Bottom Ice Accretion
Bottom Ice Accretion is a sea ice mass balance process denoting the growth of ice at the basal interface due to the freezing of seawater onto the underside of the existing ice cover.
8
Publications
710
Citations
28
Authors
13
Institutions
Publications per year
2017–2026
2
Parents
8
1–5 of 8
28
2
h-index
2
h-index
1
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
1 publications · 39 citations
1
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
1 publications · 39 citations
1
h-index
1–5 of 28
13
Memorial University of Newfoundland
St. John's, Canada
2 h-index
4 publications
132 citations
Antarctic Climate and Ecosystems Cooperative Research Centre
Hobart, Australia
1 h-index
2 publications
724 citations

National Institute of Polar Research
Tokyo, Japan
1 h-index
1 publications
362 citations

Stockholm University
Stockholm, Sweden
1 h-index
1 publications
362 citations

University of Tasmania
Hobart, Australia
1 h-index
3 publications
1.1K citations

Macquarie University
Sydney, Australia
1 h-index
1 publications
362 citations

Tokyo University of Marine Science and Technology
Tokyo, Japan
1 h-index
2 publications
724 citations
University of Bremen
Bremen, Germany
1 h-index
1 publications
39 citations
1–8 of 13
JGR · 2 publications · 167 citations
2
h-index
2 publications · 66 citations
2
h-index
1 publications · 34 citations
1
h-index
1 publications · 39 citations
1
h-index
1 publications · 362 citations
1
h-index
1–5