Articles | Volume 14, issue 24
Atmos. Chem. Phys., 14, 13719–13737, 2014
https://doi.org/10.5194/acp-14-13719-2014
Atmos. Chem. Phys., 14, 13719–13737, 2014
https://doi.org/10.5194/acp-14-13719-2014

Research article 22 Dec 2014

Research article | 22 Dec 2014

A two-habit model for the microphysical and optical properties of ice clouds

C. Liu et al.

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Cited articles

Auriol, F., Gayet, J. F., Febvre, G., Jourdan, O., Labonnote, L. C., and Brogniez, G.: In situ observation of cirrus scattering phase functions with 22° and 46° halos: Cloud field study on 19 February 1998, J. Atmos. Sci., 58, 3376–3390, 2001.
Barkey, B. and Liou, K. N.: Polar nephelometer for light-scattering measurements of ice crystals, Opt. Lett., 26, 232–234, 2001.
Baran, A. J.: A review of the light scattering properties of cirrus, J. Quant. Spectrosc. Radiat. Transf., 110, 1239–1260, 2009.
Baran, A. J.: From the single-scattering properties of ice crystals to climate prediction: A way forward, Atmos. Res., 112, 45–69, 2012.
Baran, A. J. and Labonnote, L. C.: A self-consistent scattering model for cirrus. I: The solar region, Q. J. Roy. Meteorol. Soc., 133, 1899–1912, 2007.
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Short summary
An ice cloud model is developed by assuming an ice cloud to be an ensemble of columns and aggregates with specific habit fractions at each particle size bin. The microphysical and optical properties of this two-habit model (THM) are compared with both laboratory and in situ measurements. When the THM is applied to ice cloud property retrieval, excellent spectral consistency is achieved. A comparison between observed and theoretical polarized reflectivities illustrates the applicability of THM.
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