Abstract
To investigate thermodynamic currents in Antarctica, we here discuss quasi-steady density currents flowing over a regular slope and their hydrodynamic stability, considering also bottom erosion phenomena: in other words, the current is assumed to exchange sediments with the bottom. To simplify this complex problem a model of sediment evolution is assumed. As in recent work the excess mass due to the bottom erosion and deposition is assumed to depend only on the current stress on the bottom. A nonlinear equation considering both the time and space variability of these “density-turbidity” currents for a two-layer model is obtained and a novel criterion to identify the “ignition” point of these density-turbidity currents is discussed. In Polar Oceans these interactions can play a fundamental role in the generation of new water masses, as a result of violent hydrodynamic instability concerning the downslope motion of dense shelf water along submarine canyons.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
References
Cavalieri DJ, Martin S (1994) The contributions of Alaskan, Siberian, and Canadian coastal polynyas to the cold halocline layer of the Arctic Ocean. J Geophys Res 99 (18): 343–362
Caserta A, Mieli E, Salusti E (1990) On a model of bottom erosion by dense water steady veins. Geophys Astrophys Fluid Dyn 55: 117–135
Salusti E (1996) A new model for marine density-turbidity currents with criteria for ignition. Geophys Astrophys Fluid Dyn 83: 233–260
Nansen F (1906) Northern waters: Captain Roald Amundsen’s oceanographic observations in the Arctic Seas in 1901. Skr Nor Vidensk Akad Kl 1 Mat Naturvidensk K1 3: 145
Gardner WD (1989) Periodic resupension in Baltimore canyon by focusing of internal waves. J Geophys Res 94, C12: 18185–18194
Bignami F, Salusti E, Schiarini S (1990) Observations on a bottom vein of dense water in the Southern Adriatic and Jonian Seas. J Geophys Res 95: 7249–7259
Chapman DC, Gawarkiewicz G (1995) Offshore transport of dense shelf water in the presence of a submarine canyon. J Geophys Res 100, C7: 13373–13387
Jiang L, Garwood RW Jr (1996) Three-dimensional simulations of overflows on continental slopes J Phys Ocean 26: 1214–1233
Sugimoto T, Whitehead JA (1983) Laboratory models for bay-type continental shelves in the winter. J Phys Ocean 13, 1819–1828
Quadfasel D, Rudels B, Kurz K (1988) Outflow of dense water from a Svalbard fjord into the Fram strait. Deep Sea Res 35: 1143–1150
Garrison GR, Becker P (1976) The Barrow submarine canyon: a drain for the Chukchi sea. J Geophys Res 81: 4445–4453
Ellison TH, Turner JS (1959) Turbulent entrainment in stratified flows. J Fluid Mech 6: 432–448
Simpson JE (1982) Gravity currents in the laboratory. Atmos Ocean Anny Rev Fluid Mech 14: 213–234
Simpson JE (1982) Gravity currents in the laboratory. Atmos Ocean Anny Rev Fluid Mech 14: 213–234
Drake DE, Cacchione DA (1986) Field observations of bed shear stress and sediment resuspension on continental shelves, Alaska and California. Cont Shelf Res 6: 415–429
Parker G, Fukushima Y, Pantin HM (1986) Self accelerating turbidity currents. J Fluid Mech 171: 145–181
Stacey MW, Bowen JA (1988a) The vertical structure of density and turbidity currents: theory and observation. J Geophys Res 93: 3528–3542
Stacey MW, Bowen JA (1988b) The vertical structure of turbidity currents and a necessary condition for self-maintenance. J Geophys Res 93: 3543–3553
Seymour R (1986) Near shore autosuspending turbidity flows. Ocean Eng 13, 5: 435–447
Bagnold RA (1977) Mechanism of marine sedimentation. The Sea. Wiley, Interscience, New York, vol 3, 507–528
Plapp JE, Mitchell JP (1960) A hydrodynamic theory of turbidity currents. J Geophys Res 65: 983–992
Yih CS (1963) Stability of liquid flow down an inclined plane. Phys Fluid 6: 321–334
Jacobs SS, Comiso JC (1989) Sea ice and oceanic processes on the Ross Sea continental shelf. J Geophys Res 94, C12: 18195–18211
Jacobs S, Giulivi CF (1998) Thermohaline data and ocean circulation on the Ross Sea continental shelf (This Volume)
Gouretski V (1998) The large-scale thermohaline structure of the Ross Sea (This Volume)
Whitham GB (1974) Linear and nonlinear waves Wiley, New York, pp 636
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1999 Springer-Verlag Italia, Milano
About this paper
Cite this paper
Gremes Cordero, S., Salusti, E. (1999). General Characteristics of Density-Turbidity Currents in the Ross Sea (Antarctica). In: Spezie, G., Manzella, G.M.R. (eds) Oceanography of the Ross Sea Antarctica . Springer, Milano. https://doi.org/10.1007/978-88-470-2250-8_15
Download citation
DOI: https://doi.org/10.1007/978-88-470-2250-8_15
Publisher Name: Springer, Milano
Print ISBN: 978-88-470-2252-2
Online ISBN: 978-88-470-2250-8
eBook Packages: Springer Book Archive