By P. M. Banks and G. Kockarts (Auth.)
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G, and i / at height z = z0. 14) in series enables a comparison to be made with the isothermal atmosphere model. These can be written as follows : P Po expi i(H+H0) (ΜΉ} 3 \H + H0. 4. 18) Numerical Values between 15 and 100 km In recent years the density of the homosphere has been explored above 30 km by rockets which have given a general picture of the homosphere up to the mesopause. Variations are observed and it is difficult to use a standard model to represent the atmosphere with its seasonal and latitudinal variations [1-7].
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Axford, in Atmospheric Emissions (B. M. McCormac and A. ), pp. 317-325. Van Nostrand-Reinhold, Princeton, New Jersey, 1969. 12. G. Kockarts and M. Nicolet, Ann. Géophys. 18, 269 (1962). 13. T. N. L. Patterson, Rev. Geophys. 6, 553 (1968). 14. W. I. Axford, / . Geophys. Res. 73, 6855 (1968). 15. P. M. Banks and T. E. Hölzer, / . Geophys. Res. 74, 6317 (1969). 16. -É. Blamont, Personal communication (1971). 17. H. E. Johnson and W. I. Axford, / . Geophys. Res. 74, 2433 (1969). 18. M. Nicolet, Bull.