Not exact matches
As
melting ice from these
glaciers formed streams and rivers along the
edge of the
glaciers, thick sequences
of sand and gravels were deposited.
The study shows that it's plausible, even if Mars was generally frozen over, that peak daily temperatures in summer might sneak above freezing just enough to cause
melting at the
edges of glaciers.
Himalayan
glaciers are
melting and retreating at their
edges because
of global warming.
Ice shelves (the floating front
edges of glaciers that extend tens to hundreds
of miles offshore)
melt more because
of contact with ocean water below them than they do because
of sunlight.
Now dirt and material will migrate to the top
of a
glacier as it is
melting back / receding and the
edges can even become black.
In March, Oceans
Melting Greenland (OMG) will conduct its second set
of airborne surveys
of glacier heights around the
edge of Greenland and coastal ocean conditions.
Other factors would include: — albedo shifts (both from ice > water, and from increased biological activity, and from
edge melt revealing more land, and from more old dust coming to the surface...); — direct effect
of CO2 on ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; —
melting of sea ice shelf increasing mobility
of glaciers; — sea water getting under parts
of the ice sheets where the base is below sea level; —
melt water lubricating the ice sheet base; — changes in ocean currents -LRB-?)
The
edge of the Thwaites
glacier [credit: NASA photograph by Jim Yungel] This BBC report seems unaware that a study in 2014 found that parts
of the Thwaites
Glacier are subject to
melting due to subglacial volcanoes and other geothermal «hotspots».
Now that the
glaciers have
melted, the land beneath where they were located is now rising, while the land at where the
edges of the
glaciers were located is sinking, i.e., subsiding.