Sea-level rise due to polar ice-sheet mass loss during past warm periods
BACKGROUND Although thermal expansion of seawater and melting of mountain glaciers
have dominated global mean sea level (GMSL) rise over the last century, mass loss from the …
have dominated global mean sea level (GMSL) rise over the last century, mass loss from the …
Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions
PL Whitehouse - Earth surface dynamics, 2018 - esurf.copernicus.org
Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
K Lambeck, H Rouby, A Purcell… - Proceedings of the …, 2014 - National Acad Sciences
The major cause of sea-level change during ice ages is the exchange of water between ice
and ocean and the planet's dynamic response to the changing surface load. Inversion of∼ …
and ocean and the planet's dynamic response to the changing surface load. Inversion of∼ …
Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model
WR Peltier, DF Argus… - Journal of Geophysical …, 2015 - Wiley Online Library
A new model of the last deglaciation event of the Late Quaternary ice age is here described
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level …
DF Argus, WR Peltier, R Drummond… - Geophysical Journal …, 2014 - academic.oup.com
ABSTRACT A new model of the deglaciation history of Antarctica over the past 25 kyr has
been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its …
been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its …
Rapid glaciation and a two-step sea level plunge into the Last Glacial Maximum
Abstract The approximately 10,000-year-long Last Glacial Maximum, before the termination
of the last ice age, was the coldest period in Earth's recent climate history. Relative to the …
of the last ice age, was the coldest period in Earth's recent climate history. Relative to the …
[HTML][HTML] Inception of a global atlas of sea levels since the Last Glacial Maximum
Determining the rates, mechanisms, and geographic variability of relative sea-level (RSL)
change following the Last Glacial Maximum (LGM) provides insight into the sensitivity of ice …
change following the Last Glacial Maximum (LGM) provides insight into the sensitivity of ice …
A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
The sensitivity of the Antarctic ice sheet to a changing climate: Past, present, and future
Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent
BS Lecavalier, GA Milne, MJR Simpson, L Wake… - Quaternary Science …, 2014 - Elsevier
An ice sheet model was constrained to reconstruct the evolution of the Greenland Ice Sheet
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …