Tidal variations in the cable voltage across the Korea Strait

  • Lyu, Sang-Jin (OCEAN Lab., School of Earth and Environmental Science Seoul National University) ;
  • Kim, Young-Gyu (Naval Systems R&D Center, Agency for Defense Development) ;
  • Kim, Kuh (OCEAN Lab., School of Earth and Environmental Science Seoul National University) ;
  • Book, Jeffrey W. (Naval Research Laboratory, Stennis Space Center) ;
  • Choi, Byung-Ho (Department of Civil Engineering, Sung Kyun Kwan University)
  • Published : 2002.03.01

Abstract

Cable voltage was measured simultaneously at Hamada, Japan and Pusan, Korea, using an inservice telephone cable from March to December 1990. The spectral and harmonic analyses of these data sets show that tidal signals are dominant, and that tidal constituents $M_2$ and $O_1$, which are not affected by solar geomagnetic variations, have almost the same amplitude and are of opposite phase to each other. comparing the voltage difference in 1990 with that measured using the now abandoned cable in 1998, there are dominant tidal signals at the same periods in both data sets. They have approximately the same amplitude and phase for $M_2andO_1$. The relationship between the observed voltage and the volume transport through the Korea Strait can be considered robust and stable over time. The conversion factor from voltage to transport is estimated to be $11.9{\times}10^6m^3S^{-1}volt^{-1}$ by comparing the amplitude of model-derived $M_2$ tidal transport with that of the voltage difference in 1998. This value changes to $8.6{\times}10^6m^3S^{-1}volt^{-1}$ when taking into consideration the horizontal electric current effect. This effect depends on the downstream length scale of the flow. To obtain a more reliable and stable conversion factor from voltage to transport, the voltage should be compared with observed sub-tidal transports, which may have long downstream length scales.

Keywords

References

  1. Bahk, K.S., 1991. Development ot a voltage measuring systemfor the Pusan Hamada submahne cable. J. Korean Soc. of Coastat and Ocean Engineers, 3: 255-260
  2. Book, J.W., W.J. Teague, P. Pistek, H.T. Perkins, B.-H. Choi, G.A. Jacobs, M.-S. Suk, K.-I. Chang and J.-C. Lee, 2001. Tidesin the Korea/Tsushima Strait: Observation and Model Predic-tions. Proceedings of the 11th PAMS/JECSS Workshop, Cheju,Korea, 207-210
  3. Bowden, K.F., 1956. The flow of water through the Strait ofbDover related to wind and differences in sea level. Phit.Trans. Roy. Soc. London, A, 248:517-551 https://doi.org/10.1098/rsta.1956.0008
  4. Choi, B.-H., I.K. Bang and K.H. Kim, 1994. Vertical distributionof tidal current in the Korea Strait.J. Korean Soc. of CoastaIand Ocean Engineers, 6: 421-438
  5. Choi. B.-H.. K. Kim. Y.-G. K-im and K. Kawatate. 1997. Subma-rine cable voltage measurement between Pusan and Hamadafor the years 1987-1996. Acta Oceanographica Taiwanica,36(1): 33-46
  6. Choi, B.-H., K. Kim, Y.-G. K-im, K.S. Bahk, J.O. Choi and K.Kawatate, 1992. Submarine cable measurements betweenPusan and Hamada. La mer, 30: 157-167
  7. Kang, S.K., S.-R Lee and K.-D. Yum, 1991. Tidal computation ofthe East China Sea, the Yellow Sea and the East Sea. In:Oceanography of Asian Marginal Seas, edited by K. Takano,Elsevier Oceanography Series 54: 24-48
  8. Kawatate, K.., A. Tashiro, M. Ishibashi, T. Shinozaki, T. Naga-hama, A. Kaneko, S. Mizuno, J. K.ojima, T. Aoki, T. Ishimoto,B.H. Choi, K. Kim, T. Miita and Y. Ouchi, 1991. A cross-spectral analysis of small voltage variation in a submarinecable between Hamada and Pusan with speed variation of theTsushima Warm Current. In: Oceanography of Asian MarginalSeas, edited by K. Takano, Elsevier Oceanography Series, 54:207-222 https://doi.org/10.1016/S0422-9894(08)70096-5
  9. Larsen, J.C., 1992. Transport and heat flux of the Florida Currentat 27'N derived from cross-stream voltages and profilingdata: theory and observations. Phil. Trans. R. Soc. London, A,338:169-236 https://doi.org/10.1098/rsta.1992.0007
  10. Larsen, J.C., R.L. Mackie, A. Manzella, A. Fiordelisi and S.Rieven, 1996. Robust smooth magnetotelluric transfer func-tions. Geophys. J. Int., 124: 801-819 https://doi.org/10.1111/j.1365-246X.1996.tb05639.x
  11. Longuet-Higgins, M.S., 1949. The electrical and magnetic effectof tidal streams. Mon. Not. R. Astr. Soc., 16: 285-307 https://doi.org/10.1111/j.1365-246X.1949.tb02945.x
  12. Mayer, D.A. and J.C. Larsen, 1986. Tidal transport in the floridaCurrent and Its Relationship to Tidal Heights and Cable Volt-ages. J. Phys. Oceanogr., 16: 2199-2202 https://doi.org/10.1175/1520-0485(1986)016<2199:TTITFC>2.0.CO;2
  13. Odamaki, M, 1989. Tides and tidal currents in the TsushimaStrait. J. Oceanogr. Soc. Japan, 45: 65-82 https://doi.org/10.1007/BF02108795
  14. Perkins, H.T., W.J. Teague, G.A. Jacobs, K..-I. Chang and M.-S.Suk, 2000. Currents in Korea-Tsushima Strait during Summer1999. Geophys. Res. Lett., 27: 3033-3036 https://doi.org/10.1029/2000GL011454
  15. Sanford, T.B. and R.E. Flick, 1975. On the relationship betweentransport and motional electric potentials in broad, shallowcurrents. J. Mar. Res., 33: 123-139
  16. Utada, H., Y. Hamano and T. Yukutake, 1986. A two-dimensionalconductivity model across Central Japan. J. Geomagnetismand Geoetectricity, 38: 447-473 https://doi.org/10.5636/jgg.38.447