Active and Passive Remote Sensing of Ice.
The dyadic Green's functions (DGF) for an anisotropic (tilted uniaxial) medium have been evaluated for the unbounded and the two-layered cases. Inside the uniaxial medium, there are two characteristic waves, i.e. an o-wave and and e-wave. A wave incident with either TE or TM polarization produc...
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Format: | Text |
Language: | English |
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1983
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Online Access: | http://www.dtic.mil/docs/citations/ADA133672 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA133672 |
Summary: | The dyadic Green's functions (DGF) for an anisotropic (tilted uniaxial) medium have been evaluated for the unbounded and the two-layered cases. Inside the uniaxial medium, there are two characteristic waves, i.e. an o-wave and and e-wave. A wave incident with either TE or TM polarization produces both TE and TM waves when it reflected at the interface of an isotropic and a uniaxially anisotropic media because of its coupling into both the o-wave and the e-wave. With the availability of the DGF for anisotropic media, many layered-medium problems can now be solved. For instance, the problem of radiating a Hertzian dipole with an arbitrary orientation on top of a two layer anisotropic medium can readily be solved. |
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