Gaupnefjorden branch of Sognefjorden is strongly affected by freshwater as
glacial river flow in.
Not exact matches
With the chalk ridge forming a dam to the south, and the Rhine and other
rivers flowing into the
glacial lake, the water would have kept rising.
In the Andes,
glacial melt water supports
river flow and water supply for tens of millions of people during the long dry season.
If retreating from melt that means more
glacial melt water
flows into
rivers.
In the Indus, Ganges, Yellow, and Yangtze
River basins, where irrigated agriculture depends heavily on
rivers, the loss of
glacial - fed, dry - season
flow will shrink harvests and could create unmanageable food shortages.
Part of the water
flow in these
river basins depends on snow and
glacial melt to perennial
rivers, such as the Ganges, Indus, Brahmaputra, Mekong and Yangtze (9).
Higher elevation areas could experience altered water
flow in some
river basins if current rates of
glacial retreat continue, but shifts in the location, intensity, and variability of rain and snow due to climate change will likely have a greater impact on regional water supplies.
The observed effects of cryosphere reduction include modification of
river regimes due to enhanced
glacial melt, snowmelt advance and enhanced winter base
flow; formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven by ice and permafrost melting; regional ocean freshening; sea - level rise due to glacier and ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected by lake - ice and sea - ice reduction; changes in livelihoods; reduced tourism activities related to skiing, ice climbing and scenic activities in cryospheric areas affected by degradation; and increased ease of ship transportation in the Arctic.