Large pools of melt water splotching the ice shelf probably forced
open cracks in the ice.
Not exact matches
The Russian and American scientists have never before experienced anything of such magnitude, and
in addition to powerful emissions from shallow waters where over 100 readings were recorded, it is spewing up from within
cracks in the Arctic
ice in the
open seas far from land.
As this water moves through rocks, it dissolves salt compounds and pushes through fractures
in the overlying
ice to form reservoirs closer the moon's surface, where it is expelled into space when the outermost layer of the crust
cracks open and the resulting depressurization of these reservoirs causes water vapor and
ice particles to shoot out
in the observed plumes.
I assume every glacier is different, so there's no single answer whether meltwater is successfully penetrating through
cracks to the base and staying melted, and whether stresses
in the
ice are
opening cracks further, and which glaciers have beds sloping downhill going inland
Surface meltwater can penetrate through
cracks in the surface, and force them
open, allowing large amounts of water to drain to the bed and spread out across the base of the
ice sheet, lubricating it (Zwally et al. 2002).
But
in recent years, the
ice has more often been internally fissured and riven with enormous «leads» — areas of
open water that can form as the
ice pack shifts and
cracks — or melts.
This would be fundamentally different from events
in the past where a
crack in the
ice might temporarily expose some
open water at the pole
in the midst of surrounding
ice.
Or the news from Antarctica this past May, when a
crack in an
ice shelf grew 11 miles
in six days, then kept going; the break now has just three miles to go — by the time you read this, it may already have met the
open water, where it will drop into the sea one of the biggest icebergs ever, a process known poetically as «calving.»
As you can see, the sea
ice in the Arctic has many holes and
cracks in it, and lots of
open water around it.