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[PDF] Top 20 Coupled models of glacial isostasy and ice sheet dynamics

Has 10000 "Coupled models of glacial isostasy and ice sheet dynamics" found on our website. Below are the top 20 most common "Coupled models of glacial isostasy and ice sheet dynamics".

Coupled models of glacial isostasy and ice sheet dynamics

Coupled models of glacial isostasy and ice sheet dynamics

... It is also important to note that the ice sheet deglaciation chronologies generated in Chapters 5 and 6 by the Jenssen model are glaciologically realistic as well as producing an improve[r] ... See full document

197

Coupled Northern Hemisphere permafrost–ice-sheet evolution over the last glacial cycle

Coupled Northern Hemisphere permafrost–ice-sheet evolution over the last glacial cycle

... The main limitation for long-term permafrost evolution evaluation is the lack of coupled models including a per- mafrost component that are capable of performing multi- millennial transient simulations. All ... See full document

16

Assessing the impact of Laurentide Ice Sheet topography on glacial climate

Assessing the impact of Laurentide Ice Sheet topography on glacial climate

... fully coupled AOGCM results build upon earlier lower-resolution simulations that indicate a similar dynamical adjustment with the comparison of ICE-4G and ICE-5G LIS reconstructions in an Earth sys- ... See full document

21

Interaction between ice sheet dynamics and subglacial lake circulation: a coupled modelling approach

Interaction between ice sheet dynamics and subglacial lake circulation: a coupled modelling approach

... in ice core sam- ples (Karl et ...accreted ice, drilled at the Russian research station Vostok (Jouzel et ...overlying ice sheet has been analysed (Kwok et ...numerical models, which ... See full document

12

The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle

The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle

... with coupled atmosphere–ocean models dis- agree on the LGM AMOC strength, with some models sug- gesting that it was stronger than at present, whereas other models yield a weakening ... See full document

17

Coupling of climate models and ice sheet models by surface mass balance gradients: application to the Greenland Ice Sheet

Coupling of climate models and ice sheet models by surface mass balance gradients: application to the Greenland Ice Sheet

... simulated ice sheet volume and extent in this study are within the range of known reconstructions with similar ice sheet models, a note on the excess of ice along the ... See full document

18

Simulation of the future sea level contribution of Greenland with a new glacial system model

Simulation of the future sea level contribution of Greenland with a new glacial system model

... shallow ice approximation (SIA), important for the slow-flow regions in the more central re- gions of the ice ...Hybrid models have been developed before by Pollard and DeConto (2007), Pollard and ... See full document

25

The dynamics of the Lambert Amery glacial system and its response to climatic variations

The dynamics of the Lambert Amery glacial system and its response to climatic variations

... on ice dynamics and con- tributes to the temperature distribution of the ice and influences ice flow by varying ice viscosity and basal ...Antarctica Ice Sheet due to ... See full document

199

Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity

Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity

... one glacial cycle with a state-of- the-art coupled GCM remains computationally extremely de- ...the ice sheets are comparable or even longer than periodicity of the orbital forcing, it is not ... See full document

16

Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions

Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions

... have coupled a coarse-resolution AOVGCM (ECHAM5/MPIOM/LPJ; Mikolajewicz et ...allel Ice Sheet Model ...the models evolve freely sufficiently long to be largely independent of the initial ... See full document

20

A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models

A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models

... LGM ice sheet thicken due to decreased ...LGM ice volume relative to MHO/preindustrial ice volumes, since the decrease in inte- rior ice volume outweighs the increase in marginal ... See full document

13

Modelling large-scale ice-sheet–climate interactions following glacial inception

Modelling large-scale ice-sheet–climate interactions following glacial inception

... on ice-sheet evolution on multimillennial timescales during glacial ...an ice-sheet model alone, forced by a prescribed time-dependent climate that is estimated by interpolating between ... See full document

16

The importance of snow albedo for ice sheet evolution over the last glacial cycle

The importance of snow albedo for ice sheet evolution over the last glacial cycle

... simulated ice volume evolution over the last glacial cycle ...excessive ice growth with an LGM ice volume too large by a factor of 2 ...last glacial cycle also with these alternative ... See full document

11

Numerical simulations of the Cordilleran ice sheet through the last glacial cycle

Numerical simulations of the Cordilleran ice sheet through the last glacial cycle

... Cordilleran ice sheet dur- ing the LGM against that of an observation-based data set (WorldClim, Hijmans et ...extensive ice cover on the Columbia and Rocky mountains (Seguinot et ...the ice ... See full document

26

Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments

Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments

... precisely ICE-6G version ...ica. ICE-6G also takes account of the Earth’s rotational ef- fect (Rot) on the ...from ICE- 6G have been shown to provide a good fit to several hun- dred Holocene RSL ... See full document

17

Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum

Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum

... There are a number of possible errors in using marine radio- carbon dates obtained from organic matter to provide a minimum age for the retreat of grounded ice (cf. Andrews et al., 1999; Anderson et al., 2002; ... See full document

24

Modelling last glacial cycle ice dynamics in the Alps

Modelling last glacial cycle ice dynamics in the Alps

... For large Alpine glaciers flowing in deep valleys, such as the Rhône, Rhine and Adige glaciers, several thousand model years are needed to attain a thermodynamical equilibrium between cold-ice advection from the ... See full document

21

Dark ice dynamics of the south-west Greenland Ice Sheet

Dark ice dynamics of the south-west Greenland Ice Sheet

... the ice surface at depth, resulting in a hemispheric albedo increase that will be further enhanced by specular reflection when covered by a reflective layer of meltwater (Bøggild et ...the ice surface and ... See full document

16

Ice flow models and glacial erosion over multiple glacial–interglacial cycles

Ice flow models and glacial erosion over multiple glacial–interglacial cycles

... The ICE-Cascade model outputs used in this study include the glacial erosion rate, subglacial topography, glacier thick- ness, and sediment thickness; these primary outputs are ana- lyzed for the rest of ... See full document

18

Modelling the northern hemisphere and Antarctic ice sheet changes through the last glacial cycle

Modelling the northern hemisphere and Antarctic ice sheet changes through the last glacial cycle

... As part of the global approach to the niodelling of the last glacial cycle, the Antarctic Ice Sheet model was driven by the same sea level forcing as was applied to the northern hemisphe[r] ... See full document

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