Air temperature had a highly significant positive effect on water temperature with a regression coefficient twice as big in the monthly compared to the daily model (Table 2 ).
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Timescale mediates the effects of environmental controls on water temperature in mid- to low-order streams.
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At the reach scale, the cooling effect of riparian cover became weaker with increasing timescale, its effect size halved and shifting from highly significant to marginally non-significant in the monthly model (Table 2 ); its relative importance reduced from 23.52 to 16.93% (Fig. 2 a-b).
On the other hand, older extrusive volcanic rocks often experience a decreasing trend in porosity and hydraulic conductivity with increasing geological age resulting from the filling of vesicles and fractures by secondary material.