Responses of sub-ice platelet layer thickening rate and frazil-ice concentration to variations in ice-shelf water supercooling in McMurdo Sound, Antarctica [PDF]
Persistent outflow of supercooled ice-shelf water (ISW) from beneath McMurdo Ice Shelf creates a rapidly growing sub-ice platelet layer (SIPL) with a unique crystallographic structure under the sea ice in McMurdo Sound, Antarctica.
C. Cheng +10 more
doaj +1 more source
An inter-comparison of the mass budget of the Arctic sea ice in CMIP6 models [PDF]
We compare the mass budget of the Arctic sea ice for 15 models submitted to the latest Coupled Model Intercomparison Project (CMIP6), using new diagnostics that have not been available for previous model inter-comparisons.
A. Keen +17 more
doaj +1 more source
Adhesion of frazil ice to underwater structures
The adhesion of frazil ice to different surfaces was studied in the laboratory under varying conditions. Field tests were made by submerging pipes, coated in a non-ice- nucleating grease, in frazil-producing rapids. The results of these experiments are discussed and the usefulness of protective coatings in preventing the adhesion of frazil ice to ...
Williams, G. P.
openaire +2 more sources
Laboratory study of the properties of frazil ice particles and flocs in water of different salinities [PDF]
Measurements of the size and shape of frazil ice particles and flocs in saline water and of frazil ice flocs in freshwater are limited. This study consisted of a series of laboratory experiments producing frazil ice at salinities of 0 ‰, 15
C. C. Schneck +2 more
doaj +1 more source
Frazil-ice growth rate and dynamics in mixed layers and sub-ice-shelf plumes [PDF]
The growth of frazil or granular ice is an important mode of ice formation in the cryosphere. Recent advances have improved our understanding of the microphysical processes that control the rate of ice-crystal growth when water is cooled beneath its ...
D. W. Rees Jones +2 more
doaj +1 more source
Laboratory study of frazil ice accumulation under wave conditions [PDF]
Ice growth in turbulent seawater is often accompanied by the accumulation of frazil ice crystals at its surface, forming a grease ice layer. The thickness and volume fraction of this ice layer play an important role in shaping the gradual transition from
S. De la Rosa, S. Maus
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High-resolution simulations of interactions between surface ocean dynamics and frazil ice [PDF]
Frazil and grease ice forms in the ocean mixed layer (OML) during highly turbulent conditions (strong wind, large waves) accompanied by intense heat loss to the atmosphere.
A. Herman, M. Dojczman, K. Świszcz
doaj +1 more source
The Effect of Pseudofrazil Particle Entrainment on Salinity Measurements
Salinity effects of particles entrained into conductivity cells have previously mainly been studied in the context of suspended sediment. Particles influencing conductivity cells can also be small ice crystals (frazil) that may form in supercooled water.
Maren Elisabeth Richter +5 more
doaj +1 more source
Frazil ice growth and production during katabatic wind events in the Ross Sea, Antarctica [PDF]
Katabatic winds in coastal polynyas expose the ocean to extreme heat loss, causing intense sea ice production and dense water formation around Antarctica throughout autumn and winter.
L. Thompson +6 more
doaj +1 more source
Concern has been expressed regarding the impacts of climate change on river ice and ice jam formation in cold regions. Ice jams are easily initiated in bends and narrow channels and cause disasters.
Shui-Xia Zhao +9 more
doaj +1 more source

