This paper explores patterns within and between climatological and hydrological time series from an alpine glacier basin. Time series recorded in the basin of the Haut Glacier d'Arolla over the 1989 ablation season are subdivided into five subperiods. Box‐Jenkins ARIMA (AutoRegressive Integrated Moving Average) and TFN (Transfer Function‐Noise) models are estimated for each of the five subperiods and differences between the models are interpreted in the context of changing glacier hydrology, particularly the changing nature and extent of the glacier drainage network.
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Gurnell et al. (1992) studied this question.
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