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Original Articles

A photochemical model for the space-time variations of the oxygen allotropes in the 20 to 100 km layer

Pages 160-175 | Received 21 Jun 1965, Published online: 15 Dec 2016

References

  • CHAPMAN, S., 1930, A theory of upper atmospheric ozone. Mem. Roy. Soc. , 8, pp. 103–125.
  • DÜTscu, H. U., and CARLTON, L. M., 1964, Uniform evaluation of Umkelir observations from the World Ozone Network. Part II, Summary Supplement, The vertical distribution of ozone. National Center for Atmospheric Research, Boulder, Colorado.
  • HESSTVEDT, E., 1963, On the determination of characteristic times in a pure oxygen atmosphere. Tellas, 15,1, pp. 82–88.
  • HESSTVEDT, E., 1965, Some characteristics of the oxygen-hydrogen atmosphere. Geofysiske Publikasjoner, 26, No. 1.
  • JOHNSON, F., 1954, The solar constant. J. Meteor., 11, pp. 431–439.
  • LEOVY, C., 1963, Mesospheric heating and simple models of thermally driven circulation. Doctoral Thesis, M.I.T.
  • LONDON, J., 1962, Mesosphere dynamics. Final report, New York University. Contract No. AF19 (604)-5492.
  • NICOLET, M., 1960, Properties and constitution. Physics of the Upper Atmosphere, Academic Press, 2, pp. 17–69.
  • OHRIN G.G., 1958, The radiation budget of the stratosphere. J. Meteor. , 15, pp. 440–450.
  • PLASS, G., 1956, The influence of the 9.6 µ ozone band on the atmosphere infrared cooling rate. Roy. Met. Soc. , 82, pp. 3043.
  • Handbook of Geophysics, 1960. The Macmillan Company, New York, Chapter 8, p. 5.