[PDF] Top 20 Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model
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Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model
... LIG sea-level high stand is thus far elusive, support for a contribu- tion from the AIS is usually given as a residual of total sea- level stand minus contributions from the ... See full document
19
Regional Antarctic snow accumulation over the past 1000 years
... Antarctic Ice Sheet (AIS) is the largest reservoir of fresh water on the planet and has the potential to raise global sea level by about ...mean sea level, but also on the wider ... See full document
23
Nonlinear response of the Antarctic Ice Sheet to late Quaternary sea level and climate forcing
... Greenland Ice Sheet, the AIS has large marine- based margins. The ice shelves surrounding the AIS have a buttressing effect and therefore play an important role in de- termining its ...of ice ... See full document
17
Modelling the Early Weichselian Eurasian Ice Sheets: role of ice shelves and influence of ice-dammed lakes
... Eurasian ice sheet through the Early Weichselian (90 kyr ...AGCM climate with and without the influence of ice- dammed lakes, applying the reconstructed climate to the GRISLI ice ... See full document
12
The land-ice contribution to 21st-century dynamic sea level rise
... land-based ice melt. We assess two ice melt scenarios developed under the aus- pices of the European Union ice2sea project which include updated projections of the Glacier and Ice Cap (G&IC) ... See full document
16
LIVVkit 2.1: automated and extensible ice sheet model validation
... of model improvements and to increase confidence in model ...to ice sheets themselves, has prevented a com- prehensive assessment of ISM and coupled ESM-ISM skill, and key climatological ... See full document
20
A new coupled ice sheet/climate model: description and sensitivity to model physics under Eemian, Last Glacial Maximum, late Holocene and modern climate conditions
... heat from north to south (or vice versa) are not significant in the con- trol Eemian simulation, resulting in AIS surface tempera- tures and SMB that remained relatively unchanged despite the large positive ... See full document
20
Heinrich events show two-stage climate response in transient glacial simulations
... (A2). From ExB and ExC, we obtain two Hein- rich events starting at ...concentrations from reconstructions (Berger, 1978; Spahni and Stocker, 2006a, b; Lüthi et ...Antarctic Ice Sheet and the ... See full document
16
Antarctic last interglacial isotope peak in response to sea ice retreat not ice-sheet collapse.
... the last interglacial (LIG; 130,000–115,000 years ago) global climate was warmer than today 1–4 and global mean sea level was 6-9 m higher 5–10 ...LIG sea-level high stand ... See full document
9
Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model
... the model does not capture the magnitude of the SST anomalies derived from marine ...rived from proxy data by the models is also found in model– data comparison studies for the Holocene ... See full document
26
Uncertainties in the modelled CO2 threshold for Antarctic glaciation
... matology from the climate model (surface air temperature and precipitation) is used to force the ice sheet model with no subsequent feedbacks, other than height-mass balance ... See full document
16
Persistent influence of ice sheet melting on high northern latitude climate during the early Last Interglacial
... gian Sea cores (Fig. 7a) strongly argues in favour of ice sheet melting during the early LIG, other modelling studies exhibit a similar cold North Atlantic climate (Felis et ...Labrador ... See full document
25
Greenland ice sheet contribution to sea level rise during the last interglacial period: a modelling study driven and constrained by ice core data
... RACMO2 climate fields, Xavier Fettweiss for providing the MAR climate fields and Pascale Braconnot for providing the IPSL 126 ka BP model ...of Ice and Climate at the Niels Bohr ... See full document
14
Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma
... sustained, sea-level contribu- tion from the EAIS, arising from both dynamic adjustment to the loss of fringing ice shelves, and from surface lowering resulting from ... See full document
17
Greenland ice sheet contribution to sea-level rise from a new-generation ice-sheet model
... scale ice- sheet model (Little et ...field from observed present-day geom- etry and surface velocities ...first model to use all three developments simultaneously to produce prognostic ... See full document
16
A fully coupled 3-D ice-sheet–sea-level model: algorithm and applications
... predefined ice load over 480 kyr to demon- strate how the moving time window works ...Earth model. The coastlines are fixed and an axisymmetric ice load is lo- cated on the south pole with a ... See full document
16
Mechanisms causing reduced Arctic sea ice loss in a coupled climate model
... high ice extent ...September ice extent, but in the two cases mentioned above low SPG index coincides with low temperatures in the top 70 m of the Nordic seas, low OHT, low Arctic OI heat flux and high ... See full document
13
Results from the implementation of the Elastic Viscous Plastic sea ice rheology in HadCM3
... Sea ice is an important aspect of polar climate and strongly affects the ocean-atmosphere exchange of ...of climate change in the polar ...tic sea ice model within any ... See full document
11
A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models
... broader climate model ...overlying climate model forcing (which is a large and ongoing task that is subject to change as CESM is developed further) but rather to verify that the spin- up ... See full document
13
Quantification of the Greenland ice sheet contribution to Last Interglacial sea level rise
... the ice sheet model simulations pre- sented here is that they do not include the process of basal sliding which has implications for the amount of ice mass lost ...the ice velocity, by ... See full document
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