scholarly article | Q13442814 |
P819 | ADS bibcode | 2019NatCo..10..503W |
P6179 | Dimensions Publication ID | 1111769349 |
P356 | DOI | 10.1038/S41467-018-08068-Y |
P2888 | exact match | https://scigraph.springernature.com/pub.10.1038/s41467-018-08068-y |
P932 | PMC publication ID | 6353952 |
P698 | PubMed publication ID | 30700704 |
P50 | author | Natalya Gomez | Q69843968 |
Douglas A Wiens | Q89181175 | ||
Matt A. King | Q55908221 | ||
Pippa L. Whitehouse | Q56990187 | ||
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Sea-level feedback lowers projections of future Antarctic Ice-Sheet mass loss | Q33663006 | ||
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Extensive retreat and re-advance of the West Antarctic Ice Sheet during the Holocene | Q56340212 | ||
Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions | Q56362297 | ||
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Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability | Q56961783 | ||
A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum | Q57081685 | ||
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Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum | Q57083938 | ||
On the Rebound: Modeling Earth's Ever-Changing Shape | Q57140107 | ||
Stability of the Junction of an Ice Sheet and an Ice Shelf | Q57258706 | ||
Glacial isostatic adjustment model with composite 3-D Earth rheology for Fennoscandia | Q57507555 | ||
The role of thermal effect on mantle seismic anomalies under Laurentia and Fennoscandia from observations of Glacial Isostatic Adjustment | Q57507580 | ||
Glacial isostatic adjustment in Fennoscandia—A review of data and modeling | Q57507616 | ||
Lateral viscosity variations beneath Antarctica and their implications on regional rebound motions and seismotectonics | Q57507818 | ||
Large ensemble modeling of the last deglacial retreat of the West Antarctic Ice Sheet: comparison of simple and advanced statistical techniques | Q57894940 | ||
A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment | Q57941157 | ||
Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet | Q57941184 | ||
Uplift rates from a new high-density GPS network in Palmer Land indicate significant late Holocene ice loss in the southwestern Weddell Sea | Q57950288 | ||
Empirical estimation of present-day Antarctic glacial isostatic adjustment and ice mass change | Q58055793 | ||
Antarctic contribution to sea level rise observed by GRACE with improved GIA correction | Q58072324 | ||
Antarctic ice rises and rumples: Their properties and significance for ice-sheet dynamics and evolution | Q58073646 | ||
Low post-glacial rebound rates in the Weddell Sea due to Late Holocene ice-sheet readvance | Q58073655 | ||
Late Holocene ice-flow reconfiguration in the Weddell Sea sector of West Antarctica | Q58073673 | ||
A model computation of the temporal changes of surface gravity and geoidal signal induced by the evolving Greenland ice sheet | Q58076665 | ||
Glacial isostatic adjustment in response to changing Late Holocene behaviour of ice streams on the Siple Coast, West Antarctica | Q58080605 | ||
Deglacial history of the West Antarctic Ice Sheet in the Weddell Sea embayment: Constraints on past ice volume change | Q58081905 | ||
Deglacial history of the West Antarctic Ice Sheet in the Weddell Sea embayment: Constraints on past ice volume change: COMMENT | Q58082053 | ||
The impact of dynamic topography change on Antarctic ice sheet stability during the mid-Pliocene warm period | Q58083326 | ||
Future Antarctic bed topography and its implications for ice sheet dynamics | Q58085705 | ||
Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica | Q58110019 | ||
Sea Level Fingerprints in a Region of Complex Earth Structure: The Case of WAIS | Q58117677 | ||
Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions | Q58120287 | ||
Rapid ice unloading in the Fleming Glacier region, southern Antarctic Peninsula, and its effect on bedrock uplift rates | Q58120297 | ||
Rapid bedrock uplift in the Antarctic Peninsula explained by viscoelastic response to recent ice unloading | Q58120327 | ||
A new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea-level change and present-day uplift rates | Q58120342 | ||
Observations beneath Pine Island Glacier in West Antarctica and implications for its retreat | Q58241320 | ||
Evidence for the impact of aerosols on the onset and microphysical properties of rainfall from a combination of satellite observations and cloud-resolving model simulations | Q58244347 | ||
Emplacement of Antarctic ice sheet mass affects circumpolar ocean flow | Q58305457 | ||
The Deformational Response of a Viscoelastic Solid Earth Model Coupled to a Thermomechanical Ice Sheet Model | Q58315970 | ||
The use of GPS horizontals for loading studies, with applications to northern California and southeast Greenland | Q58380485 | ||
Bedrock Erosion Surfaces Record Former East Antarctic Ice Sheet Extent | Q58385925 | ||
The glacial geomorphology of the Antarctic ice sheet bed | Q58385955 | ||
Incomplete separability of Antarctic plate rotation from glacial isostatic adjustment deformation within geodetic observations | Q58392532 | ||
Ongoing deformation of Antarctica following recent Great Earthquakes | Q58392535 | ||
A benchmark study for glacial isostatic adjustment codes | Q58392585 | ||
Reply to Comment by W. R. Peltier, D. F. Argus, and R. Drummond on “An Assessment of the ICE6G_C (VM5a) Glacial Isostatic Adjustment Model” | Q58394569 | ||
An assessment of theICE6G_C(VM5a)glacial isostatic adjustment model | Q58394575 | ||
Antarctic glacial isostatic adjustment: a new assessment | Q58402097 | ||
Relative sea-level rise around East Antarctica during Oligocene glaciation | Q58413669 | ||
Isostatic rebound due to glacial erosion within the Transantarctic Mountains | Q58458077 | ||
The Crust and Upper Mantle Structure of Central and West Antarctica From Bayesian Inversion of Rayleigh Wave and Receiver Functions | Q59122218 | ||
West Antarctic paleotopography estimated at the Eocene-Oligocene climate transition | Q59758809 | ||
Initiation of the West Antarctic Ice Sheet and estimates of total Antarctic ice volume in the earliest Oligocene | Q59758811 | ||
Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations | Q59805547 | ||
Topographic controls on post-Oligocene changes in ice-sheet dynamics, Prydz Bay region, East Antarctica | Q59854224 | ||
Seismological imaging of the Antarctic continental lithosphere: a review | Q60702755 | ||
Linear or non-linear rheology in the Earth's mantle: the prevalence of power-law creep in the postglacial isostatic readjustment of Laurentia | Q60713061 | ||
On transient rheology and glacial isostasy | Q60715365 | ||
Flow-switching and water piracy between Rutford Ice Stream and Carlson Inlet, West Antarctica | Q61077588 | ||
1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica | Q61078680 | ||
Modeling the evolution of Antarctic ice sheet over the last 420,000 years: Implications for altitude changes in the Vostok region | Q61078743 | ||
The impact of lateral variations in lithospheric thickness on glacial isostatic adjustment in West Antarctica | Q61307693 | ||
Coseismic slip distribution of the 1923 Kanto earthquake, Japan | Q61469770 | ||
P275 | copyright license | Creative Commons Attribution 4.0 International | Q20007257 |
P6216 | copyright status | copyrighted | Q50423863 |
P433 | issue | 1 | |
P407 | language of work or name | English | Q1860 |
P304 | page(s) | 503 | |
P577 | publication date | 2019-01-30 | |
P1433 | published in | Nature Communications | Q573880 |
P1476 | title | Solid Earth change and the evolution of the Antarctic Ice Sheet | |
P478 | volume | 10 |
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