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Atmospheric boundary layer height estimation using a Kalman filter and a frequency-modulated continuous-wave radar
dc.contributor.author | Lange, Diego |
dc.contributor.author | Rocadenbosch Burillo, Francisco |
dc.contributor.author | Tiana Alsina, Jordi |
dc.contributor.author | Frasier, Steve |
dc.contributor.other | Universitat Politècnica de Catalunya. Departament de Teoria del Senyal i Comunicacions |
dc.date.accessioned | 2015-04-07T09:46:02Z |
dc.date.available | 2015-04-07T09:46:02Z |
dc.date.created | 2015-06-01 |
dc.date.issued | 2015-06-01 |
dc.identifier.citation | Lange, D. [et al.]. Atmospheric boundary layer height estimation using a Kalman filter and a frequency-modulated continuous-wave radar. "IEEE transactions on geoscience and remote sensing", 01 Juny 2015, vol. 53, núm. 6, p. 3338-3349. |
dc.identifier.issn | 0196-2892 |
dc.identifier.uri | http://hdl.handle.net/2117/27128 |
dc.description.abstract | An adaptive solution based on an Extended Kalman Filter (EKF) is proposed to estimate the Atmospheric Boundary-Layer Height (ABLH) from Frequency-Modulated Continuous-Wave (FMCW) S-band weather-radar returns. The EKF estimator departs from previous works, in which the transition interface between the Mixing-Layer (ML) and the Free-Troposphere (FT) is modeled by means of an erf-like parametric function. In contrast to lidar remote sensing where aerosols give strong backscatter returns over the whole ML, clear-air radar reflectivity returns (Bragg scattering from refractive turbulence) shows strongest returns from the ML-FT interface. In addition, they are corrupted by “insect” noise (impulsive noise associated with Rayleigh scatter ing from insects and birds), all of which requires a specific treatment of the problem and the measurement noise for the clear-air radar case. The proposed radar-ABLH estimation method uses: (i) a first pre-processing of the reflectivity returns based on median filtering and threshold-limited decision to obtain “clean” reflectivity signal, (ii) a modified EKF with adaptive range intervals as time tracking estimator, and (iii) ad-hoc modelling of the observation noise covariance. The method has successfully been implemented in clear-air, single-layer, convective boundary layer conditions. ABLH estimates from the proposed radar-EKF method have been cross-examined with those from a collocated lidar ceilometer yielding a correlation coefficient as high as rho = 0.93 (mean signal-to-noise ratio, SNR = 18 (linear units), at the ABLH) and in relation to the classic threshold method. |
dc.format.extent | 12 p. |
dc.language.iso | eng |
dc.publisher | Institute of Electrical and Electronics Engineers (IEEE) |
dc.subject | Àrees temàtiques de la UPC::Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica::Teledetecció |
dc.subject.lcsh | Remote sensing |
dc.subject.lcsh | Aerosols -- Remote sensing |
dc.subject.other | Adaptive kalman filtering |
dc.subject.other | laser radar |
dc.subject.other | remote sensing |
dc.subject.other | signal processing. |
dc.title | Atmospheric boundary layer height estimation using a Kalman filter and a frequency-modulated continuous-wave radar |
dc.type | Article |
dc.subject.lemac | Teledetecció |
dc.subject.lemac | Aerosols -- Teledetecció |
dc.contributor.group | Universitat Politècnica de Catalunya. RSLAB - Grup de Recerca en Teledetecció |
dc.identifier.doi | 10.1109/TGRS.2014.2374233 |
dc.description.peerreviewed | Peer Reviewed |
dc.relation.publisherversion | http://ieeexplore.ieee.org/xpls/abs_all.jsp?arnumber=6998066&tag=1 |
dc.rights.access | Open Access |
local.identifier.drac | 15555496 |
dc.description.version | Postprint (author’s final draft) |
local.citation.author | Lange, D.; Rocadenbosch, F.; Tiana, J.; Frasier, S. |
local.citation.publicationName | IEEE transactions on geoscience and remote sensing |
local.citation.volume | 53 |
local.citation.number | 6 |
local.citation.startingPage | 3338 |
local.citation.endingPage | 3349 |
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