Izvestiya, Atmospheric and Oceanic Physics

, Volume 54, Issue 9, pp 1050–1056 | Cite as

Peculiarities of Water Circulation in the Southern Tatar Strait

  • A. G. AndreevEmail author


Satellite altimetry data have been used to study water circulation in the Tatar Strait region (the northern part of the Sea of Japan) for the time period from 1993 to 2015. Seasonal and interannual variations in current velocities in the southern Tatar Strait (46°–50° N) have been found to be determined by the difference in sea level (SL) between the Korea Strait in the southern part of the Sea of Japan (Hakata station) and the northern point of the Hokkaido Island (Wakkanai station) (SLHakata–SLWakkanai). With increases in (SLHakata–SLWakkanai), the flow of the Tsushima Current into the Tatar Strait increases, the southward flow of the Primorye Current along the western boundary of the Tartar Strait decreases, and the southward flow of the West Sakhalin Current along the eastern boundary of the Tartar Strait increases. The decreased (SLHakata–SLWakkanai) leads to the formation of cyclonic water circulation in the Tatar Strait, a change in direction of the West Sakhalin Current from southward to northward, and an increase in the southwestward water transport by the Primorye Current. An increase in (SLHakata–SLWakkanai) accompanied by increased water flow through the Korea Strait leads to an increase in seawater temperatures in the northern part of the Sea of Japan.


satellite altimetry water circulation Sea of Japan Primorye Current West Sakhalin Current 



This study was supported by the Russian Science Foundation, project no. 16-17-10025.


  1. 1.
    Ablain, M., Cazenave, A., Larnicol, G., et al., Improved sea level record over the satellite altimetry era (1993–2010) from the climate change initiative project, Ocean Sci., 2015, vol. 11, pp. 67–82.CrossRefGoogle Scholar
  2. 2.
    Andreev, A.G., Interannual variations of sea water parameters and chlorophyll a concentration in the Japan Sea in autumn, Russ. Meteorol. Hydrol., 2014, vol. 39, no. 8, pp. 542–549.CrossRefGoogle Scholar
  3. 3.
    Cho, Y.-K., Seo, G.-H., Choi, B.-J., et al., Connectivity among straits of the northwest Pacific marginal seas, J. Geophys. Res., 2009, vol. 114, C06018. doi 10.1029/ 2008JC005218Google Scholar
  4. 4.
    Fukudome, K.-I., Yoon, J.-H., Ostrovskii, A., et al., Seasonal volume transport variation in the Tsushima Warm Current through the Tsushima Straits from 10 years of ADCP observations, J. Oceanogr., 2010, vol. 66, pp. 539–551.CrossRefGoogle Scholar
  5. 5.
    Kim, T.-K. and Yoon, J.-H., Seasonal variation of upper layer circulation in the northern part of the East/Japan Sea, Cont. Shelf Res., 2010, vol. 30, pp. 1283–1301.CrossRefGoogle Scholar
  6. 6.
    Ohshima, K., The flow system in the Japan Sea caused by a sea level difference through the shallow straits, J. Geophys. Res., 1994, vol. 99, pp. 9925–9940.CrossRefGoogle Scholar
  7. 7.
    Onishi, M. and Ohtani, K., Volume transport of the Tsushima Warm Current, west of Tsugaru Strait bifurcation area, J. Oceanogr., 1997, vol. 53, pp. 27–34.CrossRefGoogle Scholar
  8. 8.
    Pishchal’nik, V.M., Arkhipkin, V.S., Yurasov, G.I., and Ermolenko, S.S., Seasonal variations in water circulation in coastal areas of Sakhalin Island, Meteorol. Gidrol., 2003, no. 5, pp. 87–94.Google Scholar
  9. 9.
    Shevchenko, G.V. and Chastikov, V.N., Seasonal and interannual variations of oceanographic conditions in the southern Tatar Strait, Russ. Meteorol. Hydrol., 2006, vol. 31, no. 3, pp. 65–78.Google Scholar
  10. 10.
    Shevchenko, G.V., Sedaeva, O.S., Romanov, A.A., and Vilyanskaya, E.A., Seasonal sea level fluctuations in the Tatar Strait according to satellite altimetry, Issled. Zemli Kosmosa, 2007, no. 3, pp. 59–72.Google Scholar
  11. 11.
    Velikanov, A.Ya., Migration of the Far Eastern sardine Sardinops melanostictus to the Sakhalin Island shores in the 20th and early 21st centuries, Vopr. Ikhtiol., 2016, vol. 56, pp. 548–561.Google Scholar
  12. 12.
    Velikanov, A.Ya. and Buslov, A.V., Another occurrence of the Far Eastern sardine Sardinops melanostictus (Clupeidae) near the western coast of Sakhalin, Izv. TINRO, 2012, vol. 171, pp. 62–68.Google Scholar
  13. 13.
    Yarichin, V.G., Some features of the horizontal water motion in the Sea of Japan north of 40 N, Tr. Dal’nevost. Nauchno-Issled. Gidrometeorol. Inst., 1982, no. 96, pp. 111–120.Google Scholar
  14. 14.
    Yurasov, G.I. and Yarichin, V.G., Techeniya Yaponskogo morya (The Currents of the Sea of Japan), Vladivostok: TOI DVO RAN, 1991.Google Scholar

Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  1. 1.V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of SciencesVladivostokRussia

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