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|Title:||Applying DINEOF algorithm on cloudy sea-surface temperature satellite data over the eastern mediterranean sea||Authors:||Nikolaidis, Andreas
Georgiou, Georgios C.
Hadjimitsis, Diofantos G.
|Keywords:||Data reconstruction;DINEOF;Remote sensing;Sea-surface temperature||Category:||Earth and Related Environmental Sciences||Field:||Natural Sciences||Issue Date:||1-Apr-2013||Publisher:||SPIE||Source:||1st International Conference on Remote Sensing and Geoinformation of the Environment, RSCy 2013; Paphos; Cyprus; 8 April 2013 through 10 April 2013||DOI:||10.1117/12.2029085||Abstract:||Data Interpolating Empirical Orthogonal Functions (DINEOF) is a special technique which is based on Empirical Orthogonal Functions (EOF) in order to reconstruct missing data from satellite images. It is an innovative method, especially useful for filling in missing data from geophysical fields. Interesting examples could be clouds in sea-surface temperature (SST). Past studies have shown that filtering the temporal covariance matrix allows to reduce spurious variability and therefore a more realistic data reconstruction can be obtained. There is also provision in the estimation of the error covariance of the reconstruction of the data. Moreover, the error fields can be obtained with some calculation rearrangement. Error fields reflect the data-coverage structure and furthermore the covariance of the physical fields. Successful experiments on the Western Mediterranean encouraged the extension of the application of the method eastwards using similar experimental implementation. The present study summarizes the experimental work done, the implementation of the method and its ability in reconstructing the sea-surface temperature field over the Eastern Mediterranean basin, and specifically over Levantine sea and Cyprus.||URI:||http://ktisis.cut.ac.cy/handle/10488/9729||ISBN:||978-081949638-6||Rights:||© 2013 SPIE.||Type:||Conference Papers|
|Appears in Collections:||Δημοσιεύσεις σε συνέδρια/Conference papers|
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