But scientists increasingly attribute much of
the observed grounding line retreat — particularly in West Antarctica — to the influence of warmer ocean water seeping beneath the ice shelves and lapping against the bases of glaciers, melting the ice from the bottom up.
But scientists increasingly attribute much of
the observed grounding line retreat — particularly in West Antarctica — to the influence of warmer ocean water seeping beneath the ice shelves and lapping against the bases of glaciers, melting the ice from the bottom up.
Not exact matches
By combining observations from the
ground and in space, the team
observed a plume of low - energy plasma particles that essentially hitches a ride along magnetic field
lines — streaming from Earth's lower atmosphere up to the point, tens of thousands of kilometers above the surface, where the planet's magnetic field connects with that of the sun.
For now, the findings can't tell scientists exactly how much sea - level rise is corresponding with the
observed changes, although a net retreat of the
grounding line suggests that there's more reason for worry than not.
A major, previously unknown subglacial lake near the
grounding line of Whillans Ice Stream is
observed to drain 2.0 km3 of water over ~ 3 years, while elsewhere a similar volume of water is being stored subglacially.
This melts the ice shelf from below24, and this melting is probably the cause of the
observed ice stream thinning, acceleration and
grounding line recession25, which is contributing to a sea level rise of 1.2 mm per decade3.
The
observed acceleration, retreat of the
grounding line, thinning of the lower section of the glacier and the
observed elevation of the basal topography provide no indication that this is not a weak underbelly of WAIS.
For now, the findings can't tell scientists exactly how much sea - level rise is corresponding with the
observed changes, although a net retreat of the
grounding line suggests that there's more reason for worry than not.
A major, previously unknown subglacial lake near the
grounding line of Whillans Ice Stream is
observed to drain 2.0 km3 of water over ~ 3 years, while elsewhere a similar volume of water is being stored subglacially.