Sub-ice-shelf Circulation
Sub-Ice-Shelf Circulation is a glaciological process denoting the movement of oceanic water beneath marine ice shelves, driven by density gradients and tidal forcing, which distinguishes it from other ice-ocean interaction dynamics through its role in regulating basal melt patterns and exchange of heat and freshwater between the continental shelf and the sub-ice-shelf cavity.
108
Publications
9.6K
Citations
369
Authors
160
Institutions
Publications per year
2017–2026
32
Parents
108
Melting of ice shelves and the mass balance of Antarctica
Stanley S. Jacobs, H.H. Helmer, C. S. M. Doake et al. · Journal of Glaciology · 1992 · 424 citations · Full text
1–5 of 108
369
17
h-index
14
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
12 publications · 2K citations
12
h-index
11
h-index
10
h-index
1–5 of 369
160

British Antarctic Survey
Cambridge, United Kingdom
26 h-index
83 publications
8.2K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
18 h-index
38 publications
5.9K citations
Natural Environment Research Council
Swindon, United Kingdom
17 h-index
50 publications
5.3K citations
Columbia University
New York, United States
17 h-index
30 publications
4.3K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
15 h-index
51 publications
6.1K citations

University of Tasmania
Hobart, Australia
8 h-index
25 publications
1.6K citations
Antarctic Climate and Ecosystems Cooperative Research Centre
Hobart, Australia
8 h-index
25 publications
1.8K citations
Jet Propulsion Laboratory
Pasadena, United States
8 h-index
20 publications
2.1K citations
1–8 of 160
17 publications · 1.2K citations
17
h-index
JGR · 13 publications · 1.2K citations
13
h-index
13 publications · 1.2K citations
12
h-index
6 publications · 622 citations
6
h-index
6 publications · 677 citations
6
h-index
1–5