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Technical Note: Glacial influence in tropical mountain hydrosystems evidenced by the diurnal cycle in water levels

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Figure

Fig. 1. Study area at the Antisana volcano, Ecuador. Stream sitesare represented by orange circles
Fig. 3. Mean monthly discharge data at two gauging stations withandglacier cover in the catchment) over 1 yr in the Antisana volcanocatchment, Ecuador
Table 1. Physico-chemical attributes of the study stream sites (see location of the sites on Fig
Fig. 4. Comparison of the wavelet analysis output (scale-averagedpower spectrum over 24 h scale) between discharge (black line) andwater-level time series (blue line) at site 7 (Los Crespos station).Dashed black and blue lines indicate the corresponding 95 % con-fidence levels for the red-noise spectrum for discharge and water-level time series, respectively.
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