Geodesic
The response of the ice shelf base on the ocean temperature change
Matematičeskoe modelirovanie, Tome 14 (2002) no. 6, pp. 43-50.

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The response of the Ice Shelf base on the possible Global ocean temperature changes has been studied by the numerical modeling. Two-dimensional model of the thermohaline ocean circulation under the Ice Shelf caused by the heat and mass transfer at the ice shelf and ocean boundary has been considered. The melting/freezing rate has been estimated. The melting/freezing can be indication of the ocean temperature global change. 
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     title = {The response of the ice shelf base on the ocean temperature change},
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O. V. Nagornov; O. V. Sergienko. The response of the ice shelf base on the ocean temperature change. Matematičeskoe modelirovanie, Tome 14 (2002) no. 6, pp. 43-50. http://geodesic.mathdoc.fr/item/MM_2002_14_6_a3/

[1] Baggeroer A., Munk W., “The Heard Islands feasibility test”, Physics Today, 45:9 (1992), 22–30 | DOI

[2] Nagornov O. V., Sergienko O. V., “Ice shelf response to the change in ocean temperature”, Development and application of computer techniques to environmental studies, eds. D. W. Pepper, C. A. Brebbia, P. Zanetti, WIT Press, Boston, Southampton, 1998, 281–295

[3] Hellmer H. H., Olbers D. J., “A two dimensional model for the thermohaline circulation under an ice shelf”, Antarctic Sci., 1:4 (1989), 325–336 | DOI

[4] Doronin D. P., Khesin D. E., Morskoi led, Gidrometeoizdat, L., 1975

[5] Tchijov V., Keller J., Romo S., Nagornov O., “Kinetics of phase transitions induced by shock-wave loading in ice”, Journal of Physical Chemistry B, 101:32 (1997), 6215–6218 | DOI

[6] MacAyeal D. R., “Thermohaline circulation below the Ross Ice Shelf: a consequence of tidally induced vertical mixing and basal melting”, J. Geophys. Res., 89 (1984), 597–606 | DOI

[7] Zagorodnov V. S., “Direct measurements of the position of the lower surface of the Ross Ice Shelf, Antarctica”, Data of Glaciological Studies: Chronicle Discussions, eds. Avsiuk G. A., Amerind Publishing Co., New Delhi, 1988, 248–251