Abstract

A long-term reliable sea surface temperature (SST) satellite data record is requisite resources for monitoring to understand climate variability. Creating a long-term data record especially for climate variability requires a combination of multiple satellite products. Consequently, missing data issues are inevitable. Hence, DINEOF (Data Interpolating Empirical Orthogonal Functions) has been applied to attain a complete and coherent multi-sensor SST data record with EOF-based technique by reconstructing the missing data. Unfortunately, the technique can lead to large discontinuities in the data reconstruction due to images depiction within long time series data. For that reason, filtering the temporal covariance matrix had been applied to reduce the spurious variability and more realistic reconstructions are obtained. However, this approach has not yet tested in tropical region with higher evaporation which cause incomplete satellite image coverage. Therefore, the objective of this research is to reconstruct SST of Lombok strait with data gaps up to 58.16% in one year. It is successfully reconstructed until the last iteration of 42 optimal EOF modes with the convergence achieved up to 0.9806×10-3, including previous set-aside data for internal cross-validation. The results highlight that the DINEOF method can effectively reconstruct SST data in Lombok Strait.

Highlights

  • Satellite-determined ocean sea surface temperature (SST) is one of the geophysical informational indexes from infrared perceptions that have been broadly utilized in oceanography because of their broad inclusion in reality

  • This research aims to reconstruct the sea surface temperature data in Lombok Strait to prove the possibility of Data Interpolating Empirical Orthogonal Functions (DINEOF) method can be used in the largest of cloudy area in the tropical sea which condensation may often occur in order to reproduce the clouds and several phenomena such as internal wave, monsoon, and El Niño–Southern Oscillation [12]

  • It is needed to detect the outliers within DINEOF as pixels for which the analysisobservations difference is larger than the statistically expected misfit calculated during the analysis

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Summary

Introduction

Satellite-determined ocean sea surface temperature (SST) is one of the geophysical informational indexes from infrared perceptions that have been broadly utilized in oceanography because of their broad inclusion in reality. These geophysical informational collections, explicitly those acquired from satellites, regularly contain holes (missing qualities) due to the presence of cloud, mists, downpour, or essentially because of deficient track inclusion. These SST information are frequently affected by mists' quality in the air, breakdowns in the satellite, or pictures commotions, which can cause missing information. Satellited-based data is not always producing cloud coverage problem

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