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Both hpAfrica2 strains contain one full-length ICE Hptfs4b element, and the hpSahul strain harbours a full-length ICE Hptfs4b and a partial ICE Hptfs3 element (data not shown), which further supports the notion that these elements are present in all phylogeographic groups.
A partial ice cover, however, yields heterogeneous fluxes of buoyancy that are not resolved by the computational grid.
The presented data set represents the most thorough experimental examination of flow characteristics beneath a partial ice cover.
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Partial ice coverage extent was found to have a relative width of transition to be consistent while increasing Froude was found to produce a smaller transition region.
The influence of different extents of partial ice coverages and different Froude numbers was explored.
Bench-scale barriers with full and partial ice saturation were studied.
The partial ice cover was found to impact the flow distribution within the channel and a classification system was developed to divide the channel cross-section into open, transitional and covered sections.
Core sub-regions retain partial ice cover throughout the year, and in winter show complete ice cover, while in peripheral sub-regions, winter coverage is not complete, and there is no ice cover at all in the summer.
What are here denoted "core" Arctic sea regions (namely the central Arctic Ocean, the Canadian Archipelago, and Hudson Bay) retain partial ice cover throughout the year, and in winter months show complete ice cover.
In addition to 12 different sites described previously [ 16], we identified further 28 chromosomal sites and one plasmid site where complete or partial ICE Hptfs3 or ICE Hptfs4 elements can be integrated (Tables 2 and 3; Figure 4).
Superchilling is a method of preserving food by partial ice-crystallization.
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