Radiative heating-cooling and the energetics of the stratosphere and mesosphere
Author:
Publisher
American Geophysical Union (AGU)
Subject
Geophysics
Link
http://www.agu.org/journals/rg/v025/i003/RG025i003p00497/RG025i003p00497.pdf
Reference43 articles.
1. Parameterization of the radiative flux divergence in the 15μm CO2 band in the 30–75 km layer;Akmaev;J. Atmos. Terr. Phys.,1982
2. Radiative damping and amplitude of long wave-length modes in the stratosphere;Alimandi;J. Atmos. Sci.,1983
3. Radiative relaxation rates for individual 15−μ CO2 lines in the upper stratosphere and lower mesosphere;Apruzese;J. Geophys. Res.,1984
4. Parameterization of IR cooling in a middle atmosphere dynamics model. 1. Effects on the zonally averaged circulation;Apruzese;J. Geophys. Res.,1982
5. Parameterization of IR cooling in a middle atmosphere dynamics model 2. Non-LTE radiative transfer and the globally averaged temperature of the mesosphere and lower thermosphere;Apruzese;J. Geophys. Res.,1984
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1. The role of water-vapour photodissociation on the formation of a deep minimum in mesopause ozone;ANN GEOPHYS-ATM HYDR;1998
2. Carbon Dioxide 15-μm Band Cooling Rates in the Upper Middle Atmosphere Calculated by Curtis Matrix Interpolation;Journal of the Atmospheric Sciences;1990-03
3. On the role of vibration-vibration transitions in radiative cooling of the CO215 μm band around the mesopause;Journal of Geophysical Research;1990
4. The solar cycle and the QBO influences on the latitude of storm tracks in the North Atlantic;Geophysical Research Letters;1988-05
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