Author:
Manninen T.,Riihelä A.,de Leeuw G.
Abstract
Abstract. Ground-based pyranometer measurements of broadband surface albedo values are affected by the atmospheric conditions. A new method for estimating the magnitude of this effect in clear sky conditions is presented. Global and reflected radiation values and AOD values at two wavelengths are needed to apply the method. Depending on the atmospheric optical depth and the sun zenith angle values the effect can be as large as 20%. For the test case of Cabauw the atmosphere caused typically 5% higher surface albedo values than the corresponding black-sky surface albedo values.
Reference32 articles.
1. Ångström, A.: On the Atmospheric Transmission of Sun Radiation and on Dust in the Air, Geogr. Ann., 11, 156–166, 1929.
2. ASTM Standard G173-03: Standard Tables for Reference Solar Spectral Irradiances: Direct Normal and Hemispherical on a 37 Tilted Surface, ASTM Standard G173-03, American Society for Testing and Materials, West Conshohocken, PA, June 1999.
3. Bird, R. E. and Riordan, C.: Simple Solar Spectral Model for Direct and Diffuse Irradiance on Horizontal and Tilted Planes at the Earth's Surface for Cloudless Atmospheres, J. Clim. Appl. Meteorol., 25, 87–97, 1986.
4. Briegleb, B. P., Minnis, P., Ramanathan, V., and Harrison, E.: Comparison of Regional Clear-Sky Albedos Inferred from Satellite Observations and Model Computations, J. Clim. Appl. Meteorol., 25, 214–226, 1986.
5. Carrer, D., Geiger, B., Roujean, J.-L., Hautecoeur, O., Cedilnik, J., Mahfouf, J.-F., Meurey, C., and Franchisteguy, L.: Land surface albedo from MSG/SEVIRI: Retrieval method, validation, and application for weather forecast, Proc. IGARSS'09 IV, 288–291, 2009.
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