A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment
about
Ice-sheet mass balance and climate changeFrom warm to cold: migration of Adélie penguins within Cape Bird, Ross Island.Sea-level constraints on the amplitude and source distribution of Meltwater Pulse 1AAbrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise.Lower satellite-gravimetry estimates of Antarctic sea-level contribution.Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.Centennial-scale Holocene climate variations amplified by Antarctic Ice Sheet discharge.An assessment of forward and inverse GIA solutions for Antarctica.Mid-Holocene pulse of thinning in the Weddell Sea sector of the West Antarctic ice sheet.Past penguin colony responses to explosive volcanism on the Antarctic Peninsula.Gradual demise of a thin southern Laurentide ice sheet recorded by Mississippi drainage.A geomorphological seabed classification for the Weddell Sea, AntarcticaCoral reefsHolocene Relative Sea-Level Changes from Near-, Intermediate-, and Far-Field LocationsUplift rates from a new high-density GPS network in Palmer Land indicate significant late Holocene ice loss in the southwestern Weddell SeaAntarctic contribution to sea level rise observed by GRACE with improved GIA correctionGlacial isostatic adjustment in response to changing Late Holocene behaviour of ice streams on the Siple Coast, West AntarcticaIncreased ice loading in the Antarctic Peninsula since the 1850s and its effect on glacial isostatic adjustmentA mascon approach to assess ice sheet and glacier mass balances and their uncertainties from GRACE dataControls on Last Glacial Maximum ice extent in the Weddell Sea embayment, AntarcticaA new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea-level change and present-day uplift ratesThe Deformational Response of a Viscoelastic Solid Earth Model Coupled to a Thermomechanical Ice Sheet ModelGreenland and Antarctica Ice Sheet Mass Changes and Effects on Global Sea LevelIncomplete separability of Antarctic plate rotation from glacial isostatic adjustment deformation within geodetic observationsCollapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation
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P2860
A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment
description
article
@en
im Jahr 2012 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2012
@uk
name
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@en
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@nl
type
label
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@en
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@nl
prefLabel
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@en
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@nl
P1476
A deglacial model for Antarcti ...... c glacial isostatic adjustment
@en
P2093
Michael J. Bentley
Pippa L. Whitehouse
P356
10.1016/J.QUASCIREV.2011.11.016
P577
2012-01-01T00:00:00Z