Pollard, D., Deconto, R. M. & Alley, R. B. Potential Antarctic
Ice Sheet retreat driven by hydrofracturing and ice cliff failure.
«Potential Antarctic
Ice Sheet Retreat Driven by Hydrofracturing and Ice Cliff Failure.»
Not exact matches
We determine that this difference is
driven by the growth and
retreat of large continental
ice sheets that are present in the cold
ice - age climates; these
ice sheets reflect a lot of sunlight and their growth consequently amplifies the impact of CO2 changes.»
Ice sheets begin to
retreat from their maximum extent due to the increase in sunlight
driven by the overall orbital variations.
Black carbon disrupts the South Asian monsoon (by altering the land - sea temperature gradient that
drives the movement of moist air), helps melt the Greenland
ice sheet (by increasing the solar energy the darkened
ice absorbs), and accelerates the
retreat of Himalayan glaciers.
Carlson, A.E., F.S. Anslow, E.A. Obbink, A.N. LeGrande, D.J. Ullman, and J.M Licciardi (2009) Surface - melt
driven Laurentide
Ice Sheet retreat during the early Holocene.
Early Holocene summer warmth
drove dramatic Greenland
ice sheet (GIS)
retreat.