DETERMINATION OF AEROSOL SIZE DISTRIBUTION FROM BACKSCATTERED RADIATION BY MEANS OF "PSEUDO" EMPIRICAL ORTHOGONAL FUNCTIONS (SCATTERING).
The amount of information (types of solutions, accuracy and moments of the solution) about tropospheric rural aerosol size distribution that can in theory be obtained from backscattered measurements, without using any additional information about the anticipated solution, has been discussed. In prac...
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| Language: | en |
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The University of Arizona.
1986
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| Online Access: | http://hdl.handle.net/10150/188140 |