Lower stratospheric radiative heating rates and sensitivities calculated from Antarctic balloon observations

Author:

Hicke Jeffrey,Tuck Adrian,Vömel Holger

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference35 articles.

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2. Berk , A. L. S. Bernstein D. C. Robertson MODTRAN: A moderate resolution model for LOWTRAN 7 Bedford, Mass. 1989

3. Very narrow band model calculations of atmospheric fluxes and cooling rates using the MODTRAN code;Bernstein;J. Atmos. Sci.,1996

4. The contributions of several absorption bands to stratospheric radiative dissipation rates;BreEer;J. Atmos. Sci.,1996

5. Line-by-line calculations of atmospheric fluxes and cooling rates: Application to water vapor;Clough;J. Geophys. Res.,1992

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1. Direct retrieval of stratospheric CO 2 infrared cooling rate profiles from AIRS data;Geophysical Research Letters;2006-06

2. MODTRAN 5: a reformulated atmospheric band model with auxiliary species and practical multiple scattering options: update;SPIE Proceedings;2005-06-01

3. Dynamical heating in the polar lower stratosphere and its impact on the tropopause;Journal of Geophysical Research: Atmospheres;2002-05-18

4. Polar stratospheric cloud impacts on Antarctic stratospheric heating rates;Quarterly Journal of the Royal Meteorological Society;2001-07

5. MODTRAN4: radiative transfer modeling for remote sensing;Algorithms for Multispectral, Hyperspectral, and Ultraspectral Imagery VI;2000-08-23

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