Glacier change and
glacier runoff variation in the Tuotuo River basin, the source region of Yangtze River in western China.
Not exact matches
Regular
variation in the solid
runoff of Antarctic
glaciers with the period of 18.6 years is revealed as a result of long - term observations.
Inter-annual
runoff variation in the Himalayan
glacier catchment is driven more by precipitation than by the mass balance change of
glaciers (36);