Estimating Cl2 over snow and sea ice from meteorological data
The refractive-index structure parameter C2, defined from [n(x)- n(x + r)]2 = Cn2r"3 (1.1) is an important quantity in the study of electromagnetic wave propagation in the atmospheric surface layer. Here nis the turbulent refractive-index fluctuation, x and x + r are
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| Format: | Text |
| Language: | English |
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1987
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.837 http://www.nwra.com/resumes/andreas/publications/JOSA_1988.pdf |
| Summary: | The refractive-index structure parameter C2, defined from [n(x)- n(x + r)]2 = Cn2r"3 (1.1) is an important quantity in the study of electromagnetic wave propagation in the atmospheric surface layer. Here nis the turbulent refractive-index fluctuation, x and x + r are |
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