Abstract

In this study, an improved Data INterpolating Empirical Orthogonal Functions (DINEOF) algorithm for determination of missing values in a spatio-temporal dataset is presented. Compared with the ordinary DINEOF algorithm, the iterative reconstruction procedure until convergence based on every fixed EOF to determine the optimal EOF mode is not necessary and the convergence criterion is only reached once in the improved DINEOF algorithm. Moreover, in the ordinary DINEOF algorithm, after optimal EOF mode determination, the initial matrix with missing data will be iteratively reconstructed based on the optimal EOF mode until the reconstruction is convergent. However, the optimal EOF mode may be not the best EOF for some reconstructed matrices generated in the intermediate steps. Hence, instead of using asingle EOF to fill in the missing data, in the improved algorithm, the optimal EOFs for reconstruction are variable (because the optimal EOFs are variable, the improved algorithm is called VE-DINEOF algorithm in this study). To validate the accuracy of the VE-DINEOF algorithm, a sea surface temperature (SST) data set is reconstructed by using the DINEOF, I-DINEOF (proposed in 2015) and VE-DINEOF algorithms. Four parameters (Pearson correlation coefficient, signal-to-noise ratio, root-mean-square error, and mean absolute difference) are used as a measure of reconstructed accuracy. Compared with the DINEOF and I-DINEOF algorithms, the VE-DINEOF algorithm can significantly enhance the accuracy of reconstruction and shorten the computational time.

Highlights

  • Satellite-derived sea surface temperature (SST) data from infrared observations have been widely used in oceanography due to their extensive coverage, in time and space

  • To better validate the VE-Data INterpolating Empirical Orthogonal Functions (DINEOF) algorithm, the I-DINEOF algorithm was added in this paper to make a comparison with the VE-DINEOF algorithm

  • An improved DINEOF algorithm was presented in this study

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Summary

Introduction

Satellite-derived sea surface temperature (SST) data from infrared observations have been widely used in oceanography due to their extensive coverage, in time and space. These SST data are often influenced by the presence of clouds in the atmosphere, malfunctions in the satellite or images noises, which can cause missing data. The loss of data may reach a high percentage in some periods. A complete data set is desirable or even essential for many applications using satellite-derived data. PLOS ONE | DOI:10.1371/journal.pone.0155928 May 19, 2016

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