«In previous tests, we found snow
melt runoff was positively correlated with average air temperatures [increases] throughout the winter, but correlations don't always necessarily mean that one thing causes another,» Dudley told LiveScience.
I believe India, Pakistan, Kashmir, Nepal, China will feel the full effect of lost glacier
melt runoff that feeds major rivers in their part of the world and provide irrigation and drinking water for tens of millions of people.
Freshwater flux from Greenland is composed of
melt runoff from ice and tundra runoff as well as ice discharge («calving» of icebergs).
Black ice on roads, which takes on the color of the pavement below it, forms when precipitation freezes on impact or
melted runoff refreezes.
Not exact matches
The study suggests that up until 1997, whenever the ice caps and glaciers
melted, the
runoff would be filtered through a layer of older snow called the «firn» and trickle down to the ice surface, where it would freeze again, allowing the glaciers and ice caps to grow each winter.
To catch the
runoff from the
melted snow, residents had wisely built a damn, but it was inefficient, providing water for only a few dozen families, and stirring up strife between neighbors desperate for its live - saving waters.
They also used a physically based computer model of the hydrologic cycle, which takes daily weather observations and computes the snow accumulation,
melting, and
runoff to estimate the total snowpack in the western U.S.
Additionally, as the state's snowpack
melts earlier because of warming, Cayan said, there is more
runoff from higher elevation, which increases flooding.
A shorter period covered by snow, more spring rain and faster snow
melt can combine to release large amounts of
runoff that have the potential to stress urban hydrologic systems and cause flooding in urban areas.»
Precipitation was very important in the summer and the winter, when rains and
melting snow boosted
runoff and delivered nitrogen and phosphorus, which algae use as food sources, to the lake.
They knew the fire had been accidental, yet they found classic signs of arson: large, shiny blisters on wood resembling alligator skin, chipping concrete, and
melted metal doorway thresholds, all typically attributed to accelerant and accelerant
runoff, resulting in excessively high heat.
The discovery of widespread
melting came after hydrologist Åsa K. Rennermalm of Rutgers University, New Jersey, noticed that stream
runoffs at her field site in west Greenland were unusually heavy.
Northwest Greenland experienced record
melt, setting summer records for surface temperatures, production of meltwater, and total
runoff.
The lakes receive a large amount of
runoff in the spring from the
melting snowpack.
It is also likely to affect the ability to control floods, as snowpack that
melts earlier in the year increases downhill
runoff.
And «ponding» is also a risk with this type of roof design, which can occur when snow is heated to
melt off but
runoff backs up rather than flows and eventually causes elastic fabric to stretch and tear.
Melt water
runoff from a
melting of the Greenland Ice Sheet is a potentially major source of freshening not yet included in the models found in the MMD (see Section 8.7.2.2).
The thickness of the remaining, multi-year ice, along with its geographic location, will make it more difficult to
melt than the ice that was spread across the Arctic, and exposed to Pacific and Atlantic ocean currents, along with
runoff from fresh water rivers.
The hike through the valley leads you over rocks, streams, and rivers created by the
runoff of snow and the
melting of ice from both the Hooker Glacier and those glaciers hanging off Mount Sefton.
Which leads me to another question — the
melting glacial / Greenland / Antarctic ice water is depleted in CO2 (check out the bubbles in your ice cubes)-- how much additional CO2 is being sequestered by this
runoff into the oceans, and what happens to CO2 increase when we run out of glaciers?
This is enough energy to
melt approximately 7.5 gm of ice, which when added to the condensate yields a total of 8.5 gm of potential
runoff».
Pacific water, ice -
melt, precipitation and river
runoff are distinct sources of freshwater to the Canada Basin.
Ice
melt, precipitation and
runoff are all increasing under the current climatic trends31, 37, and are altering the freshwater budget of the Arctic Ocean.
Runoff from steep ice - cliffs, or through subglacial flow driven by water percolating through pores or fractures, will convert a high fraction of
melting into ablation.
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).
There are some large rivers dumping into the artic from Siberia, and Siberia has been very cold this winter, so the river
runoff is less likely to
melt the ice.
It is reasonable to assume that the freshwater input will continue to increase in the future because the earth is warming, causing increasing ice
melt and increased precipitation (both over ocean and over land, which yields larger river
runoff to the ocean).
What's been published correlating summer and winter Siberian temperature with river
runoff temperature and the following seasons» Arctic ice
melt?
From recent research, I would suggest that this is entirely plausible; I could cite several examples of substantial increases (
runoff, glacier
melt, precipitation, sea - ice loss) which, collectively, amount to a real net increase in the Arctic freshwater budget.
Finally, if the North American hydrologic cycle is enhanced, and / or Greenland's southern ice caps
melt, the increased fresh water
runoff from land areas could dilute the ocean surface water and critically reduce its salinity.
As
runoff from
melting glaciers increases and warming seawater expands, sea level could rise as much as six feet, inundating low - lying coastal areas and islands.
With the model you can:... Analyse changes to river flow,
runoff, soil moisture, groundwater recharge, snow
melt, frost days and irrigation demand Simulate the impacts anywhere in the world Output the results in a range of graphic formats....»
Runoff from the
melting of ice sheets (Section 10.3.3) is not included here.
But there are risks that the snowpack could
melt faster than the reservoirs can handle the
runoff.
During the rainy season or the season of
melting snow, any groundwater contribution is masked by heavy surface
runoff and shallow aquifer effects.
Also the site does inform that the graphs are calculated and may have flaws, they do not account for snow
melt or
runoff.
Because a large share of the
runoff in the glacial water systems comes from
melting, most of this
runoff, up to 80 %, takes place in the summer.
Alpine
runoff throughout the Pacific Northwest is increasing in the winter (Nov. - March), as more frequent rain on snow events enhance
melting and reduce snow storage.
As glacier area is lost there will be a long term decline in glacier
runoff and alpine streamflow during the
melt season.
Eventually the resulting decline in glacier extent reduces the area available for
melting causing a decrease in glacier
runoff.
Unlike non-glacier
runoff, glacier
runoff correlates better with temperature than precipitation, due to the dominant role of glacier
melt compared to precipitation in summer
runoff from glacierized basins.
The initial response is an increase in glacier
melt rate enhancing glacier
runoff, while the glacier extent is still substantial in comparison to previous size.
There are two changes in glacier
runoff that occur as a result of warming and enhanced glacier
melt.
A continuing trend in glacier loss will seriously decrease the water reserves stored as ice, reducing
melt season
runoff.
The forecast thus is given at the start of the
melt season and provides an assessment of the amount of glacier
runoff that will be generated.
However, a large majority of streams in glaciated basins in BC showed a statistically significant decrease in August streamflow during 1976 to 1996, which suggests that these glaciers even with increased
melt rates are providing less
runoff (Stahl and Moore, 2006).
The combination of snow
melt, glacial
melt and rainfall water sources provides for reliable
runoff in these basins.
Upcoming rains will bolster spring
runoff (but probably also
melt quite a bit of snowpack; see below).
Covering an area of 30,000 km2 and 48 % of BC's gauged systems glacier -
melt moderates inter-annual variability in streamflow and helps to maintain higher
runoff volume in times of extreme warm and dry conditions.
This loss in
melt extent is reducing glacier
runoff and summer alpine streamflow.