In dry
years glacier runoff constitutes most of later summer inflows to several large reservoirs.
Not exact matches
The team found that, for the last 20
years, the
glacier and ice cap mass loss has been exactly equal to the amount of meltwater
runoff lost to the sea.
Even worse, loss of summer
glacier runoff will mean a collapse of rice and wheat agriculture in the northwest of the country as Himalayan
glaciers continue to melt (current estimates are as high as 80 % loss within 30
years, and
runoff is already in decline).
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.
In fact in a dry
year such as 1998
glaciers yielded 28 billion gallons of
runoff to Baker Lake, while other sources were below average, which amounted to 45 % of the total basin flow.
In fact in a dry
year such as 1998
glaciers yielded 110 million m3 of
runoff to Baker Lake, while other sources were below average, which amounted to 45 % of the total basin flow (Pelto, 2008).
Although
glaciers calving into the ocean cause much of the ice loss in Greenland, other research cited in the study shows that the majority of ice loss in recent
years is from increased surface melt and
runoff.