. Heights in the sketch are proportional to the length of a tube from the earth's surface to the equatorial crossing. The relative volumes with respect to unit terminal cross section are indicated. I n Fig. 19 the tubes corresponding t o several magnetic latitudes are displayed with their curvature removed. The volumes with respect to a fixed end area are approximately in the ratio 1 (20' latitude), 10 (40'), 100 (55'), and 1000 (65').

Geophys. Research 66, 4027 (1961). 67. K. L. Bowles, G. R. Ochs, and J. R. Green, J. Research Natl. Bur. Standards 66D,395 (1962). 68. B. J. O’Brien, J. Geophys. Research 67, 3687 (1962). 69. F. E. Roach, J. Geophys. Research 68, 1015 (1963). Recent Developments in Computer Organization F. P. BROOKS, JR. I B M Corporation, Poughkeepsie, New I-ork Page I. , . . . . . , , . , . . . . . , . , . . . . . , . . . . . . . . 45 11. Metaprograms . . . . . . . . . . . . . .

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