Effects of Cloud Horizontal Inhomogeneity on the Optical Thickness Retrieved from Moderate-Resolution Satellite Data
Open Access
- 1 July 2002
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 59 (14) , 2227-2242
- https://doi.org/10.1175/1520-0469(2002)059<2227:eochio>2.0.co;2
Abstract
Cloud remote sensing techniques are conventionally based on the independent pixel approximation (IPA). Here, three-dimensional (3D) radiative effects on IPA-based retrieved optical thickness from a visible-wavelength moderate-resolution (about 1 km) sensor are investigated. A Monte Carlo 3D radiative transfer model and a lognormal spectral cloud model are used to simulate monochromatic radiance reflected from overcast boundary layer cloud. A characterization of statistical properties of the optical thickness by the mean (M) and variance (S2) of the logarithm of the optical thickness is proposed, where S represents a degree of cloud inhomogeneity. Biases in retrieved values of the two parameters with the IPA are defined as ΔM and ΔS2 and attributed to neglect of net horizontal radiative transport in the IPA. Sensitivities of ΔM and ΔS2 are tested with respect to geometrical roughness, M, S, mean geometrical thickness, spectral exponent of optical thickness fluctuation, ground surface reflectance, ... Abstract Cloud remote sensing techniques are conventionally based on the independent pixel approximation (IPA). Here, three-dimensional (3D) radiative effects on IPA-based retrieved optical thickness from a visible-wavelength moderate-resolution (about 1 km) sensor are investigated. A Monte Carlo 3D radiative transfer model and a lognormal spectral cloud model are used to simulate monochromatic radiance reflected from overcast boundary layer cloud. A characterization of statistical properties of the optical thickness by the mean (M) and variance (S2) of the logarithm of the optical thickness is proposed, where S represents a degree of cloud inhomogeneity. Biases in retrieved values of the two parameters with the IPA are defined as ΔM and ΔS2 and attributed to neglect of net horizontal radiative transport in the IPA. Sensitivities of ΔM and ΔS2 are tested with respect to geometrical roughness, M, S, mean geometrical thickness, spectral exponent of optical thickness fluctuation, ground surface reflectance, ...Keywords
This publication has 39 references indexed in Scilit:
- Accuracy of the independent pixel approximation for satellite estimates of oceanic boundary layer cloud optical depthJournal of Geophysical Research: Atmospheres, 1997
- The Landsat Scale Break in Stratocumulus as a Three-Dimensional Radiative Transfer Effect: Implications for Cloud Remote SensingJournal of the Atmospheric Sciences, 1997
- Estimating Cloud Field Albedo Using One-Dimensional Series Of Optical DepthJournal of the Atmospheric Sciences, 1996
- Inferring Optical Depth of Broken Clouds from Landsat DataJournal of Climate, 1995
- Independent Pixel and Monte Carlo Estimates of Stratocumulus AlbedoJournal of the Atmospheric Sciences, 1994
- A Parameterization of Warm Clouds for Use in Atmospheric General Circulation ModelsJournal of the Atmospheric Sciences, 1994
- The Albedo of Fractal Stratocumulus CloudsJournal of the Atmospheric Sciences, 1994
- Cumulus cloud radiative properties and the characteristics of satellite radiance wavenumber spectraRemote Sensing of Environment, 1992
- Solar Radiative Fluxes for Stochastic, Scale-invariant Broken Cloud FieldsJournal of the Atmospheric Sciences, 1992
- Lidar Observations of the Fine-Scale Variability of Marine Stratocumulus CloudsJournal of Applied Meteorology and Climatology, 1988