Abstract:
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It is classic to decompose a time series into oscillations, smooth variability, as well as an irregular component. When we observe more than one such time series, the description of an oscillation becomes more complex, as an underlying geometry will underpin our description. We shall discuss how to describe this phenomena, and show its utility when modelling and inferring observations from climate time series, namely the global drifter programme. We shall also discuss what happens if the generating mechanism of the time series is evolving very rapidly, violating classic assumptions, and what additional assumptions are needed to still be able to make inferences.
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