Abstract

The real world phenomena being observed by sensors are generally non-stationary in nature. The classical linear techniques for analysis and modeling natural time-series observations are inefficient and should be replaced by non-linear techniques of whose theoretical aspects and performances are varied. In this manner adopting the most appropriate technique and strategy is essential in evaluating sensors’ data. In this study, two different time-series analysis approaches, namely least squares spectral analysis (LSSA) and wavelet analysis (continuous wavelet transform, cross wavelet transform and wavelet coherence algorithms as extensions of wavelet analysis), are applied to sea-level observations recorded by tide-gauge sensors, and the advantages and drawbacks of these methods are reviewed. The analyses were carried out using sea-level observations recorded at the Antalya-II and Erdek tide-gauge stations of the Turkish National Sea-Level Monitoring System. In the analyses, the useful information hidden in the noisy signals was detected, and the common features between the two sea-level time series were clarified. The tide-gauge records have data gaps in time because of issues such as instrumental shortcomings and power outages. Concerning the difficulties of the time-frequency analysis of data with voids, the sea-level observations were preprocessed, and the missing parts were predicted using the neural network method prior to the analysis. In conclusion the merits and limitations of the techniques in evaluating non-stationary observations by means of tide-gauge sensors records were documented and an analysis strategy for the sequential sensors observations was presented.

Highlights

  • The surface of the sea deforms continuously

  • We aim to provide a methodological review for time-frequency analysis of non-stationary sensors observations using the least squares spectral analysis (LSSA) and wavelet analysis separately and clarifying superiorities and weaknesses of the experimented techniques

  • TUSELS presently consists of a data center in Ankara and a series of operational tide gauges located along the surrounding Mediterranean, Marmara, Aegean- and Black-Sea coasts of Turkey [39,40,41,42]

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Summary

Introduction

The surface of the sea deforms continuously. Its level, measured relative to an arbitrary datum, is calledsea level‘ and changes with time and is the most obvious indicator of ocean changes. We aim to provide a methodological review for time-frequency analysis of non-stationary sensors observations using the least squares spectral analysis (LSSA) and wavelet analysis separately and clarifying superiorities and weaknesses of the experimented techniques With this purpose we applied the techniques to estimate the spectra of the sea-level changes, employing the 19-year and 10-year data recorded at the Antalya-II and Erdek tide-gauge stations, respectively. From the CWTs of Erdek and Antalya-II tide-gauge records, we constructed the cross wavelet transform (XWT) which exposes the common power and relative phase of two sea-level data sets in time-frequency space, revealing the differences and similarities of the sea-level changes recorded in the open and semi-enclosed seas with respect to the locations of the Antalya-II and Erdek tide gauges Another useful quantity in measuring the cross-correlation between two time series as a function of frequency is the wavelet coherence (WTC). Wavelet is a strong method for the time-frequency analysis of non-stationary sequential data and is suggested for investigating sea-level changes

Tide-Gauge Stations in Turkey
Time-Series Analysis
Neural-Network Method for Sea-Level Data Predictions
Wavelet Analysis
Conclusions
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