[PDF] Top 20 Communication : on the stability of ice 0, ice i, and Ih
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Communication : on the stability of ice 0, ice i, and Ih
... the stability of ice ...the ice zero unit cell, and identify the ground state as ...of ice, suggesting that the ice i structure ... See full document
6
Solid–liquid interfacial free energy of ice Ih, ice Ic, and ice 0 within a mono atomic model of water via the capillary wave method
... culations of Espinosa et al. 7 lies below that estimated from the Turnbull correlation, consistent with a positive Tolman length and a lowering of the interfacial free energy as expected for ice nuclei. 46 ... See full document
11
Investigating the sensitivity of numerical model simulations of the modern state of the Greenland ice-sheet and its future response to climate change
... Glimmer ice-sheet ...an ice-sheet model over Green- land because (a) the largest uncertainties are likely to be over Greenland ...personal communication, 2010), (b) no associated orography exists ... See full document
21
Brief communication: widespread potential for seawater infiltration on Antarctic ice shelves
... of ice shelves covered by a potential brine zone may also be set to grow in a warming ...underneath ice shelves have been observed to increase in re- cent decades, particularly in West Antarctica (Paolo et ... See full document
7
Satellite-derived submarine melt rates and mass balance (2011–2015) for Greenland’s largest remaining ice tongues
... Abstract. Ice-shelf-like floating extensions at the termini of Greenland glaciers are undergoing rapid changes with po- tential implications for the stability of upstream glaciers and the ice sheet ... See full document
10
Brief communication “The aerophotogrammetric map of Greenland ice masses”
... The ice-margin vectors in the PROMICE dataset derive from aerophotogrammetric maps at scales of 1 : 100 000 and 1 : 250 000, referred to as G100 and G250 in the ...the ice sheet, and are based on 1 : 150 ... See full document
5
Communication : thermodynamics of stacking disorder in ice nuclei
... of ice 1 is constructed for nuclei in su- percooled water, and combined with classical nucleation ...hexagonal ice I within the range of experimental estimates, this predicts critical nuclei are ... See full document
6
Antarctic bedrock topography uncertainty and ice sheet stability
... including ice volume changes created solely by the differences in topog- raphy, we calculate changes in ice sheet volume as the difference between the warm climate simulation after 3 kyrs and the end of the ... See full document
6
Sensitivity, stability and future evolution of the world’s northernmost ice cap, Hans Tausen Iskappe (Greenland)
... The accumulation has been derived from field measurements and four shallow cores that cover most of the 20th century (Reeh et al., 2001). The accumulation is the highest in the north(-west), which is related to the ... See full document
21
Thermodynamics of ice interfaces and structures within a coarse grained model of water
... between ice-Ic and ice-Ih is diffi- cult to definitively ...in ice-Ic, the isotropic component of the free energy can be lower or higher, respectively, than that of ...for ice-Ic is ... See full document
185
Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada)
... measuring ice texture and fabric re- quires that an ice core or block is sliced into 1 cm thick vertical and horizontal sections with a band saw and then thinned to the desired thickness (< ... See full document
15
The relation between sea ice thickness and freeboard in the Arctic
... sea ice thickness through converting ice freeboard measurements to thickness by assuming hydro- static equilibrium (Laxon, 1994; Laxon et ...measuring ice freeboard is based on exper- iments showing ... See full document
8
Kinematic response of ice-rise divides to changes in ocean and atmosphere forcing
... For both ice rises, divide migration shows a clear depen- dence on mesh resolution. As the regular mesh simulations are most likely under-resolved, we will mainly focus here on the refined mesh simulations. In the ... See full document
19
On the influence of model physics on simulations of Arctic and Antarctic sea ice
... ocean-sea ice model to the representation of physics in its sea ice com- ponent: two hindcast simulations have been studied over the period 1983–2007, for both Arctic and Antarctic sea ice, with an ... See full document
13
An analysis of at home demand for ice cream in the United States
... characterize ice cream purchases were all based on a representative sample of the 2005 United States popula- ...purchased ice cream within a 12-mo period were included in the analysis, whether they ... See full document
8
Increased Arctic sea ice volume after anomalously low melting in 2013
... thick ice cover in the MYI region north of Greenland and Ellesmere Island (Figure 1d), with ice being 21% thicker, on average, than the five year ...all ice types, as FYI is replaced by MYI over the ... See full document
18
Ice swimming – ‘Ice Mile’ and ‘1 km Ice event’
... ‘International Ice Swimming Association’ (IISA) [22]. The IISA introduced the ‘Ice Mile’ as its ultim- ate achievement of swimming in ice cold ...an ice swimmer can complete an of- ficial ... See full document
7
Seismic wave propagation in anisotropic ice – Part 1: Elasticity tensor and derived quantities from ice-core properties
... To be able to calculate the opening angels from the COF eigenvalues, the fabrics are classified into the different fabric groups based on their eigenvalues: cone, thick girdle and par- tial girdle fabric (Table 1). This ... See full document
18
Wave-induced stress and breaking of sea ice in a coupled hydrodynamic discrete-element wave–ice model
... sea ice–wave model is de- veloped and used to analyze wave-induced stress and break- ing in sea ice for a range of wave and ice ...sea ice module is a discrete-element bonded-particle model, ... See full document
15
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr
... With the EDC3 chronology (Parrenin et al., 2007a), the sur- face temperature history is deduced from the isotopic content of the ice without correction for source temperature varia- tions. The β coefficient in Eq. ... See full document
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