본문 바로가기
KERD
논문KCI 등재

Observation of Semi-diurnal Internal Tides and Near-inertial Waves at the Shelf Break of the East China Sea

1

조회

0

다운로드

1

인용

0

참고문헌

키워드

주제분류해양학

초록

Semi-diurnal internal tides and near-inertial waves are investigated using moored current meter measurements at four sites along the shelf break of the East China Sea during August 1987 and May-June 1988. Each mooring is equipped with four current meters spanning from near surface to near bottom. Spectral analyses of all current data reveal dominant spectra at the semi-diurnal frequency band, where the upper and lower current measurements show out-of-phase relationship between them with significant coherences. These are consistent with typical characteristics of the first-mode semi-diurnal internal tide. Strong intensification of the near-bottom baroclinic currents is observed only at one site, where the ratio of the bottom slope to the slope of the internal-wave characteristics at the semi-diurnal frequency is close to unity. An energetic near-inertial wave event is observed during the first half of May-June 1988 observation at two mooring sites. Rotary spectra reveal that the most dominant signal is clockwise rotating motion at the near-inertial frequency band. Upward phase and downward energy propagations, shown in time-depth contour plots of near-inertial bandpass filtered currents, are confirmed by cross correlations between the upper- and lower-layer current measurements. The upward-propagating phase speed is estimated to be about 0.13 cm s−1 at both sites. Significant coherences and in-phase relationships of near-inertial currents at the same or similar depths between the two sites are observed in spite of their long distance of about 110 km.

Abstract

Semi-diurnal internal tides and near-inertial waves are investigated using moored current meter measurements at four sites along the shelf break of the East China Sea during August 1987 and May-June 1988. Each mooring is equipped with four current meters spanning from near surface to near bottom. Spectral analyses of all current data reveal dominant spectra at the semi-diurnal frequency band, where the upper and lower current measurements show out-of-phase relationship between them with significant coherences. These are consistent with typical characteristics of the first-mode semi-diurnal internal tide. Strong intensification of the near-bottom baroclinic currents is observed only at one site, where the ratio of the bottom slope to the slope of the internal-wave characteristics at the semi-diurnal frequency is close to unity. An energetic near-inertial wave event is observed during the first half of May-June 1988 observation at two mooring sites. Rotary spectra reveal that the most dominant signal is clockwise rotating motion at the near-inertial frequency band. Upward phase and downward energy propagations, shown in time-depth contour plots of near-inertial bandpass filtered currents, are confirmed by cross correlations between the upper- and lower-layer current measurements. The upward-propagating phase speed is estimated to be about 0.13 cm s−1 at both sites. Significant coherences and in-phase relationships of near-inertial currents at the same or similar depths between the two sites are observed in spite of their long distance of about 110 km.

참고문헌 (31)

  1. Anderson I, "Near-inertial motions off the oregon coast", J Geophys Res, 88, pp.5960~5972 (1983)
  2. Baines PG, "On internal tide generation models", Deep- Sea Res, 29, pp.307~338 (1982)
  3. Baines PG, "Internal tides, internal waves, and near inertial motions in Baroclinic processes on continental shelves", pp.19~32 (1986), American Geophysical Union
  4. Chen C, "Near-inertial oscillations over the Texas-Louisiana shelf", J Geophys Res, 101, pp.3509~3524 (1996)
  5. Choi BH, "A tidal model of the Yellow Sea and the Eastern China Sea", pp.72~ (1980), KORDI
  6. Emery WJ, "Data analysis methods in physical oceanography, 2nd edn", pp.638~ (2001), Elsevier
  7. Gonella J, "Alocal study of inertial oscillations in the upper layers of the ocean", Deep-Sea Res, 18, pp.775~788 (1971)
  8. Guo BS, "Kuroshio warm filament and source of warm water of the Tsushima Current", Proceedings of Japan China joint symposium of the cooperative study on the Kuroshio, pp.112~127 (1989)
  9. Holloway PE, "Internal tides on the australian northwest shelf: a preliminary investigation", J Phys Oceanogr, 13, pp.1357~1370 (1983)
  10. Holloway PE, "On the semidiurnal internal tide at a shelf-break region on the australian northwest shelf", J Phys Oceanogr, 14, pp.1787~1799 (1984)
  11. Holloway PE, "A comparison of semidiurnal internal tides from different bathymetric locations on the australian northwest shelf", J Phys Oceanogr, 15, pp.240~251 (1985)
  12. Huthnance JM, "Tidal currents in the northwest African upwelling region", Deep-Sea Res, 29, pp.285~306 (1982)
  13. Jacobs GA, "Inertial oscillations in the Korea Strait", J Geophys Res, 106(26), pp.943~958 (2001)
  14. Ocean circulation and material flux of the East China Sea (2nd Year) -Eastern East China Sea, "KORDI", KORDI, 378~, pp.BSCN 00278-901-1 (1996)
  15. Kundu PK, "An analysisof inertial oscillations observed near oregon coast", J Phys Oceanogr, 6, pp.879~893 (1976)
  16. Kuroda Y, "Observation of internal tides in the East China Sea with an underwater sliding vehicle", J Geophys Res, 100, pp.10801~10816 (1995)
  17. Larsen LH, "East China Sea tide currents", Cont Shelf Res, 4, pp.77~103 (1985)
  18. Leaman KD, "Observations on the vertical polarization and energy flux of near-inertial waves", J Phys Oceanogr, 6, pp.894~908 (1976)
  19. Lie HJ, "Near-inertial current oscillations off the mideast coast of Korea", Prog Oceanogr, 21, pp.241~253 (1988)
  20. Lie HJ, "Recent advances in understanding the circulation and hydrography of the East China Sea", Fish Oceanogr, 11, pp.318~328 (2002)
  21. Matsuno TT, "Small scale internal waves and turbulent fluctuations near the continental shelf break in the East China Sea", J Oceanogr, 53, pp.259~269 (1997)
  22. Millot C, "Inertial oscillations on the continental shelf of the Gulf of lions: observations and theory", J Phys Oceanogr, 11, pp.639~657 (1981)
  23. Niwa Y, "Response of the deep ocean internal wave field to traveling midlatitude storms as observed in long-term current measurements", J Geophys Res, 104, pp.10981~10989 (1999)
  24. Niwa Y, "Three-dimensional numerical simulation of M2 internal tides in the East China Sea", J Geophys Res, 109, pp.C04027~ (2004)[DOI]
  25. Munk W, "Internal wave sand small-scale process in Evolution of Physical Oceanography", pp.264~291 (1981), MIT Press
  26. Park JH, "Near-inertial oscillations interacting with mesoscale circulation in the southwestern Japan", East Sea, 2005, pp.32, L10611~
  27. Park JH, "Internal tides in the southwestern Japan", East Sea, 2006, pp.36, 22~34
  28. Park JH, "Distribution of deep near-inertial waves observed in the Kuroshio extension", J Oceanogr, 66, pp.709~717 (2010)
  29. Phillips OM, "The dynamics of the upper ocean, 2nd edn", pp.344~, Cambridge University Press
  30. Pollard RT, "On the generation by winds of inertial waves in the ocean", Deep-Sea Res, 17, pp.795~812 (1970)
  31. Song W, "A study on the source of the Tsushima warm current water", Proceedings of Japan China joint symposium of the cooperative study on the Kuroshio, pp.99~111 (1989)

관련 논문AI추천

이 간행물의 다른 논문 (8건)