Empirical estimation of present-day Antarctic glacial isostatic adjustment and ice mass change
This study explores an approach that simultaneously estimates Antarctic mass balance and
glacial isostatic adjustment (GIA) through the combination of satellite gravity and altimetry …
glacial isostatic adjustment (GIA) through the combination of satellite gravity and altimetry …
Large ensemble modeling of the last deglacial retreat of the West Antarctic Ice Sheet: comparison of simple and advanced statistical techniques
A 3-D hybrid ice-sheet model is applied to the last deglacial retreat of the West Antarctic Ice
Sheet over the last∼ 20 000 yr. A large ensemble of 625 model runs is used to calibrate the …
Sheet over the last∼ 20 000 yr. A large ensemble of 625 model runs is used to calibrate the …
High‐spatial‐resolution mass rates from GRACE and GRACE‐FO: Global and ice sheet analyses
BD Loomis, D Felikson, TJ Sabaka… - Journal of Geophysical …, 2021 - Wiley Online Library
Abstract GRACE and GRACE‐FO gravimetry data are unique in its ability to observe global
water mass variability and has frequently been applied for the determination of global mass …
water mass variability and has frequently been applied for the determination of global mass …
Existing and potential evidence for Holocene grounding-line retreat and readvance in Antarctica
Widespread existing geological records from above the modern ice-sheet surface and
outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more …
outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more …
[HTML][HTML] A coupled ice sheet–sea level model incorporating 3D Earth structure: variations in Antarctica during the last deglacial retreat
N Gomez, K Latychev, D Pollard - Journal of Climate, 2018 - journals.ametsoc.org
A Coupled Ice Sheet–Sea Level Model Incorporating 3D Earth Structure: Variations in
Antarctica during the Last Deglacial Retreat in: Journal of Climate Volume 31 Issue 10 (2018) …
Antarctica during the Last Deglacial Retreat in: Journal of Climate Volume 31 Issue 10 (2018) …
Closing the sea level budget on a regional scale: Trends and variability on the Northwestern European continental shelf
Long‐term trends and decadal variability of sea level in the North Sea and along the
Norwegian coast have been studied over the period 1958–2014. We model the spatially …
Norwegian coast have been studied over the period 1958–2014. We model the spatially …
Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks
Marine ice-cliff instability (MICI) processes could accelerate future retreat of the Antarctic Ice
Sheet if ice shelves that buttress grounding lines more than 800 metres below sea level are …
Sheet if ice shelves that buttress grounding lines more than 800 metres below sea level are …
Frequency dependent mantle viscoelasticity via the complex viscosity: Cases from Antarctica
Studies of glacial isostatic adjustment (GIA) often use paleoshorelines and present‐day
deformation to constrain the viscosity of the mantle and the thickness of the elastic …
deformation to constrain the viscosity of the mantle and the thickness of the elastic …
Seismic evidence for lithospheric foundering beneath the southern Transantarctic Mountains, Antarctica
Abstract The 3000-km-long Transantarctic Mountains (TAMs), which separate cratonic East
Antarctica from tectonically active West Antarctica, remain one of the least understood of …
Antarctica from tectonically active West Antarctica, remain one of the least understood of …
[HTML][HTML] Abrupt Holocene ice-sheet thinning along the southern Soya Coast, Lützow-Holm Bay, East Antarctica, revealed by glacial geomorphology and surface …
M Kawamata, Y Suganuma, K Doi, K Misawa… - Quaternary Science …, 2020 - Elsevier
Geological reconstruction of the retreat history of the East Antarctic Ice Sheet (EAIS) since
the Last Glacial Maximum (LGM) is essential for understanding the response of the ice sheet …
the Last Glacial Maximum (LGM) is essential for understanding the response of the ice sheet …