Determination of ice cloud models using MODIS and MISR data

Representation of ice clouds in radiative transfer simulations is subject to uncertainties associated with the shapes and sizes of ice crystals within cirrus clouds. In this study, we examined several ice cloud models consisting of smooth, roughened, homogeneous and inhomogeneous hexagonal ice cryst...

Full description

Saved in:
Bibliographic Details
Published inInternational journal of remote sensing Vol. 33; no. 13; pp. 4219 - 4253
Main Authors Xie, Yu, Yang, Ping, Kattawar, George W, Minnis, Patrick, Hu, Yongxiang, Wu, Dong L
Format Journal Article
LanguageEnglish
Published Goddard Space Flight Center Taylor & Francis 10.07.2012
Taylor
Subjects
Online AccessGet full text
ISSN1366-5901
0143-1161
1366-5901
DOI10.1080/01431161.2011.642323

Cover

More Information
Summary:Representation of ice clouds in radiative transfer simulations is subject to uncertainties associated with the shapes and sizes of ice crystals within cirrus clouds. In this study, we examined several ice cloud models consisting of smooth, roughened, homogeneous and inhomogeneous hexagonal ice crystals with various aspect ratios. The sensitivity of the bulk scattering properties and solar reflectances of cirrus clouds to specific ice cloud models is investigated using the improved geometric optics method (IGOM) and the discrete ordinates radiative transfer (DISORT) model. The ice crystal habit fractions in the ice cloud model may significantly affect the simulations of cloud reflectances. A new algorithm was developed to help determine an appropriate ice cloud model for application to the satellite-based retrieval of ice cloud properties. The ice cloud particle size retrieved from Moderate Resolution Imaging Spectroradiometer (MODIS) data, collocated with Multi-angle Imaging Spectroradiometer (MISR) observations, is used to infer the optical thicknesses of ice clouds for nine MISR viewing angles. The relative differences between view-dependent cloud optical thickness and the averaged value over the nine MISR viewing angles can vary from −0.5 to 0.5 and are used to evaluate the ice cloud models. In the case for 2 July 2009, the ice cloud model with mixed ice crystal habits is the best fit to the observations (the root mean square (RMS) error of cloud optical thickness reaches 0.365). This ice cloud model also produces consistent cloud property retrievals for the nine MISR viewing configurations within the measurement uncertainties.
Bibliography:http://dx.doi.org/10.1080/01431161.2011.642323
GSFC
ISSN: 0143-1161
Report Number: GSFC-E-DAA-TN9683
GSFC-E-DAA-TN9683
Goddard Space Flight Center
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1366-5901
0143-1161
1366-5901
DOI:10.1080/01431161.2011.642323