Not exact matches
They found that western Antarctica has recently seen
warmer, saltier
water being driven
under the shelf — the part of the ice
sheet that sticks out over the ocean (Science, doi.org/xkx).
A new study led by the University of Texas Institute for Geophysics has found that wind over the ocean off the coast of East Antarctica causes
warm, deep
waters to upwell, circulate
under Totten Ice Shelf, and melt the fringes of the East Antarctic ice
sheet from below.
While the
water under the Antarctic ice is not itself related to global
warming, the suprisingly large amount of
water, the surprising speed with which it moves, and its effect of «lubricating» the movement of the Antarctic ice, may affect how the ice
sheets respond to
warming.
Rinse olives
under warm water and drain on a paper towel — lined baking
sheet.
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-?)
Warm ocean
water plays a significant role in melting glacial ice from below, and a better mapping of Antarctica's and Greenland's landforms beneath the ice suggests that ocean melting of the glacier fronts may play a more significant role than previously thought as the ice
sheets retreat (
under a global
warming scenario).
The rise was caused partly by the simple thermal expansion of sea
water under the influence of global
warming, and increasingly by the melting of glaciers and ice
sheets.
From a combination of climate models, satellite data, and paleoclimate records the scientists conclude that the West Antarctic ice
sheet, Arctic ice cover, and regions providing fresh
water sources and species habitat are
under threat from continued global
warming.