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    Dissociation of Molecular Oxygen in the Schumann-Runge Bands 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 005:;page 1099
    Author(s): Frederick, J. E.; Hudson, R. D.
    Publisher: American Meteorological Society
    Abstract: Oscillator strengths and predissociation linewidths deduced in recent studies predict a dissociation rate for O2 in the Schumann-Runge bands which is significantly larger in the upper stratosphere and lower mesosphere than ...
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    Atmospheric Opacity. in the Schumann-Runge Bands and the Aeronomic Dissociation of Water Vapor 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 005:;page 1088
    Author(s): Frederick, J. E.; Hudson, R. D.
    Publisher: American Meteorological Society
    Abstract: Knowledge of the agronomic production of odd hydrogen in the dissociation of water vapor is limited by uncertainties in the penetration of solar irradiance in the Schumann-Rung bands of O2 and by incomplete information ...
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    Predissociation of Nitric Oxide in the Mesosphere and Stratosphere 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 004:;page 737
    Author(s): Frederick, J. E.; Hudson, R. D.
    Publisher: American Meteorological Society
    Abstract: Absorption of solar photons by nitric oxide in the wavelength ranges 181.3?183.5 and 189.4?191.6 nm leads to predissociation of the molecule in the mesosphere and upper stratosphere. Molecular oxygen controls the penetration ...
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    Radiation and Ozone 

    Source: Bulletin of the American Meteorological Society:;2009:;volume( 090 ):;issue: 011:;page 1669
    Author(s): Ohring, G.; Bojkov, R. D.; Bolle, H-J.; Hudson, R. D.; Volkert, H.
    Publisher: American Meteorological Society
    Abstract: Radiation is the driving force for the general circulation of the atmosphere and controls the Earth's climate. Ozone is responsible for the warm stratosphere and protects life on Earth from harmful solar ultraviolet ...
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