Abstract

Seawaters exhibit various types of cyclic and trend-like temporal alterations in their biological, physical, and chemical processes. Surface water dynamics may vary, for instance, when the timings, durations, or amplitudes of seasonal developments of water properties alter between years and locations. We introduce a workflow using remote sensing to identify surface waters undergoing similar dynamics. The method, called ocean surface dynamics partitioning, classifies pixels based on their temporal change patterns instead of their properties at successive time snapshots. We apply an efficient parallel computing method to calculate Dynamic Time Warping (DTW) time series distances of large datasets of Earth Observation MERIS-instrument reflectance data Rrs(510 nm) and Rrs(620 nm), and produce a matrix of time series distances between 12,252 locations/time series in the Baltic Sea, for both wavelengths. We define cluster prototypes by hierarchical clustering of distance matrices and use them as initial prototypes for an iterative process of partitional clustering in order to identify areas that have similar reflectance dynamics. Lastly, we compute distances from the time series of the reflectance data to selected physical factors (wind, precipitation, and changes in sea surface temperature) obtained from Copernicus data archives. The workflow is reproducible and capable of managing large datasets in reasonable computation times and identifying areas of distinctive dynamics. The results show spatially coherent and logical areas without a priori information about the locations of the satellite image time series. The alignments of the reflectance time series vs. the observational time series of the physical environment clarify the causalities behind the cluster formation. We conclude that following the changes in an aquatic realm by biogeochemical observations at certain temporal intervals alone is not sufficient to identify environmental shifts. We foresee that the changes in dynamics are a sensitive measure of environmental threats and therefore they will be important to follow in the future.

Highlights

  • The proper methodological choices and the dynamics of the northernmost basins were studied with different Dynamic Time Warping (DTW) algorithms and partitioning methods in Suominen [38], and on a general level the spatial patterns were similar to the patterns observed in this study

  • We define our approach as ocean surface dynamics partitioning as the unit of partitioning is dynamics as a whole

  • The surface layer dynamics partitioning succeeded to identify diversity in a marginal sea, where the dynamics is unclear at times

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Summary

Introduction

Chemical, and biological processes in oceans and seas proceed in temporal cycles of different lengths, from diurnal and seasonal [1,2,3,4,5] to longer periods, such as the El Niño cycle in the Pacific Ocean [6,7]. Compared to trend-like changes, such as eutrophication [8,9,10] and seawater acidification [11,12], cyclic processes show a degree of recurrence, yet they may be difficult to observe if embedded within other dynamic processes. For example, multiple factors like seawater stratification, river outlets, and local geographical features are present. The momentary state of a given point of the sea surface reflects recent weather conditions and many

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