• No results found

[PDF] Top 20 Modelling last glacial cycle ice dynamics in the Alps

Has 10000 "Modelling last glacial cycle ice dynamics in the Alps" found on our website. Below are the top 20 most common "Modelling last glacial cycle ice dynamics in the Alps".

Modelling last glacial cycle ice dynamics in the Alps

Modelling last glacial cycle ice dynamics in the Alps

... Parallel Ice Sheet Model (PISM) to model the entire last glacial cycle (120–0 ka) in the Alps, using horizontal resolutions of 2 and 1 ...for Ice Coring in Antarctica (EPICA) ... See full document

21

A geomorphology based reconstruction of ice volume distribution at the Last Glacial Maximum across the Southern Alps of New Zealand

A geomorphology based reconstruction of ice volume distribution at the Last Glacial Maximum across the Southern Alps of New Zealand

... Southern Alps was deposited post-LGM (Suggate, 1965; Adams, 1980) simply due to the ‘ absence of any con fl icting evidence ’ Adams (1980, ...Southern Alps, with Rother et ...A modelling study by ... See full document

16

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

... of modelling results with a so-called Baseline Experiment ...between modelling results and palaeoclimate ...the last glacial cycle with different combinations of key model ...the ... See full document

16

Modelling ice sheet evolution and atmospheric CO2 during the Late Pliocene

Modelling ice sheet evolution and atmospheric CO2 during the Late Pliocene

... ANICE ice-sheet model (Bintanja and Van de Wal, 2008; de Boer et ...the Last Glacial Maximum (Sin- garayer and Valdes, 2010), they were able to simultaneously simulate the evolution of the ice ... See full document

17

Numerical reconstructions of the flow and basal conditions of the Rhine glacier, European Central Alps, at the Last Glacial Maximum

Numerical reconstructions of the flow and basal conditions of the Rhine glacier, European Central Alps, at the Last Glacial Maximum

... the ice surface. Since in our model the ice sur- face temperature is decoupled from the mass balance, tem- perature has only lower-order effects on the ice flow dynam- ics, which is mainly controlled ... See full document

30

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

... major ice shelves, that as it flows towards the sea the width of the ice shelf initially narrows as it progresses, creating a choke point in the ice shelf which likely provides significant ... See full document

199

A new sub-grid surface mass balance and flux model for continental-scale ice sheet modelling: testing and last glacial cycle

A new sub-grid surface mass balance and flux model for continental-scale ice sheet modelling: testing and last glacial cycle

... the ice sheet extent and ...on, ice accumulating in higher regions flows downhill and accumulates in regions close to the ELA and in valleys ...ample, ice to build up in the northern part of ...the ... See full document

15

The effect of sediment loading in Fennoscandia and the Barents Sea during the last glacial cycle on glacial isostatic adjustment observations

The effect of sediment loading in Fennoscandia and the Barents Sea during the last glacial cycle on glacial isostatic adjustment observations

... for glacial isostatic adjustment (GIA) rou- tinely include the effects of meltwater redistribution and changes in topography and ...the dynamics of ice sheets may be com- parable to that of sea level ... See full document

14

Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle

Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle

... pre-LGM ice sheets helped shape the evolution of the ice sheets themselves (Beghin et ...the dynamics of a single continental-scale ice sheet on a flat continent (Roe and Lindzen, 2001; Li- ... See full document

19

New approaches to field model data comparison: numerical modelling of the last glacial cycle in the Welland catchment, England

New approaches to field model data comparison: numerical modelling of the last glacial cycle in the Welland catchment, England

... recent glacial-interglacial ...the glacial period, with addition of material from upslope at each time period, but the bulk of the deposits laid down were sourced from geological resetting of older ...the ... See full document

49

Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0

Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0

... the ice sheet in this area); thus, there is an overall movement of freshwater ...Fennoscandian ice sheet causes a significant lateral movement of water to its ends when us- ing dynamic river ... See full document

26

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

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

... of ice sheet retreat are consistent between the two simulations and show a rapid deglaciation of the southern sector of the ice sheet, including a rapid northwards retreat across the Interior Plateau of ... See full document

26

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

... Laurentide ice sheet and the orientation of the Atlantic storm track sug- gests that the North American glacial topography may have influenced the ice-sheet evolution in ...static ice sheets ... See full document

17

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

273

Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum

Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum

... separation was performed following Stein and Alpert (1993). They developed this technique to separate pure contribu- tions of different processes in a climate change signal from synergistic effects that result from ... See full document

7

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

... individual ice streams across the western AP shelf was therefore asynchronous between troughs in terms of the timing of initial grounding line ...and ice-shelf breakup and reformation episodes ... See full document

24

Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle

Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle

... star). Ice flowing into Taylor Valley originates on the northern flank of Taylor ...D1–D3. Ice flow is from the SW to the NE (lower left to upper ...of ice from Ferrar Glacier (lower right), with a ... See full document

16

The simulated climate of the Last Glacial Maximum and insights into the global marine carbon cycle

The simulated climate of the Last Glacial Maximum and insights into the global marine carbon cycle

... of glacial–interglacial ...during glacial periods is still under ...the Last Glacial Maximum (LGM) using the CSIRO Mk3L-COAL (Carbon–Ocean– Atmosphere–Land) earth system model to test the ... See full document

25

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach

... and ice from a surplus in the surface energy balance when the ice sheet surface tem- perature reaches melting ...and ice sheets, which are not accounted for by the PDD method, are important for ... See full document

14

Eurasian contribution to the last glacial dust cycle: how are loess sequences built?

Eurasian contribution to the last glacial dust cycle: how are loess sequences built?

... al. (2012) have described abrupt millennial-scale changes ex- pressed by detailed synchronous mean grain size variations over the 60–10 ka b2k interval in deposited wind blown mate- rial, from coarser material during the ... See full document

17

Show all 10000 documents...

Related subjects