Results 61 to 70 of about 470,222 (200)
Freezing Water and Supercooling: Anchor Ice and Frazil Ice [PDF]
AbstractThe supercooling of water in nature occurs more frequently than is generallyknown. It always takes place when still water is in process of being covered with thefirst ice needles. It is of even greater importance when ice formation takes place in running and turbulent water, in which case it represents the necessary conditions for the formation
openaire +1 more source
Abstract Sea ice is situated close to the termini of many outlet glaciers in the Arctic and Antarctic and has the potential to influence their dynamics and, therefore, their contribution to sea level rise. However, the nature, prevalence, and ice‐dynamic significance of sea ice‐glacier interactions remains subject to several open questions.
Katherine A. Deakin +3 more
wiley +1 more source
davidreesjones/frazil-dynamics: Revised release of frazil-dynamics software
<p>Revised version of software corresponds to revised version of manuscript: Rees Jones, D. W. and Wells, A. J.: Frazil-ice growth rate and dynamics in mixed layers and sub-ice-shelf plumes, The Cryosphere Discuss., <a href="https://doi.org/10 ...
David Rees Jones, davidreesjones
core +1 more source
The vertical concentration distribution of frazil-ice crystals in a stream during the formation and growth of frazil ice was discussed in a preliminary way by Gosink and Osterkamp (1981).
T. E. Osterkamp, J. P. Gosink
core +2 more sources
Is Radar Phase Information Useful for Sea Ice Detection in the Marginal Ice Zone?
With continuing sea ice reductions in the Arctic, dynamic physical and ecological processes have more active roles compared to the ice-locked, isolated Arctic Ocean of previous decades.
Fuhong Ding +3 more
doaj +1 more source
Ice Detection with Sentinel-1 SAR Backscatter Threshold in Long Sections of Temperate Climate Rivers
Climate change leads to more variable meteorological conditions. In many Northern Hemisphere temperate regions, cold seasons have become more variable and unpredictable, necessitating frequent river ice observations over long sections of rivers ...
Edvinas Stonevicius +2 more
doaj +1 more source
Measurements of frazil ice flocs in rivers
Abstract. Frazil floc sizes and concentrations have been investigated in a small number of laboratory studies, but no detailed field measurements have been reported previously. In this study, a submersible camera system was deployed a total of 11 times during the principal and residual supercooling phases in the North Saskatchewan, Peace, and ...
Chuankang Pei +3 more
openaire +1 more source
Modeling Hydro‐Ice‐Thermal Dynamics in Open Channels by a Double Layer‐Averaged Model
Abstract Ice processes in open channels are inherently multi‐physics phenomena, characterized by strong coupling of hydrodynamics, heat transfer, and phase‐change dynamics. While many models have been proposed to investigate ice processes, previous studies are often limited by oversimplified representations of flow, presumptions on channel geometry ...
Hengyan Wang +4 more
wiley +1 more source
Past and future interannual variability in Arctic sea ice in coupled climate models [PDF]
The diminishing Arctic sea ice pack has been widely studied, but previous research has mostly focused on time-mean changes in sea ice rather than on short-term variations that also have important physical and societal consequences.
J. R. Mioduszewski +5 more
doaj +1 more source
Future Warming of Circumpolar Deep Water Linked to Surface Buoyancy Forcing
Abstract Circumpolar Deep Water (CDW) is a warm water mass in the deep Southern Ocean and its transport onto the Antarctic continental shelf is the main contributor of heat to the region. Observations suggest that CDW has warmed and shifted poleward recently, potentially contributing to increased poleward heat transport and the accelerated melting of ...
Hangyu Meng +5 more
wiley +1 more source

