[PDF] Top 20 Capabilities and performance of Elmer/Ice, a new-generation ice sheet model
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Capabilities and performance of Elmer/Ice, a new-generation ice sheet model
... years of consistent devel- opments and present the current state of the new-generation ice sheet model Elmer/Ice (Elmer library version ... See full document
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Greenland Ice Sheet contribution to sea-level rise from a new-generation ice-sheet model
... S., and Zwinger, T.: Benchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP–HOM), The Cryosphere, 2, 95–108, ... See full document
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Probabilistic calibration of a Greenland Ice Sheet model using spatially resolved synthetic observations: toward projections of ice mass loss with uncertainties
... sequence of parameter combinations, each of which is chosen randomly from the region of parameter space surrounding the last ...probability of the new point is greater than at the ... See full document
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Marine mammal strandings and environmental changes: a 15-year study in the St. Lawrence ecosystem.
... Canada) and since 2003, by RQUMM, a marine mammal response network co-ordinated by the non-governmental organi- zation, Groupe de recherche et d’e´ducation sur les mammife`res marins (GREMM) under contract to ... See full document
10
Investigating the evolution of major Northern Hemisphere ice sheets during the last glacial-interglacial cycle
... knowledge of the Earth’s glacial and climatic his- tory can be obtained by the numerical modeling of ice ...extent and volume of the Northern Hemisphere (NH) ice sheets ... See full document
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Greenland Ice Sheet seasonal and spatial mass variability from model simulations and GRACE (2003–2012)
... patterns of mass change from GRACE-LM in northeast Greenland, but it is unclear how variations in flow of different glaciers con- tribute to seasonal fluctuations in ice sheet discharge, ... See full document
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Simulation of the satellite radar altimeter sea ice thickness retrieval uncertainty
... variability of the effective scattering surface as a result of the sub-footprint spatial backscatter and elevation distribution sometimes called preferential ...part of the ice volume ... See full document
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A new coupled ice sheet-climate model: description and sensitivity to model physics under Eemian, Last Glacial Maximum, late Holocene and modern climate conditions
... instead of a positive-degree-day (PDD) model, to calculate the SMB for reasons that have been recently described ...or ice melt ...effect of changing albedo and related non-sensible ... See full document
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Refreezing on the Greenland ice sheet: a comparison of parameterizations
... content of the snow before the melting season ...effects of refreezing below this depth requires a more comprehensive calculation of the temperature profile in the upper ice and snow ... See full document
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Laboratory and modeling studies on the effects of water and soot emissions and ambient conditions on the properties of contrail ice particles in the jet regime
... more ice particles undetectable by the OPC and reducing the ice particle concentration mea- sured ...scatter and loss in the sampling process may also contribute to the reduction of the ... See full document
12
Enthalpy benchmark experiments for numerical ice sheet models
... conservation of water volume is also addressed here. An initially cold ice body that runs through a warmer period with an associated built up of a liquid water layer at the base must be able to ... See full document
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Modelling the mid-Pliocene Warm Period climate with the IPSL coupled model and its atmospheric component LMDZ5A
... magnitude of the warming, this period is of high inter- est for understanding feedbacks and mechanisms that sus- tained such a warm ...strengths and weaknesses of each model when ... See full document
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Climate of the Greenland ice sheet using a high-resolution climate model – Part 1: Evaluation
... It is known that the mixing scheme in RACMO2 is too active, especially under very stable atmospheric conditions (Van Meijgaard et al., 2008). This SHF winter bias is smaller at S5, because this site is closer to the ... See full document
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Retrieval of the thickness of undeformed sea ice from simulated C-band compact polarimetric SAR images
... ratio and thin ice thickness was first demonstrated by On- stott (1992), based on C-band radar data from the eastern Arctic ...thin ice thick- ness (0 to 0.1 m) from L- and C-band fully ... See full document
17
Grounding line transient response in marine ice sheet models
... each model in order to calculate a steady state ...buttressed ice-shelf (C F = ...position of less than 20 km (see Fig. 1). We chose the simpler, stable case of a forward slope for the simple ... See full document
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Orange fiber as a novel fat replacer in lemon ice cream
... that ice creams supplemented with pretreated orange peel fiber (ICG) did not significantly change the most important physical and sensory properties of the ice creams, such as the color ... See full document
9
Simulating the Greenland ice sheet under present-day and palaeo constraints including a new discharge parameterization
... R., and Wang, W. L.: Insights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project II: Greenland, ... See full document
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Ice and AIS: ship speed data and sea ice forecasts in the Baltic Sea
... N and 19.8–21.0 ◦ E, Fig. 1), which is regularly passed by ships and known for its severe ice ...south of the so-called Kvark Strait (Green et ...mean ice drift in the test region is ... See full document
10
King George Island ice cap geometry updated with airborne GPR measurements
... Abstract. Ice geometry is a mandatory requirement for numerical modelling ...the ice thickness, the bedrock topography and the ice surface topography of the King George Island ... See full document
8
Individual and combined effects of ice sheets and precession on MIS-13 climate
... BP) and the other when it occurs at aphelion (at 495 ka ...volumes of the Eurasian and North American ice sheets (ranging from 0 to the Last Glacial Maximum one) are done under these two ... See full document
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