Abstract
A laboratory experiment is constructed to simulate the density-driven circulation under an idealized Antarctic ice shelf and to investigate the flux of dense and freshwater in and out of the ice shelf cavity. Our results confirm that the ice front can act as a dynamic barrier that partially inhibits fluid from entering or exiting the ice shelf cavity, away from two wall-trapped boundary currents. This barrier results in a density jump across the ice front and in the creation of a zonal current which runs parallel to the ice front. However despite the barrier imposed by the ice front, there is still a significant amount of exchange of water in and out of the cavity. This exchange takes place through two dense and fresh gravity plumes which are constrained to flow along the sides of the domain by the Coriolis force. The flux through the gravity plumes and strength of the dynamic barrier are shown to be sensitive to changes in the ice shelf geometry and changes in the buoyancy fluxes which drive the flow.
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References
Adrian RJ (2005) Twenty years of particle image velocimetry. Exp Fluids 39(2):159–169
Årthun M, Nicholls KW, Boehme L (2013) Wintertime water mass modification near an antarctic ice front. J Phys Oceanogr 43:359–365. doi:10.1175/JPO-D-12-0186.1
Assmann K, Hellmer H, Beckmann A (2003) Seasonal variation in circulation and water mass distribution on the Ross Sea continental shelf. Antarct Sci 15(1):3–11. doi:10.1017/S0954102003001007
Cenedese C, Whitehead JA, Ascarelli TA, Ohiwa M (2004) A dense current flowing down a sloping bottom in a rotating fluid. J Phys Oceanogr 34:188–203
Conway H, Hall BL, Denton GH, Gades AM, Waddington ED (1999) Past and future grounding-line retreat of the West Antarctic ice sheet. Science 286(5438):280–283
Cossu R, Wells Whlin MG (2004) Influence of the Coriolis force on the velocity structure of gravity currents in straight submarine channel systems. J Geophys Res 115:C11016. doi:10.1029/2010JC006208
Davey FJ (2004) Ross Sea Bathymetry. In: Institute of Geological and Nuclear Sciences Geophysical Map 16, scale 1:2,000,000, Version 1.0., Institute of Geology and Nuclear Sciences, Lower Hutt, New Zealand
Determan J, Gerdes R (1994) Melting and freezing beneath ice shelves: implications from a three-dimensional ocean-circulation model. Ann Glaciol 20:413–419
Etling D, Gelhardt F, Schrader U, Brennecke F, Kuhn G, Chabert dHieres G, Didelle H (2000) Experiments with density currents on a sloping bottom in a rotating fluid. Dyn Atmos Oceans 31:139–164
Foldvik A, Gammelsrød T, Nygaard E, Osterhus S (1983) Current measurements near Ronne Ice Shelf: implications for circulation and melting. J Geophys Res 106:4463–4477
Gordon AL, Orsi AH, Muench R, Huber BA, Zambianchi E, Visbeck M (2009) Western Ross Sea continental slope gravity currents. Deep-Sea Res. Part II 56(796–817):20. doi:10.1016/j.dsr2.2008.10.037
Greenspan HP, Howard LN (1963) On a time-dependent motion of a rotating fluid. J Fluid Mech 17:385
Griffiths RW, Hopfinger EJ (1983) Gravity currents moving along a lateral boundary in a rotating frame. J Fluid Mech 134:357–399
Griffiths RW (1986) Gravity currents in rotating systems. Ann Rev Fluid Mech 18:59–89
Grosfeld K, Gerdes R, Determann J (1997) Thermohaline circulation and interaction between ice shelf cavities and the adjacent open ocean. J Geophys Res 102(C7):15595–15610. doi:10.1029/97JC00891
Hattermann T, Nøst AK, Lilly JM, Smedsrud JM (2012) Two years of oceanic observations below the Fimbul Ice Shelf, Antarctica. Geophys Res Lett 39(L12605):1–6. doi:10.1029/2012GL051012
Hellmer HH, Olbers DJ (1989) A two-dimensional model for the thermohaline circulation under an ice shelf. Antarct Sci 1:325–336
Holland DM, Jenkins A (1999) Modeling thermodynamic iceocean interactions at the base of an ice shelf. J Phys Oceanogr 29:1787–1800
Holland DM, Jenkins A (2001) Adaptation of an isopycnic coordinate ocean model for the study of circulation beneath ice shelves. Mon Wea Rev 129:1905–1927
Holland PR, Feltham DL (2006) The effects of rotation and ice shelf topography on frazil-laden Ice Shelf Water plumes. J Phys Oceanogr 36:2312–2327
Holman JP (2002) Heat transfer. McGraw-Hill, New York
Houcine I, Vivier H, Plasari E, David R, Villermaux J (1996) Planar laser induced fluorescence technique for measurements of concentration fields in continuous stirred tank reactors. Exp Fluids 22(2):95–102
