Sea surface state measured using GPS reflected signals

We discuss an airborne experiment aimed to establish the potential of the Paris concept (PAssive Reflectometry and Interferometry System) to retrieve small features in the sea surface topography. The date and location were chosen to coincide with a TOPEX/POSEIDON (T/P) overflight. The signals of the...

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Detalles Bibliográficos
Autores: Rius, Antonio, Aparicio, Josep M., Cardellach, Estel, Martín-Neira, Manuel, Chapron, Bertrand
Tipo de recurso: artículo
Fecha de publicación:2002
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:dnet:digitalcsic_::c976abb8a180426d9f9ec458c9b1e74e
Acceso en línea:http://hdl.handle.net/10261/346595
https://api.elsevier.com/content/abstract/scopus_id/0036946013
Access Level:acceso abierto
Palabra clave:GNSS-R
ocean altimetry
ocean surface wind
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Descripción
Sumario:We discuss an airborne experiment aimed to establish the potential of the Paris concept (PAssive Reflectometry and Interferometry System) to retrieve small features in the sea surface topography. The date and location were chosen to coincide with a TOPEX/POSEIDON (T/P) overflight. The signals of the Global Positioning System (GPS) reflected off the sea surface are tracked and compared to the directly received ones, to compute the relative delays. The features detected in the peak tracking are likely caused by topographic and sea roughness variations. While very promising, these results open the challenge to use additional information to appropriately separate both contributions.