Results 31 to 40 of about 3,714 (183)

ANTARCTIC ICE SHEET SLOPE AND ASPECT BASED ON ICESAT’S REPEAT ORBIT MEASUREMENT [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2017
Accurate information of ice sheet surface slope is essential for estimating elevation change by satellite altimetry measurement. A study is carried out to recover surface slope of Antarctic ice sheet from Ice, Cloud and land Elevation Satellite (ICESat)
L. Yuan   +13 more
doaj   +1 more source

Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS

open access: yesContributions to Geophysics and Geodesy, 2019
In this study, we estimate the ice mass changes, the ice elevation changes and the vertical displacements in Antarctica based on analysis of multi-geodetic datasets that involve the satellite gravimetry (GRACE), the satellite altimetry (ICESat) and the ...
Fang ZOU   +2 more
doaj   +1 more source

The Dynamics of the Antarctic Ice Sheet [PDF]

open access: yesAnnals of Glaciology, 1989
A three-dimensional dynamic, thermodynamic ice-sheet model has been developed to simulate the past, present, and future behaviour of the Antarctic ice sheet. The present ice velocities depend on the deep ice temperatures which in turn depend on the past changes of the ice sheet, including surface temperature, accumulation rate, and ice thickness.
W.F. Budd, D. Jenssen
openaire   +1 more source

Modelling the evolution of the Antarctic ice sheet since the last interglacial [PDF]

open access: yesThe Cryosphere, 2014
We present the effects of changing two sliding parameters, a deformational velocity parameter and two bedrock deflection parameters on the evolution of the Antarctic ice sheet over the period from the last interglacial until the present.
M. N. A. Maris   +5 more
doaj   +1 more source

Changes in the Antarctic’s Summer Surface Albedo, Observed by Satellite since 1982 and Associated with Sea Ice Anomalies

open access: yesRemote Sensing, 2023
In polar regions, positive feedback of snow and ice albedo can intensify global warming. While recent significant decreases in Arctic surface ice albedo have drawn considerable attention, Antarctic surface albedo variability remains underexplored.
Yuqi Sun   +3 more
doaj   +1 more source

Remote Sensing of Antarctic Glacier and Ice-Shelf Front Dynamics—A Review

open access: yesRemote Sensing, 2018
The contribution of Antarctica’s ice sheet to global sea-level rise depends on the very dynamic behavior of glaciers and ice shelves. One important parameter of ice-sheet dynamics is the location of glacier and ice-shelf fronts.
Celia A. Baumhoer   +3 more
doaj   +1 more source

Did the West Antarctic Ice Sheet Create the East Antarctic Ice Sheet? [PDF]

open access: yesAnnals of Glaciology, 1982
The mostly terrestrial East Antarctic ice sheet is ten times larger and probably more stable than the mostly marine West Antarctic ice sheet. It is natural to suppose that the former appeared first, and that perhaps the latter was partially formed from an outflow of East Antarctic ice onto the West Antarctic continental shelf.
openaire   +1 more source

Physical processes and feedbacks obscuring the future of the Antarctic Ice Sheet

open access: yesGeosystems and Geoenvironment, 2022
The Antarctic Ice Sheet holds a vital role in Earth's climate system and its changes have global implications for the climate, sea level, coastal ecosystems and population.
Dawei Li
doaj   +1 more source

Modeling the Antarctic ice sheet [PDF]

open access: yesAnnals of Glaciology, 1997
A three-dimensional (3-D), high-resolution, non-linearly viscous, non-isothermal ice-sheet model is employed to calculate the “present-day” equilibrium regime of the Antarctic ice sheet and its evolution during the last glacial cycle.
Mikhail Verbitsky, Barry Saltzman
openaire   +1 more source

West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data

open access: yesFrontiers in Earth Science, 2022
Observations of rapid ongoing grounding line retreat, ice shelf thinning and accelerated ice flow from the West Antarctic Ice Sheet (WAIS) may forebode a possible collapse if global temperatures continue to increase. Understanding and reconstructing West
Johanna Gille-Petzoldt   +30 more
doaj   +1 more source

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