Atmos. Chem. Phys. Discuss., 8, 17549-17580, 2008
www.atmos-chem-phys-discuss.net/8/17549/2008/
doi:10.5194/acpd-8-17549-2008
© Author(s) 2008. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Physical interpretation of the spectral radiative signature in the transition zone between cloud-free and cloudy regions
J. C. Chiu1, A. Marshak2, Y. Knyazikhin3, P. Pilewskie4, and W. J. Wiscombe2,5
1University of Maryland Baltimore County, Baltimore, MD, USA
2NASA/Goddard Space Flight Center, Greenbelt, MD, USA
3Boston University, Boston, MA, USA
4University of Colorado at Boulder, Boulder, CO, USA
5Brookhaven National Laboratory, New York, NY, USA

Abstract. One-second-resolution zenith radiance measurements from the Atmospheric Radiation Measurement program's new shortwave spectrometer (SWS) provide a unique opportunity to analyze the transition zone between cloudy and cloud-free air, which has considerable bearing on the aerosol indirect effect. In the transition zone, we find a remarkable linear relationship between the sum and difference of radiances at 870 and 1640 nm wavelengths. The intercept of the relationship is determined primarily by aerosol properties, and the slope by cloud properties. We then show that this linearity can be predicted from simple theoretical considerations and furthermore that it supports the hypothesis of inhomogeneous mixing, whereby optical depth increases as a cloud is approached but the effective drop size remains unchanged. In addition, the width of transition zones from SWS data is in the range of 50–150 m, which differs from the width in satellite observations (a few kilometers) and in airborne lidar data (1–2 km).

Citation: Chiu, J. C., Marshak, A., Knyazikhin, Y., Pilewskie, P., and Wiscombe, W. J.: Physical interpretation of the spectral radiative signature in the transition zone between cloud-free and cloudy regions, Atmos. Chem. Phys. Discuss., 8, 17549-17580, doi:10.5194/acpd-8-17549-2008, 2008.
 
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