Results 41 to 50 of about 69,716 (313)

Ice Floe Trajectory Under the Action of Propeller Pumping

open access: yesShanghai Jiaotong Daxue xuebao, 2021
In order to study the influence of propeller pumping action on ice trajectory during the process of ice propeller interference, this paper built a motion trajectory measurement platform based on circulating water tank, combining high-speed camera and the
WANG Chao, YANG Bo, WANG Chunhui, GUO Chunyu, XU Pei
doaj   +1 more source

Ice sheet extent and early deglacial history of the southwestern sector of the Greenland ice sheet [PDF]

open access: yes, 2009
The offshore and coastal geomorphology of southwest Greenland records evidence for the advance and decay of the Greenland Ice Sheet during the Last Glacial Maximum.
Xu, S.   +16 more
core   +1 more source

Influence of Velocity on Ice-Cone Interaction

open access: yes, 2001
A series of upward breaking cone tests was conducted at NRC/IMD’s ice tank in level ice using EG/AD/S correct density model ice. Cone angles of 45° and 60° were tested. The effect of ice draft velocity in the range 0.005 to 0.5 m/s was studied for ice thicknesses ranging from 35 to 110 mm. The mean peak forces in both horizontal and vertical directions
Lau, M.   +3 more
openaire   +3 more sources

Subglacial roughness of the Greenland Ice Sheet: relationship with contemporary ice velocity and geology [PDF]

open access: yesThe Cryosphere, 2019
Abstract. The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly constrained, both in its bulk properties, for example geology, presence of sediment, and of water, and interfacial conditions, such as roughness and bed rheology. There is, therefore, limited understanding of how spatially heterogeneous subglacial properties relate to ice ...
M. A. Cooper   +9 more
openaire   +5 more sources

The distribution of basal motion beneath a High Arctic polythermal glacier [PDF]

open access: yes, 2003
The longitudinal pattern of surface velocity of a large, predominantly colds polythermal glacier (John Evans Glacier, Ellesmere Island, Canada) was measured over summer and winter periods.
Nienow, Peter W.   +12 more
core   +1 more source

An ice-sheet scale comparison of eskers with modelled subglacial drainage routes [PDF]

open access: yes, 2015
Eskers record the signature of channelised meltwater drainage during deglaciation providing vital information on the nature and evolution of subglacial drainage.
Stokes, C.R.   +23 more
core   +1 more source

Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set

open access: yesJournal of Glaciology, 2023
The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures ...
Signe H. Larsen   +5 more
doaj   +1 more source

Potential subglacial lake locations and meltwater drainage pathways beneath the Antarctic and Greenland ice sheets [PDF]

open access: yes, 2013
We use the Shreve hydraulic potential equation as a simplified approach to investigate potential subglacial lake locations and meltwater drainage pathways beneath the Antarctic and Greenland ice sheets. We validate the method by demonstrating its ability
Clark, Chris   +13 more
core   +1 more source

Bayesian Inference of Ice Softness and Basal Sliding Parameters at Langjökull

open access: yesFrontiers in Earth Science, 2021
We develop Bayesian statistical models that are designed for the inference of ice softness and basal sliding parameters, important glaciological quantities.
Giri Gopalan   +3 more
doaj   +1 more source

Impact of boundary conditions on the modeled thermal regime of the Antarctic ice sheet [PDF]

open access: yesThe Cryosphere
A realistic initialization of ice flow models is critical for predicting future changes in ice sheet mass balance and their associated contribution to sea level rise. The initial thermal state of an ice sheet is particularly important, as it controls ice
I.-W. Park   +4 more
doaj   +1 more source

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