Extension of kirchhoff method under stationary phase approximation to determination of polarimetric thermal emission from the sea

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To access the full text documents, please follow this link: http://hdl.handle.net/2117/98034

dc.contributor	Universitat Politècnica de Catalunya. Departament de Teoria del Senyal i Comunicacions
dc.contributor	Universitat Politècnica de Catalunya. RSLAB - Grup de Recerca en Teledetecció
dc.contributor	Universitat Politècnica de Catalunya. ANTENNALAB - Grup d'Antenes i Sistemes Radio
dc.contributor.author	Camps Carmona, Adriano José
dc.contributor.author	Corbella Sanahuja, Ignasi
dc.contributor.author	Rius Casals, Juan Manuel
dc.date	1998-07
dc.identifier.citation	Camps, A., Corbella, I., Rius, J. Extension of kirchhoff method under stationary phase approximation to determination of polarimetric thermal emission from the sea. "Electronics Letters", Juliol 1998, vol. 34, núm. 15, p. 1501-1503.
dc.identifier.citation	0013-5194
dc.identifier.citation	10.1049/el:19981055
dc.identifier.uri	http://hdl.handle.net/2117/98034
dc.language.iso	eng
dc.publisher	Institution of Electrical Engineers
dc.relation	http://ieeexplore.ieee.org.recursos.biblioteca.upc.edu/document/706250/
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Àrees temàtiques de la UPC::Enginyeria de la telecomunicació
dc.subject	Telecommunication
dc.subject	Wind
dc.subject	Telecomunicació
dc.title	Extension of kirchhoff method under stationary phase approximation to determination of polarimetric thermal emission from the sea
dc.type	info:eu-repo/semantics/publishedVersion
dc.type	info:eu-repo/semantics/article
dc.description.abstract	Wind direction over the sea can be determined from radiometric measurements of the third Stokes parameter (T/sub U/). The Kirchhoff method is extended under the stationary phase approximation to compute the dependence of T/sub U/ on frequency, wind speed and incidence angle. Numerical predictions, in agreement with experimental measurements, are presented.
dc.description.abstract	Peer Reviewed

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