Some Chemical Aspects of Upper-atmosphere
Upper atmospheric composition and structure observation and measurement by chemiluminescent gas trails
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Upper atmospheric composition and structure observation and measurement by chemiluminescent gas trails
Upper atmospheric diurnal tide determined via sodium vapor trail measurements
Upper atmospheric helium ion chemical loss process, distribution of nitrogen ion and rate coefficient of helium ion-molecular nitrogen reaction
Upper atmosphere diurnal and seasonal latitudinal variations satellite data, showing diurnal bulge migration with subsolar point, 2 PM bulge peak, etc
Upper atmospheric nitric oxide determined from Aerobee measurement of UV dayglow spectra
Upper atmospheric composition, temperature, density, and pressure, and their variations
Uranus upper atmosphere occultation observations are reported for August 15-16, 1980, and April 26, 1981. Mean atmospheric light curves of 154 + or - 15 K and 132 + or - 15 K, respectively, are derived from the light curves. A comparison of all available Uranus occultation data since March 1977 suggests a significant mean atmospheric temperature change, with a typical 15 K/year variation. It is suggested that molecular and eddy diffusion, together with atmospheric dynamics, are potentially as important as radiation in the upper atmosphere heat balance of Uranus. The close agreement of occultation immersion and emersion temperatures further suggests that effective meridional transport occurs on Uranus.
The Upper Atmosphere Research Satellite (UARS) has been proposed for intensive studies of the 15-100 km-altitude region of the earth's atmosphere, begining in 1991. This 14,000-lb satellite will carry a suite of 10 instruments able to study the energy input and loss, photochemistry, and circulation of the upper atmosphere, as well as the extensive web of interactions among these three processes. UARS's remote sensors will give attention to the atmospheric molecular species of the nitrogen, hydrogen, and chlorine families.
Upper atmospheric turbulence velocity probability density investigated in 90 to 110 km region
Upper atmospheric dynamics, considering day-night density and pressure variation, wind structure, gravity waves, etc
Upper atmospheric winds measured up to 200 km height using chemiluminescent trail of rockets
Chemiluminescence of chemical compounds released in upper atmosphere and model of releases leading to upper atmospheric chemi-ionization
Mars upper atmosphere thermal structure from spectroscopic measurements and Mariner IV OCCULTATION experiment
Equatorial upper atmosphere wind measurements from IQSY sodium vapor cloud rocket launchings in India
Venusian upper atmosphere dissociation and ionization, considering photochemical and dynamic processes and molecular, eddy and ambipolar diffusions
Upper atmosphere structure and variations including density and composition in lower thermosphere, diurnal variations, variations with solar activity, etc
Mars upper atmosphere ionized carbon dioxide and CO emission spectra in 1900-4300 A region measured by Mariner 6, observing atomic hydrogen and oxygen lines
Upper atmosphere dynamics and model based on equations of mass, momentum, and energy