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Titlebook: Mesospheric Models and Related Experiments; Proceedings of the F G. Fiocco Conference proceedings 1971 D. Reidel Publishing Company, Dordre

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A Meridional Model of the Oxygen-Hydrogen Atmosphere,mings of the latter — the distributions of atomic and molecular oxygen in the lower thermosphere, and water vapor above 70 km — were eliminated when vertical eddy mixing was introduced by Colegrove . (1965) for the pure oxygen model, and by Hesstvedt (1968) for the oxygen-hydrogen model.
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Discussion of the Formation of Major Positive and Negative Ions up to the 50 km Level,d and Ferguson, 1969; Ferguson and Fehsenfeld, 1969). Similar progress has been made on explaining the .-region negative ion chemistry, and some very successful results have been obtained in recent months (Ferguson, private communication).
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Eigil Hesstvedtcles. The particles can be atoms in a crystal, molecules in a gas or liquid, electrons in a plasma, amino acid units in a protein, elementary constituents in a complex polymer, etc. The forces between particles originate from Coulomb forces between electric charges and from magnetic dipole forces be
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