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Dissociation of Molecular Oxygen in the Schumann-Runge Bands
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 ...
Atmospheric Opacity. in the Schumann-Runge Bands and the Aeronomic Dissociation of Water Vapor
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 ...
The Detection of Long-Term Changes in Stratospheric Ozone: Scientific Requirements and Current Results from Satellite-Based Measurement Systems
Publisher: American Meteorological Society
Abstract: The ability to detect subtle trends in upper stratospheric ozone places strict requirements on satellite-based Solar Backscatter Ultraviolet (SBUV) sensors intended for this purpose. Simulation of the long-term change in ...
Atmospheric Temperatures near the Tropical Tropopause: Temporal Variations, Zonal Asymmetry and Implications for Stratospheric Water Vapor
Publisher: American Meteorological Society
Abstract: Analysis of temperature measurements obtained over an eight-year period in the vicinity of the low-latitude tropopause confirms the existence of longitude regions which are consistently colder by approximately 2?3 K than ...
Predissociation of Nitric Oxide in the Mesosphere and Stratosphere
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 ...
Ozone Abundances in the Lower Mesosphere Deduced from Backscattered Solar Radiances
Publisher: American Meteorological Society
Abstract: Backscatter ultraviolet data obtained by the Explorer E satellite imply very large ozone column abundances above 56 km in the tropics during mid-day. The number of molecules in a vertical column decays by a factor of 2?3 ...