Seasonal variations of water temperature and discharge in rivers draining ice-free and partially-glacierized Alpine basins
2009
Records of discharge and temperature of water in rivers draining from 3 Alpine basins between
ice-free and 66% glacier-covered, in the upper Aare and Rhone catchments, Switzerland, were
examined in order to assess the impacts of percentage glacierisation of large basins on runoff
regime and seasonal pattern of river water temperature. The month with maximum runoff is
delayed from May for the ice-free Allenbach to July and August for the ice-melt dominated
Lonza and Massa. Ice-melt contributions to runoff suppressed water temperatures in summer in
the two glacier-fed rivers, but a distinctive seasonal temperature regime was observed only in the
Massa, draining the most highly-glacierised basin. Maximum water temperature in the Massa
occurred at low flow in April. Subsequently as icemelt discharge increased, water temperature
decreased and mean monthly temperature was maintained at about the same level between July
and September.
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