The Development of Midlatitude Cirrus Models for MODIS Using FIRE-I, FIRE-II, and ARM In Situ Data

Detailed in situ data from cirrus clouds have been collected during dedicated field campaigns, but the use of the size and habit distribution data has been lagging in the development of more realistic cirrus scattering models. In this study, the authors examine the use of in situ cirrus data collected during three field campaigns to develop more realistic midlatitude cirrus microphysical models. Data are used from the First International Satellite Cloud Climatology Project (ISCCP) Regional Experiment (FIRE)-I (1986) and FIRE-II (1991) campaigns and from a recent Atmospheric Radiation Measurement (ARM) Program campaign held in March‐April of 2000. The microphysical models are based on measured vertical distributions of both particle size and particle habit and are used to develop new scattering models for a suite of moderate-resolution imaging spectoradiometer (MODIS) bands spanning visible, near-infrared, and infrared wavelengths. The sensitivity of the resulting scattering properties to the underlying assumptions of the assumed particle size and habit distributions are examined. It is found that the near-infrared bands are sensitive not only to the discretization of the size distribution but also to the assumed habit distribution. In addition, the results indicate that the effective diameter calculated from a given size distribution tends to be sensitive to the number of size bins that are used to discretize the data and also to the ice-crystal habit distribution.

[1]  A. Macke,et al.  Single Scattering Properties of Atmospheric Ice Crystals , 1996 .

[2]  K. Liou,et al.  Finite-difference time domain method for light scattering by small ice crystals in three-dimensional space , 1996 .

[3]  Bryan A. Baum,et al.  Remote sensing of cloud properties using MODIS airborne simulator imagery during SUCCESS: 1. Data and models , 2000 .

[4]  R. Koelemeijer,et al.  Cirrus optical thickness and crystal size retrieval from ATSR-2 data using phase functions of imperfect hexagonal ice crystals , 1999 .

[5]  P. Watts,et al.  Testing the coherence of cirrus microphysical and bulk properties retrieved from dual‐viewing multispectral satellite radiance measurements , 1999 .

[6]  J. Foot,et al.  Some observations of the optical properties of clouds. II: Cirrus , 1988 .

[7]  Peter N. Francis,et al.  An observational and theoretical study of the radiative properties of cirrus: Some results from ICE'89 , 1994 .

[8]  A. Lacis,et al.  A description of the correlated k distribution method for modeling nongray gaseous absorption, thermal emission, and multiple scattering in vertically inhomogeneous atmospheres , 1991 .

[9]  W. Paul Menzel,et al.  Remote sensing of cloud properties using MODIS airborne simulator imagery during SUCCESS: 2. Cloud thermodynamic phase , 2000 .

[10]  Andrew J. Heymsfield,et al.  Relative Humidity and Temperature Influences on Cirrus Formation and Evolution: Observations from Wave Clouds and FIRE II , 1995 .

[11]  A. Heymsfield Cirrus Uncinus Generating Cells and the Evolution of Cirriform Clouds. Part I: Aircraft Observations of the Growth of the Ice Phase , 1975 .

[12]  K. M. Miller,et al.  The 27-28 October 1986 FIRE IFO cirrus case study : cloud microstructure , 1990 .

[13]  Ping Yang,et al.  Average ice crystal size and bulk short-wave single-scattering properties of cirrus clouds , 1998 .

[14]  K. Liou,et al.  Geometric-optics-integral-equation method for light scattering by nonspherical ice crystals. , 1996, Applied optics.

[15]  P. Francis,et al.  Aircraft measurements of the solar and infrared radiative properties of cirrus and their dependence on ice crystal shape , 1999 .

[16]  David P. Kratz,et al.  THE CORRELATED k-DISTRIBUTION TECHNIQUE AS APPLIED TO THE AVHRR CHANNELS , 1995 .

[17]  Anthony J. Baran,et al.  Sensitivity of retrieved POLDER directional cloud optical thickness to various ice particle models , 2000 .

[18]  W. Wiscombe,et al.  Exponential-sum fitting of radiative transmission functions , 1977 .

[19]  Andrew J. Heymsfield,et al.  A parameterization of the particle size spectrum of ice clouds in terms of the ambient temperature and the ice water content , 1984 .

[20]  Andrew A. Lacis,et al.  Sensitivity of cirrus cloud albedo, bidirectional reflectance and optical thickness retrieval accuracy to ice particle shape , 1996 .

[21]  Effects of ice-crystal structure on halo formation: cirrus cloud experimental and ray-tracing modeling studies. , 1994, Applied optics.

[22]  Michael D. King,et al.  Remote sensing of optical and microphysical properties of cirrus clouds using Moderate-Resolution Imaging Spectroradiometer channels: Methodology and sensitivity to physical assumptions , 2000 .

[23]  Andrew J. Heymsfield,et al.  A Balloon-Borne Continuous Cloud Particle Replicator for Measuring Vertical Profiles of Cloud Microphysical Properties: Instrument Design, Performance, and Collection Efficiency Analysis , 1997 .