Eulogio Pardo-Igúzquiza

Dr. Eulogio Pardo-Igúzquiza

orcid

Research Focus & Metrics

Academic Career Length

35Years (1992-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 September 1999 in Journal of Hydrology
Verified
Journal Article
Closed access
DGD.I.F Grimes
D.I.F Grimes
EPEulogio Pardo-Igúzquiza
Eulogio Pardo-Igúzquiza
RBR Bonifacio
R Bonifacio

1 February 1993 in Mathematical Geology
Verified
Journal Article
Closed access
PDF file
EPEulogio Pardo-Igúzquiza
Eulogio Pardo-Igúzquiza
MCM. Chica-Olmo
M. Chica-Olmo

1 May 2006 in Remote Sensing of Environment
Verified
Journal Article
Closed access
EPEulogio Pardo-Igúzquiza
Eulogio Pardo-Igúzquiza
MCMario Chica-Olmo
Mario Chica-Olmo
PAPeter Atkinson
Peter Atkinson


16 January 2008 in IEEE Transactions on Geoscience and Remote Sensing
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Journal Article
Closed access
PAPeter Atkinson
Peter Atkinson
EPEulogio Pardo-Igúzquiza
Eulogio Pardo-Igúzquiza
MCMario Chica-Olmo
Mario Chica-Olmo
The main aim of this paper is to show the implementation and application of downscaling cokriging for super-resolution image mapping. By super-resolution, we mean increasing the spatial resolution of satellite sensor images where the pixel size to be predicted is smaller than the pixel size of the empirical image with the finest spatial resolution. It is assumed that coregistered images with different spatial and spectral resolutions of the same scene are available. The main advantages of cokriging are that it takes into account the correlation and cross correlation of images, it accounts for the different supports (i.e., pixel sizes), it can explicitly take into account the point spread function of the sensor, and it has the property of prediction coherence. In addition, ancillary images (topographic maps, thematic maps, etc.) as well as sparse experimental data could be included in the process. The main problem is that super-resolution cokriging requires several covariances and cross covariances, some of which are not empirically accessible (i.e., from the pixel values of the images). In the adopted solution, the fundamental concept is that of covariances and cross-covariance models with point support. Once the set of point-support models is estimated using linear systems theory, any pixel-support covariance and cross covariance can be easily obtained by regularization. We show the performance of the method using Landsat Enhanced Thematic Mapper Plus images.

1 January 2005 in Palaeogeography, Palaeoclimatology, Palaeoecology
Verified
Journal Article
Closed access
Gonzalo Jiménez-MorenoGonzalo Jiménez-Moreno
Gonzalo Jiménez-Moreno
FRFrancisco J. Rodríguez-Tovar
Francisco J. Rodríguez-Tovar
EPEulogio Pardo-Igúzquiza
Eulogio Pardo-Igúzquiza
SFSéverine Fauquette
Séverine Fauquette
JSJean-Pierre Suc
Jean-Pierre Suc
PMPál Müller
Pál Müller