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P. Koepke and K. T. Kriebel


The shortwave radiation field, i.e., in the solar spectral range, emerging at the top of the atmosphere is anisotropic due to the optical properties of the atmosphere and the reflectance characteristics of the underlying surface. Thus, anisotropy conversion factors are used to account for anisotropy in the derivation of flux densities from satellite measured broadband radiances. Uncertainties in the conversion factors due to uncertainties of the actual parameters of the atmosphere and the surface lead to errors in the derived net fluxes at the top and the bottom of the atmosphere and in the derived surface albedo. The errors for cloud-free situations over land, which this paper is only concerned with, are analyzed by simulation, using measured surface bidirectional reflectance functions and realistic values of the optical parameters of the atmosphere, including gas and aerosol absorption and multiple Battering. To derive surface albedo from planetary albedo, a linear relationship is commonly used. Improved values of its slope and intercept are presented, depending on solar zenith angle, turbidity and absorption.

The anisotropy conversion factors over land surfaces range from about 0.3 to 2 for low and 0.8 to 1.3 for high sun. To achieve an accuracy of 20 W m−2 in the net fluxes at the top of the atmosphere the uncertainty of the anisotropy conversion factors must be less than about 0.07 for vegetated and about 0.02 for surfaces with high albedo, decreasing with solar zenith angle. For the surface albedo derived from satellite measured radiances, the masking effect of the atmosphere gives additional errors. Thus, to achieve an accuracy of 20 W m−2 in the net fluxes at the surface the error due to anisotropy must be even lower. Global averages of anisotropy conversion factors have been derived from Nimbus-7 ERB data which are sufficiently accurate to be applied for global investigations or zonal averages. However, application of these factors to smaller areas, especially to surfaces with specific vegetation, will lead to larger uncertainties according to the deviation of the particular area from the global or zonal average. In such cases, regional anisotropy conversion factors, e.g., derived as described in Part II (Kriebel and Koepke) should be used.

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K. T. Kriebel and P. Koepke


A method is presented to obtain area mean radiant flux densities at the surface in the solar spectral range in cloud-free conditions. This is accomplished by fitting a realistic radiation model with actual atmospheric data and an anisotropic mixed surface reflection function. The latter is assumed to model anisotropy correctly but not the angular average value, i.e., the surface albedo. The surface albedo is tuned until computed and measured radiances incident on a satellite radiometer agree. Then the radiant flux densities, and the albedos and net fluxes, produced by the model are considered to be correct.

In a case study, the method is applied in La Mancha, Spain. Uniqueness and accuracy of the tuned radiation model is assessed by means of airborne radiance measurements. The overall agreement of measured and computed radiances is found to be 5%.

Flux densities and net fluxes derived from the tuned radiation model have accuracies of about ±15 W m−2, limited mainly by the present accuracy of the METEOSAT VIS channel calibration; surface albedo can be determined to approximately ±0.01 to ±0.015. These accuracies are obtained for instantaneous flux densities allowing their diurnal variability without time averaging to be derived.

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M. Hess, P. Koepke, and I. Schult

The software package OPAC (Optical Properties of Aerosols and Clouds) is described. It easily provides optical properties in the solar and terrestrial spectral range of atmospheric particulate matter. Microphysical and optical properties of six water clouds, three ice clouds, and 10 aerosol components, which are considered as typical cases, are stored as ASCII files. The optical properties are the extinction, scattering, and absorption coefficients, the single scattering albedo, the asymmetry parameter, and the phase function. They are calculated on the basis of the microphysical data (size distribution and spectral refractive index) under the assumption of spherical particles in case of aerosols and cloud droplets and assuming hexagonal columns in case of cirrus clouds. Data are given for up to 61 wavelengths between 0.25 and 40 μm and up to eight values of the relative humidity. The software package also allows calculation of derived optical properties like mass extinction coefficients and Ångström coefficients.

Real aerosol in the atmosphere always is a mixture of different components. Thus, in OPAC it is made possible to get optical properties of any mixtures of the basic components and to calculate optical depths on the base of exponential aerosol height profiles. Typical mixtures of aerosol components as well as typical height profiles are proposed as default values, but mixtures and profiles for the description of individual cases may also be achieved simply.

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