The emissivity of foam-covered water surface at L-band: theoretical modeling and experimental results from the FROG 2003 field experiment

Sea surface salinity can be measured by microwave radiometry at L-band (1400–1427 MHz). This frequency is a compromise between sensitivity to the salinity, small atmospheric perturbation, and reasonable pixel resolution. The description of the ocean emission depends on two main factors: 1) the sea w...

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Detalles Bibliográficos
Autores: Rodríguez, R, Monerris Belda, Alessandra, Sabia, Roberto, Miranda Mendoza, Jorge José, Camps Carmona, Adriano José|||0000-0002-9514-4992, Vall-Llossera Ferran, Mercedes Magdalena|||0000-0003-1357-7098, Villarino Villarino, Ramón, Reul, N, Chapron, B, Corbella Sanahuja, Ignasi|||0000-0001-5598-7955, Duffo Ubeda, Núria|||0000-0002-9398-3995, Torres Torres, Francisco|||0000-0003-1160-6350
Tipo de recurso: artículo
Fecha de publicación:2005
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/10108
Acceso en línea:https://hdl.handle.net/2117/10108
https://dx.doi.org/10.1109/TGRS.2004.839651
Access Level:acceso abierto
Palabra clave:Brightness temperature
Microwave remote sensing
Signal theory (Telecommunication)
Microones -- Mesurament
Senyal, Teoria del (Telecomunicació)
Oceanografia
Àrees temàtiques de la UPC::Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica
Descripción
Sumario:Sea surface salinity can be measured by microwave radiometry at L-band (1400–1427 MHz). This frequency is a compromise between sensitivity to the salinity, small atmospheric perturbation, and reasonable pixel resolution. The description of the ocean emission depends on two main factors: 1) the sea water permittivity, which is a function of salinity, temperature, and frequency, and 2) the sea surface state, which depends on the wind-induced wave spectrum, swell, and rain-induced roughness spectrum, and by the foam coverage and its emissivity. This study presents a simplified two-layer emission model for foam-covered water and the results of a controlled experiment to measure the foam emissivity as a function of salinity, foam thickness, incidence angle, and polarization. Experimental results are presented, and then compared to the two-layer foam emission model with the measured foam parameters used as input model parameters. At 37 psu salt water the foam-induced emissivity increase is 0.007 per millimeter of foam thickness (extrapolated to nadir), increasing with increasing incidence angles at vertical polarization, and decreasing with