Jenkins A (1991) A one-dimensional model of ice shelf-ocean interaction. J Geophys Res Oceans 96(C11):20671–20677
Jenkins A, Dutrieux P, Jacobs S, McPhail S, Perrett J, Webb A, White D (2012) Autonomous underwater vehicle exploration of the ocean cavity beneath an Antarctic ice shelf. Oceanography 25(3):202–203. doi:10.5670/oceanog.2012.95
Killworth OD, Paldor N, Stern ME (1984) Wave propagation and growth on a surface front in a two-layer geostrophic current. J Marine Res 42:761–785
Komar PD (1969) The channelized flow of turbidity currents with application to Monterey deep-sea fan channel. J Geophys Res 74:4544–4558. doi:10.1029/JC074i018p04544
Lane-Serff G, Baines P (1998) Eddy formation by dense flows on slopes in a rotating fluid. J Fluid Mech 363:229–252
MacAyeal DR (1984) Thermohaline circulation below the Ross ice shelf: a consequence of tidally induced vertical mixing and basal melting. J Geophys Res 89:597–606
MacAyeal DR (1985) Evolution of tidally triggered meltwater plumes below ice shelves. In: Jacobs SS (ed) Oceanology of the antarctic continental shelf. American Geophysical Union, Washington
Makinson K, Schrder M, Østerhus S (2006) Effect of critical latitude and seasonal stratification on tidal current profiles along Ronne Ice Front, Antarctica. J Geophys Res 111:C03022. doi:10.1029/2005JC003062
Makinson K, Schröder M, Østerhus S (2005) Seasonal stratification and tidal current profiles along Ronne Ice Front. Frisp, Report 16
Marshall J, Plumb RA (2008) Atmosphere, ocean and climate dynamics: an introductory text, vol 93. Academic Press, pp 123–128
Mathiot P, Jourdain NC, Barnier B, Galle B, Molines JM, Le Sommer J, Penduff T (2012) Sensitivity of coastal polynyas and high-salinity shelf water production in the Ross Sea, Antarctica, to the atmospheric forcing. Ocean Dyn 62:701–723. doi:10.1007/s10236-012-0531-y
Millero FJ (1978) Freezing point of sea water: Eighth report of the Joint Panel of Oceanographic Tables and Standards. Appendix 6 UNESCO Tech Pap Mar Sci 28:29–31
Nicholls KW (1996) Temperature variability beneath Ronne Ice Shelf, Antarctica, from thermistor cables. J Phys Oceanogr 11:1199–1210
Nicholls KW, Padman L, Schröder M, Woodgate RA, Jenkins A, Østerhus S (2003) Water mass modification over the continental shelf north of Ronne Ice Shelf, Antarctica. J Geophys Res 108(C8):3260. doi:10.1029/2002JC001713
Nicholls KW, Österhus S, Makinson K (2009) Ice-Ocean processes over the continental shelf of the southern Weddell Sea, Antarctica: a review. Rev Geophys 47:RG3003. doi:10.1029/2007RG000250
Nunez-Riboni I, Fahrbach E (2010) An observation of the banded structure of the Antarctic Coastal Current at the prime meridian. Polar Res 29:322–329
Orsi AH, Smethie WM Jr, Bullister JL (2002) On the total input of Antarctic waters to the deep ocean: a preliminary estimate from chlorofluorocarbon measurements. J Geophys Res 107(C8). doi:10.1029/2001JC000976
Stern ME, Whitehead JA, Hua BL (1982) The intrusion of a density current along the coast of a rotating fluid. J Fluid Mech 123:237–266
Stern AA, Dinniman MS, Zagorodnov V, Tyler SW, Holland DM (2013) Intrusion of warm surface water beneath the McMurdo Ice Shelf, Antarctica. J Geophys Res Oceans 118:7036–7048. doi:10.1002/2013JC008842
Wahlin AK, Darelius E, Cenedese C, Lane-Serff GF (2008) Laboratory observations of enhanced entrainment in dense overflows in the presence of submarine canyons and ridges. Deep-sea Res 1(55):737–750. doi:10.1016/J.DSR.2008.02.007
Zatsepin AG, Didkovski VL, Semenov AV (1996) A self-oscillatory mechanism of inducing a vortex sloping bottom in a rotating fluid. Oceanology 38:43–50
Acknowledgments
A. Stern and D, Holland were supported from NSF grants ANT-1144504 and ANT-0732869, both from the Antarctic Integrated System Science (AISS) program of the USA National Science Foundation (NSF), as well as the Center for Sea Level Change (CSLC) of New York University Abu Dhabi Grant G1204. The technical assistance of Henri Didelle and Samuel Viboud is highly valued. The experimental campaign was supported by the European Community's Sixth Framework Programme through the Integrated Infrastructure Initiative HYDRALAB III, Contract no. 022441 (RII3).
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Stern, A.A., Holland, D.M., Holland, P.R. et al. The effect of geometry on ice shelf ocean cavity ventilation: a laboratory experiment. Exp Fluids 55, 1719 (2014). https://doi.org/10.1007/s00348-014-1719-3
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DOI: https://doi.org/10.1007/s00348-014-1719-3