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Polarimetric emission of rain events: simulation and experimental results at X-Band
dc.contributor.author | Duffo Ubeda, Núria |
dc.contributor.author | Vall-Llossera Ferran, Mercedes Magdalena |
dc.contributor.author | Camps Carmona, Adriano José |
dc.contributor.author | Corbella Sanahuja, Ignasi |
dc.contributor.author | Torres Torres, Francisco |
dc.contributor.other | Universitat Politècnica de Catalunya. Departament de Teoria del Senyal i Comunicacions |
dc.date.accessioned | 2010-06-04T11:41:53Z |
dc.date.available | 2010-06-04T11:41:53Z |
dc.date.created | 2009-06 |
dc.date.issued | 2009-06 |
dc.identifier.citation | Duffo, N. [et al.]. Polarimetric emission of rain events: simulation and experimental results at X-Band. "Remote Sensing", Juny 2009, vol. 1, p. 107-121. |
dc.identifier.issn | 2072-4292 |
dc.identifier.uri | http://hdl.handle.net/2117/7523 |
dc.description.abstract | Accurate models are used today for infrared and microwave satellite radiance simulations of the first two Stokes elements in the physical retrieval, data assimilation etc. of surface and atmospheric parameters. Although in the past a number of theoretical and experimental works have studied the polarimetric emission of some natural surfaces, specially the sea surface roughened by the wind (Windsat mission), very limited studies have been conducted on the polarimetric emission of rain cells or other natural surfaces. In this work, the polarimetric emission (four Stokes elements) of a rain cell is computed using the polarimetric radiative transfer equation assuming that raindrops are described by Pruppacher-Pitter shapes and that their size distribution follows the Laws-Parsons law. The Boundary Element Method (BEM) is used to compute the exact bistatic scattering coefficients for each raindrop shape and different canting angles. Numerical results are compared to the Rayleigh or Mie scattering coefficients, and to Oguchi’s ones, showing that above 1-2 mm raindrop size the exact formulation is required to model properly the scattering. Simulation results using BEM are then compared to the experimental data gathered with a X-band polarimetric radiometer. It is found that the depolarization of the radiation caused by the scattering of non-spherical raindrops induces a non-zero third Stokes parameter, and the differential phase of the scattering coefficients induces a non-zero fourth Stokes parameter. |
dc.format.extent | 15 p. |
dc.language.iso | eng |
dc.subject | Àrees temàtiques de la UPC::Enginyeria de la telecomunicació::Processament del senyal |
dc.subject | Àrees temàtiques de la UPC::Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica |
dc.subject.lcsh | Microwaves |
dc.subject.lcsh | Signal theory (Telecommunication) |
dc.title | Polarimetric emission of rain events: simulation and experimental results at X-Band |
dc.type | Article |
dc.subject.lemac | Senyal, Teoria del (Telecomunicació) |
dc.subject.lemac | Microones |
dc.contributor.group | Universitat Politècnica de Catalunya. RSLAB - Grup de Recerca en Teledetecció |
dc.contributor.group | Universitat Politècnica de Catalunya. RF&MW - Grup de Recerca de sistemes, dispositius i materials de RF i microones |
dc.identifier.doi | 10.3390/rs1020107 |
dc.rights.access | Open Access |
local.identifier.drac | 1612580 |
dc.description.version | Postprint (published version) |
local.citation.author | Duffo, N.; Vall·Llosera, M.; Camps, A.; Corbella, I.; Torres, F. |
local.citation.publicationName | Remote Sensing |
local.citation.volume | 1 |
local.citation.startingPage | 107 |
local.citation.endingPage | 121 |
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