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ADCP-referenced geostrophic velocity and transport in the West Spitsbergen Current

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
During the summer of 2000 and 2002 (June-July) the West Spitsbergen Current (WSC) was investigated by the Institute of Oceanology, Polish Academy of Sciences. CTD and current measurements by a vessel-mounted Acoustic Doppler Current Profiler (ADCP) were performed along three transects perpendicular to the WSC main stream and covering the region from 76°30' N to 78°20' N and from 02°30' E to 15° E. In general, the geostrophic, baroclinic flow patterns and the ADCP-measured currents were found to be in good agreement but measured current velocities were significantly higher than calculated values. This fact supports earlier observations that the barotropic component is dominant in the WSC. Since ADCP has a better spatial resolution than CTD records, the West Spitsbergen Current could be investigated and described in much greater detail than before. The main stream of Atlantic Water is topographically steered by the continental slope (isobars 800-2000 m) and the complex, multistream structure of the West Spitsbergen Current is clearly visible. The absolutely referenced total geostrophic transport is about three times higher than the estimated value assuming the level of no motion lies at 1000 m.
Czasopismo
Rocznik
Strony
425--435
Opis fizyczny
Bibliogr. 12 poz., mapa, tab., wykr.
Twórcy
autor
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland
autor
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland
autor
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland
Bibliografia
  • [1] Aagaard K., Darnall C., Greisman P., 1973, Year-long current measurements in the Greenland-Spitsbergen passage, Deep-Sea Res., 20, 743-746.
  • [2] Aagaard K., Swift J. H., Carmack E. C., 1985, Thermohaline circulation in the Arctic mediterranean seas, J. Geophys. Res., 90, 4833-4846.
  • [3] Cokelet E. D., Schall M. L., Dougherty D. M., 1996, ADCP-referenced geostrophic circulation in the Bering Sea basin, J. Phys. Oceanogr., 26, 1113-1127.
  • [4] Fahrbach E., Meincke J., Österhus S., Rohardt G., Schauer U., Tverberg V., Verduin J., 2001, Direct measurements of volume transports through Fram Strait, Polar Res., 20 (2), 217-224.
  • [5] Gill A. E., 1982, Atmosphere-ocean dynamics, Acad. Press, New York, 662 pp.
  • [6] Hopkins T. S., 1991, The GIN Sea-A synthesis of its physical oceanography and literature review 1972-1985, Earth Sci. Rev., 30, 175-318.
  • [7] Meinen C. S., Watts D. R., Clarke R. A., 2000, Absolutely referenced geostrophic velocity and transport on a section across the North Atlantic Current, Deep-Sea Res., 47, 309-322.
  • [8] Osiński R., 2000, The misalignment angle in vessel-mounted ADCP, Oceanologia, 42 (3), 385-394.
  • [9] Pickart R. S., Lindstrom S. S., 1994, A comparison of techniques for referencing geostrophic velocities, J. Atmos. Ocean. Technol., 11, 814-824.
  • [10] Pollard R., Read J., 1989, A method for calibrating shipmounted Acoustic Doppler Profilers, and the limitations of gyro compasses, J. Atmos. Ocean. Technol., 6, 859-865.
  • [11] Pond S., Pickard G. L., 1978, Introductory dynamical oceanography, Pergamon Press, Oxford, 241 pp.
  • [12] Woodgate R. A., Schauer U., Fahrbach E., 1998, Moored current meters in Fram Strait at 79° N: Preliminary results with special emphasis on the West Spitsbergen Current, Ber. Fachber. Phys., 1, 1-25.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0013-0074
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