Abstract
The ice cap covering Antarctica does in general not terminate at the edge of the continent. In most regions the ice is pushed into the sea, taking the appearance of a floating ice shelf. At the edges of the shelves, huge parts break off and drift away as tabular icebergs, characteristic for the Antarctic. As a result, the edge of an ice shelf usually has the form of a straight, vertical wall. Although the major part of this ice wall is submerged, it rises some tens of meters out of the sea — hence the common name ‘barrier’. Under typical conditions the submerged part of the ice wall measures roughly 200 m, while the sub-ice sea depths range from a few tens to a few hundreds of meters. Because the ice wall does not reach to the sea bottom, the shelf edge forms (in oceanographic sense) a highly remarkable type of ‘coast’. The present paper addresses the oceanic circulation near the shelf-ice edge, and concentrates on two aspects, namely the large-scale flow driven by wind stresses in the open sea, and the smaller-scale circulation driven by melting of the ice wall.
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References
Buckley J R, Gammelsrtd T, Johannessen J A, Johannessen 0 M and Reed L P (1979), Upwelling: oceanic structure at the edge of the Arctic ice pack in winter. Science 203, 165–167
Clarke A J (1978), On wind-driven quasi-geostrophic water movements near fast-ice edges. Deep-Sea Res. 25, 41–51
Foster T D and Carmack E C (1976), Temperature and salinity structureArctic in the Weddell Sea. Journ. Phys. Oceanogr. 6, 36–44
GammelsrØd T, Mork M and RØed L P (1975), Upwelling possibilities at an ice edge : homogeneous model. Mar. Sci. Commun. 1, 115–145
Van Heijst G J F (1984), An analytical model for ice-edge upwelling. Geophys. Astrophys. Fluid Dyn. 29, 155–177
Horne E P W (1985), Ice-induced vertical circulation in an Arctic fiord. Journ. Geophys. Res. 90, 1078–1086
Huppert H E and Josberger E G (1980), The melting of ice in cold stratified water. Journ. Phys. Oceanogr. 10, 953–960
Huppert H E and Turner J S (1978), On melting icebergs. Nature 271, 46–48
Huppert H E and Turner J S (1980), Ice blocks melting into a salinity gradient. Journ. Fluid Mech. 100, 367–384
Jacobs S S, Ruppert H E, Holdsworth G and Drewry D J (1981), Thermohaline steps induced by melting of the Erebus Glacier Tongue. Journ. Geophys. Res. 86, 6547–6555
Johannessen O M, Johannessen J A, Morison J, Farrelly B A and Svendsen E A S (1983), Oceanographic conditions in the marginal ice zone north of Svalbard in early fall 1979 with emphasis on mesoscale processes. Journ. Geophys. Res. 88, 2755–2769
Josberger E G and Martin S (1981), A laboratory and theoretical study of the boundary layer adjacent to a vertical melting ice wall in salt water. Journ. Fluid Mech. 111, 439–473
MacAyeal D R (1984), Thermohaline circulation below the Ross Ice Shelf: a consequence of tidally induced vertical mixing and basal melting. Journ. Geophys. Res. 89, 597–606
Neshyba S (1977), Upwelling by icebergs. Nature 267, 507–508
Niebauer H J (1982), Wind and melt driven circulation in a marginal sea ice edge frontal system: a numerical model. Cont. Shelf Res. 1, 49–98
Pedlosky J (1979), Geophysical fluid dynamics. Springer Verlag, 624 pp
Sverdrup H U (1953), The currents off the coast of Queen Maud Land. Norsk Geografisk Tidsskrift 14, 239–249
Turner J S (1973), Buoyancy effects in fluids. Cambridge University Press, 367 pp
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© 1987 D. Reidel Publishing Company
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van Heijst, G.J.F. (1987). On the Oceanic Circulation Near a Shelf-Ice Edge. In: Van der Veen, C.J., Oerlemans, J. (eds) Dynamics of the West Antarctic Ice Sheet. Glaciology and Quaternary Geology, vol 4. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3745-1_3
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DOI: https://doi.org/10.1007/978-94-009-3745-1_3
Publisher Name: Springer, Dordrecht
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