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...

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Detalles Bibliográficos
Autores: Camps Carmona, Adriano José|||0000-0002-9514-4992, Vall-Llossera Ferran, Mercedes Magdalena|||0000-0003-1357-7098, Villarino Villarino, Ramón, Reul, Nicolas, Chapron, Bertrand, Corbella Sanahuja, Ignasi|||0000-0001-5598-7955, Duffo Ubeda, Núria|||0000-0002-9398-3995, Torres Torres, Francisco|||0000-0003-1160-6350, Miranda Mendoza, Jorge José, Sabia, Roberto, Monerris Belda, Alessandra, Rodríguez Sánchez, Rubén
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:2117/1045
Acceso en línea:https://hdl.handle.net/2117/1045
Access Level:acceso abierto
Palabra clave:Microwave measurements
Oceanography
Radiometry
Remote sensing
microwave measurement
ocean temperature
oceanographic regions
oceanographic techniques
radiometry
remote sensing
seawater
Microones -- Mesurament
Oceanografia
Radiometria
Sensors remots
Àrees temàtiques de la UPC::Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica::Circuits de microones, radiofreqüència i ones mil·limètriques
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 /spl sim/0.007 per millimeter of foam thickness (extrapolated to nadir), increasing with increasing incidence angles at vertical polarization, and decreasing with increasing incidence angles at horizontal polarization.