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Saveliev Aleksandr Vladimirovich,Danchenkov Mikhail Alekseevich,Hong Gi-Hoon Korea Institute of Ocean ScienceTechnology 2002 Ocean and Polar Research Vol.24 No.2
Seasonal and interannual variation of volume transport through the La-Perouse Strait were estimated using the difference of sea level observed at Krillion of Sakhalin, Russia, and Wakkanai of Hokkaido, Japan, during the period of 1975-1988. Historical sea level measurements between Russian and Japanese tide gauge data were normalized using an independent direct volume transport measurement. Volume transport from the East Sea (Sea of Japan) to the Sea of Okhotsk varied from -0.01 to 1.18 Sv with an annual mean value of 0.61 Sv. Monthly water transport rates showed a unimodal distribution with its maximum occurring in summer (August) and minimum in winter (December-February). The annual mean volume transport varied from 0.2 to 0.8 Sv during the period of 1975-1988 with the maximum variance of 0.6 Sv.
New findings from CREAMS Observations: Water Masses and Eddies in the East Sea
Kim, Kuh,Kim, Kyung-Ryul,Kim, Young-Gyu,Cho, Yang-Ki,Chung, Jong-Yul,Choi, Byung-Ho,Byun, Sang-Kyung,Hong, Gi-Hoon,Takematsu, Masaki,Yoon, Jong-Hwan,Volkov, Yuri,Danchenkov, Mikhail The Korean Society of Oceanography 1996 Journal of the Korean Society of Oceanography Vol.31 No.4
CREAMS (Circulation Research of the East Asian Marginal Seas) is an international research program, which began in 1993 in order to understand the water mass structure and circulation in the East Sea. Since the beginning of CREAMS, there have been four cruises in the summer and two in the winter, covering most parts of the East Sea for the first time in more than 60 years since the historical survey reported by Uda (1934). CREAMS investigations have provided many new insights into the various aspects of oceanographic problems in the East Sea such as water masses, deep sea currents and circulation, eddies, particle fluxes and so on. In this paper, we briefly review understandings before CREAMS and summarize initial new findings from CREAMS expeditions in terms of water masses and currents.