Other
Scientific paper
May 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006agusmsa53a..07k&link_type=abstract
American Geophysical Union, Fall Meeting 2007, abstract #SA53A-07
Other
0340 Middle Atmosphere: Composition And Chemistry, 0350 Pressure, Density, And Temperature, 0360 Radiation: Transmission And Scattering, 1640 Remote Sensing (1855)
Scientific paper
Adequate retrieval of kinetic temperature and other parameters in the summer polar mesosphere and lower thermosphere (MLT) from limb infrared radiances requires detailed accounting for the breakdown of local thermodynamic equilibrium (NLTE). A large fraction of the limb radiance is formed by resonant scattering of the upwelling radiation from the stratosphere and therefore, does not have links to the local thermal radiation sources. Moreover, in case of CO2, this scattering depends strongly on the V-V rate of the ν2 quanta exchange between isotopes. As a result, both the temperature values and the position of the retrieved mesopause depend on the rate coefficient of this process. On the other hand, the lower boundary of a noctilucent cloud (NLC) lies near the lower crossing point of the temperature profile and the frost point curve. This suggests that NLC observations may provide an important tool for validating temperature and water vapor density retrievals as well as the NLTE model describing the formation of infrared radiance in the MLT. This paper will describe these considerations including examples using the TIMED-SABER data for the polar summer mesosphere.
Feofilov A.
Goldberg Richard A.
Gordley Larry L.,
Kutepov Andrey
Marshall Benjamin T.
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