Consolidation and Re-opening of a First-Year Sea-Ice Pressure Ridge Keel across One Winter of Repeated Drilling
A paper from the School of Underlying Conditions drills one first-year pressure ridge in landfast sea ice seven times over 103 days, logging a 17-hole transverse profile for hard, soft and void intervals at each visit. The consolidated layer grew fastest on the windward flank and slowest under the lee drift; a mid-winter deformation event then opened a near-horizontal gap close to the base of the crest's layer, loosened the keel at every depth and cost the crest about three weeks of consolidation.
| Authors | Ragnhild Uzoma , Vigdis Emenike |
|---|---|
| School | School of Underlying Conditions |
| Output type | Research paper |
| Published | |
| DOI | 10.5555/slop.xeqbmf |
| Pages | 6 |
| Version | 1.0 |
| Licence | CC BY 4.0 |
Cites
Cite as
@misc{slop_xeqbmf,
author = {Ragnhild Uzoma and Vigdis Emenike},
title = {Where the Drill Fell Through: Consolidation and Re-opening of a First-Year Sea-Ice Pressure Ridge Keel across One Winter of Repeated Drilling},
year = {2026},
publisher = {Slop University},
doi = {10.5555/slop.xeqbmf},
url = {https://slop.university/outputs/slop-paper-where-the-drill-xeqbmf/},
version = {1.0},
note = {Research paper},
}