Results 91 to 100 of about 3,714 (183)
Antarctic last interglacial isotope peak in response to sea ice retreat not ice-sheet collapse
The peak in Antarctic ice core isotope values, 128,000 years before present, was concurrent with a significantly warmer-than-present Antarctic climate.
Max D. Holloway +5 more
doaj +1 more source
Changes in ice dynamics and mass balance of the Antarctic ice sheet [PDF]
The concept that the Antarctic ice sheet changes with eternal slowness has been challenged by recent observations from satellites. Pronounced regional warming in the Antarctic Peninsula triggered ice shelf collapse, which led to a 10-fold increase in glacier flow and rapid ice sheet retreat.
openaire +4 more sources
Does Polar Warming Asymmetry Exist in Bathy‐Planet Experiments?
Abstract Ocean bathymetry and continental geometry shape ocean circulation, but whether these geographic constraints can sustain polar warming asymmetry in a fully coupled climate system remains unclear. Here we construct a fully coupled “bathy‐planet” configuration (BATHY), in which continental topography is removed and most land surfaces are replaced
Yihan Zhang +4 more
wiley +1 more source
The Source of Arctic Precipitation in HadGEM3‐GC5
Abstract Snow and rain are increasing in the Arctic. Climate model projections indicate a 50% increase in precipitation by the end of the century. This increase is driven by increased local evaporation following reduced sea ice coverage alongside enhanced global evaporation and transport into the Arctic.
J. K. Ridley +3 more
wiley +1 more source
An improved retrieval method for liquid water content of the Antarctic ice sheet using SMOS data
With global climate warming, Antarctic ice sheet melting has garnered increasing attention, as changes in liquid water content (LWC) significantly affect sea level rise and regional climate.
Yi Zhou +8 more
doaj +1 more source
We conducted GPS observations on the Antarctic ice sheet in the vicinity of Syowa Station, during wintering of the 48th Japanese Antarctic Research Expedition (JARE-48). Continuous GPS data for about one year was obtained for the first time.
Naoki Arai +3 more
doaj +1 more source
Approximating ice sheet – bedrock interaction in Antarctic ice sheet projections
Abstract. The bedrock response to a melting ice sheet provides a negative feedback on ice mass loss. When modelling the future behaviour of the Antarctic Ice Sheet, accounting for the impact of bed deformation on ice dynamics can reduce predictions of future sea level rise by up to 40 % in comparison with scenarios that assume a rigid Earth.
Caroline Jacoba van Calcar +3 more
openaire +1 more source
An ancient river landscape preserved beneath the East Antarctic Ice Sheet. [PDF]
Jamieson SSR +8 more
europepmc +1 more source
Millennial-scale variability of the Antarctic ice sheet during the early Miocene. [PDF]
Sullivan NB +5 more
europepmc +1 more source
Constraining the contribution of the Antarctic Ice Sheet to Last Interglacial sea level. [PDF]
Barnett RL +7 more
europepmc +1 more source

