Interrelationships between atmospheric turbidity, the diffusely reflected visible radiation at the top of the earth's atmosphere and the global solar radiation at the surface

Author:

Rao C. R. Nagaraja,Takashima T.

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference12 articles.

1. Adams, C. R., Kattawar, G. W., 1970: Solution of radiative transfer by an invariant imbedding method.JQRST.,10, 341?356.

2. Braslau, N., Dave, J. V., 1973: Effect of aerosols on the transfer of solar energy through realistic model atmospheres. Part I: Non-absorbing aerosols.J. Appl. Meteor.,12, 601?615.

3. Gautier, C., Diak, G., Masse, S., 1980: A simple physical model to estimate incident solar radiation at the surface from GOES satellite data.J. Appl. Meteor.,19, 1005?1012.

4. Gautier, C., Frouin, R., 1985: Satellite-derived ocean surface radiation fluxes. In:Advances in Remote Sensing Retrieval Methods (Deepak, A., Fleming, H. E., Chahine, M. T., eds.), 311?329.

5. Griggs, M., Stowe, L. L., 1984: Measurements of aerosol parameters from satellites. In:IRS '84: Current Problems in Atmospheric Radiation (Fiocco, G., ed.), 42?45.

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