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Moreover, concentrated on the northwest quarter of the island, the lakes with these types of catchment are exposed to more variable and intense precipitation fuelled by the NAO. Given that the quantity, timing and variability of water inputs to a lake are all dependent on the complex interactions between the weather and the biophysical environment as water flows through the hydrologic cycle, this particular combination of hydrological behaviour and local weather conditions appear to be the key drivers behind the observed differences in covariation patterns between these peatland lakes and the other lakes in our study. Our results suggest that anthropogenic pressures, as defined by the presence of water abstraction activities from lakes and the human population density of their catchments, play a significant role in modifying the influence of the NAO on lake water levels.