Atmos. Chem. Phys. Discuss., 8, 15901-15939, 2008
www.atmos-chem-phys-discuss.net/8/15901/2008/
doi:10.5194/acpd-8-15901-2008
© Author(s) 2008. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Cloud phase identification of low-level Arctic clouds from airborne spectral radiation measurements: test of three approaches
A. Ehrlich1, E. Bierwirth1, M. Wendisch1, J.-F. Gayet2, G. Mioche2, A. Lampert3, and J. Heintzenberg4
1Johannes Gutenberg-University Mainz, Institute for Atmospheric Physics, Mainz, Germany
2Laboratoire de Météorologie Physique (LAMP), Univ. Blaise Pascal, Aubière Cedex, France
3Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany
4Leibniz-Institute for Tropospheric Research, Leipzig, Germany

Abstract. Boundary layer clouds were investigated with a complementary set of remote sensing and in situ instruments during the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign in March and April 2007. The clouds that formed in a cold air outbreak over the open Greenland sea showed a variety in their thermodynamic state. Beside the predominant mixed-phase clouds pure liquid and ice clouds were observed. Utilizing the measurements of solar radiation reflected by the clouds three methods to retrieve the thermodynamic phase of the cloud were defined and compared. Two ice indices IS and IP were obtained by analyzing the spectral pattern of the cloud top reflectance in the near infrared (1500–1800 nm wavelength) characterized by ice and water absorption. A third ice index IA is based on the different side scattering of spherical liquid water particles and nonspherical ice crystals which was recorded in simultaneous measurements of cloud albedo and reflectance.

Radiative transfer simulations showed that IS, IP and IA range between 5 to 80, 0 to 20 and 1 to 1.25, respectively, with lowest values indicating pure liquid water clouds and highest values pure ice clouds. IS and IP were found to be strongly sensitive to the effective diameter of the ice crystals present in the cloud. Therefore the identification of mixed-phase clouds requires a priori knowledge of the ice crystal dimension. IA has the disadvantage that this index is mainly dominated by the uppermost cloud layer (τ<1.5). Typical boundary layer mixed-phase clouds with a liquid cloud top layer will be identified as pure liquid water clouds. All three methods were applied to measurements above a cloud field observed during ASTAR 2007. The comparison with independent in situ microphysical measurements showed a good agreement in identifying the dominant mixed-phase clouds and a pure ice cloud at the edge of the cloud field.


Citation: Ehrlich, A., Bierwirth, E., Wendisch, M., Gayet, J.-F., Mioche, G., Lampert, A., and Heintzenberg, J.: Cloud phase identification of low-level Arctic clouds from airborne spectral radiation measurements: test of three approaches, Atmos. Chem. Phys. Discuss., 8, 15901-15939, doi:10.5194/acpd-8-15901-2008, 2008.
 
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