Classification of calving fronts around Antarctica [PDF]
Iceberg calving is the largest loss term in Antarctic mass balance. The iceberg areas vary from a few square meters (growler) to several hundred square kilometres (huge tabular icebergs or ice islands) and their shape (blocky, domed or tabular) depends ...
Wesche, Christine
core
Episodes of Early Pleistocene West Antarctic Ice Sheet Retreat Recorded by Iceberg Alley Sediments. [PDF]
Bailey I +32 more
europepmc +1 more source
Evolution of the East Antarctic Ice Sheet: A Numerical Study of Thermo-Mechanical Response Patterns With Changing Climate [PDF]
Philippe Huybrechts, J. Oerlemans
openalex +1 more source
Tracing Particle Paths in the Antarctic Ice Sheet [PDF]
C. S. M. Doake
openalex +1 more source
Estimating Antarctic climate variability of the last millennium [PDF]
Climate variability is determined by the climate system’s internal variability as well as its response to external forcing. A quantitative understanding of past Antarctic climate variability is therefore essential if we are to attribute and to detect ...
Laepple, Thomas, Münch, Thomas
core
West Antarctic ice sheet dynamics
Mercer [1978] pointed out that a climatic warming, caused, for instance, by an increasing atmospheric CO2 concentration, may lead to a very rapid deglaciation (within a few hundred years) of the West Antarctic Ice Sheet, resulting in a sea level rise of about 5 m.
openaire +2 more sources
A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
J. Marschalek +64 more
semanticscholar +1 more source
Environmental Constraints on West Antarctic Ice-Sheet Formation [PDF]
Dean R. Lindstrom, Douglas R. MacAyeal
openalex +1 more source
Responces of melting below Antarctic ice shelf to climate [PDF]
The Antarctic Ice Sheet is buttressed by floating ice shelves. Calving at ice shelf front and basal melting below ice shelf are main ablation processes of Antarctic ice sheet(Rignot et al., 2013).
小長谷 貴志 +3 more
core +1 more source
Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet
Mathieu Morlighem +36 more
semanticscholar +1 more source

