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Original Articles

Numerical modelling of the Halten Bank area: a validation study

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Pages 113-133 | Received 02 Dec 1992, Accepted 06 Aug 1993, Published online: 15 Dec 2016

References

  • Bleck, R., Rooth, C., Hu, D. and Smith, L. T. 1992. Salinity-driven thermocline transients in a wind- and thermohaline-forced isopycnic coordinate model of the North Atlantic. J. Phys. Oceanogr. 22, 1486–1505.
  • Blumberg, A. F. and Mellor, G. L. 1987. A Description of a Three-Dimensional Coastal Ocean Circulation Model. In: Three-dimensional coastal ocean models, ed. Norman S. Heaps, Coastal Estuarine Sci. Ser., Vol. 4, AGU, Washington, DC, pp. 1–16.
  • Böning, C. W. and Budich, R. G. 1992. Eddy dynamics in a primitive equation model: Sensitivity to horizontal resolution and friction. J. Phys. Oceanogr. 22, 361–381.
  • Chassignet, E. P. 1992. Rings in numerical models of ocean general circulation: a statistical study. J. Geophys. Res. 97 (C6), 9479–9492.
  • Drijfthut, S. S. 1992. Ring genesis and the related heat transport. Part II: A model comparison. J. Phys. Oceanogr. 22, 268–285.
  • Eide, L. I. 1979. Evidence of a topographically trapped vortex on the Norwegian Continental Shelf. Deep Sea Res. 26 (6A), 601–621.
  • Engedahl, H. and Martinsen, E. A. 1988. Documentation of the two-dimensional ocean .model at DNMI. Tech. Rep. no. 67, Det norske meteorologiske institutt, Oslo, Norway.
  • Gammelsrød, T. and Hackett, B. 1981. The circulation of the Skagerrak determined by inverse methods. In: The Norwegian coastal current, vol. II, eds. R. Swtre and M. Mork, Geilo, Norway, 1980, 311–330.
  • GESAMP (IMO/FAO/UNESCO/WMO/WHO/IAEA/ UN/UNEP Joint Group of Experts on the Scientific Aspects of Marine Pollution), 1991: Coastal Modelling, GESAMP Reports and Studies No. 43, 192 pp.
  • Gjevik, B. and Straume, T. 1989. Model simulation of the M2 and K1 tide in the Nordic Seas and the Arctic Ocean. Tellus 41A, 73–96.
  • Hackett, B. and Røed, L. P. 1992. MOMOP Phase 2. Evaluation of models and influence of data assimilation (I). Evaluation of two baroclinic ocean models for the Halten Bank region. Tech. Rep. no. 49, Nansen Environmental and Remote Sensing Center, Lysaker, Norway.
  • Haugan, P. M., Evensen, G., Johannessen, J. A., Johannessen, O. M. and Petterson, L. H. 1991. Modeled and observed mesoscale circulation and wave-current refractions during the 1988 Norwegian Continental Shelf Experiment. J. Geophys. Res. 96 (C6), 10,487–10,506.
  • Hellerman, S. and Rosenstein, M. 1983. Normal Monthly Wind Stress over the World Ocean with Error Estimates. J. Phys. Oceanogr. 13, 1093–1104.
  • Huang, R. X. and Bryan, K. 1987. A multilayer model of the thermohaline and wind-driven •ocean circulation. J. Phys. Oceanogr. 17, 1090–1924.
  • Johannessen, J. A. 1991. The Norwegian continental shelf experiment prelaunch ERS 1 investigation. 1 Geophys. Res. 96 (C6), 10,409–10,410.
  • Johannessen, J. A. and Haugan, P. M. 1991. A MOMOP Study: Processing and Presentation of NORCSEX’88 Oceanographic Data. Technical Report no. 37, Nansen Environmental and Remote Sensing Center, Bergen, Norway.
  • Levitus, S. 1982. Climatological atlas of the world ocean. NOAA Prof pap. 13, US Dep. of Commerce, NOAA, Rockville, Maryland.
  • Martinsen, E. A., Røed, L. P. and Gjevik, B. 1979. A numerical model for long barotropic waves and storm surges along the western coast of Norway. J. Phys. Oceanogr. 9, 1126–1138.
  • McCartney, M. S. and Talley, L. D. 1984. Warm-to-cold water conversion in the northern North Atlantic Ocean. J. Phys. Oceanogr. 14, 922–935.
  • McCreary, J. P., Fukamachi, Y. and Kundu, P. K. 1991. A numerical investigation of jets and eddies near eastern ocean boundaries, J. Geophys. Res. 96 (C2), 2515–2534.
  • Mellor, G. L. and Yamada, T. 1982. Development of a turbulence closure model for geophysical fluid problems. Rev. Geophys. Space Phys. 20, 851–875.
  • Oey, L.-Y. and Chen, P. 1992a. A Nested-grid ocean model: With application to the simulation of meanders and eddies in the Norwegian Coastal Current. J. Geophys. Res. 97 (C12), 20,063–20,086.
  • Oey, L.-Y. and Chen, P. 1992b. A model simulation of circulation in the Northeast Atlantic shelves and seas. J. Geophys. Res. 97 (C12), 20,087–20,115.
  • Røtoed, L. P., Hackett, B. and Skåtun, H. 1989. Metocean Modeling Project (MOMOP): Final Report. Results of the model intercomparison (abridged version). Veritec Report no. 89-3312, Veritas Offshore Technology and Services A/S, Høvik, Norway, 70 p.
  • Semtner, A. J. and Chervin, R. M. 1992. Ocean general circulation from a global eddy-resolving model. J. Geophys. Res. 97 (C4), 5493–5550.
  • Slagstad, D. and Støle-Hansen, K. 1991. MetOcean MOdeling Project Phase 2. Results from SINMOD-3D. SIN TEF Report 5TF48 F91005, 57 pp.
  • Slagstad, D. 1987. A 4-Dimensional Physical Model of the Barents Sea. SINTEF Report STF 48 F87013, 34 pp.
  • Smagorinsky, J. 1963. General circulation experiments with the primitive equations. I: The basic experiment. Mon. Wea. Rev. 91, 99–164.
  • Stern, M. E. 1975. Ocean circulation physics, Int. Geoph. Ser., Vol. 19, Academic Press.
  • Thompson, J. D. and Schmitz, W. J. 1989. A limited-area model of the Gulf stream: Design, initial experiments, and model-data intercomparison. J. Phys. Oceanogr. 19, 791–814.
  • Treguier, A. M. 1992. Kinetic energy analysis of an eddy-resolving, primitive equation model of the North Atlantic. J. Geophys. Res. 97 (Cl), 687–701.