Volume transport through the La-Perouse (Soya) Strait between the East Sea (Sea of Japan) and the Sea of Okhotsk

Aleksandr Vladimirovich Saveliev; Mikhail Alekseevich Danchenkov; Gi Hoon Hong

doi:10.4217/OPR.2002.24.2.147

Volume transport through the La-Perouse (Soya) Strait between the East Sea (Sea of Japan) and the Sea of Okhotsk

Aleksandr Vladimirovich Saveliev
, Mikhail Alekseevich Danchenkov^*
, Gi Hoon Hong

^*Corresponding author for this work

Far Eastern Regional Hydrometeorological Research Institute

Research output: Contribution to journal › Article › peer-review

4 Scopus citations

Abstract

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.

Original language	English
Pages (from-to)	147-152
Number of pages	6
Journal	Ocean and Polar Research
Volume	24
Issue number	2
DOIs	https://doi.org/10.4217/OPR.2002.24.2.147
State	Published - 2002
Externally published	Yes

Keywords

Multiyear variability
Sea level
The East Sea (Sea of Japan)
The La-Perouse (Soya) strait
The Sea of Okhotsk
Volume transport

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10.4217/OPR.2002.24.2.147

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title = "Volume transport through the La-Perouse (Soya) Strait between the East Sea (Sea of Japan) and the Sea of Okhotsk",

abstract = "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.",

keywords = "Multiyear variability, Sea level, The East Sea (Sea of Japan), The La-Perouse (Soya) strait, The Sea of Okhotsk, Volume transport",

author = "Saveliev, \{Aleksandr Vladimirovich\} and Danchenkov, \{Mikhail Alekseevich\} and Hong, \{Gi Hoon\}",

year = "2002",

doi = "10.4217/OPR.2002.24.2.147",

language = "英语",

volume = "24",

pages = "147--152",

journal = "Ocean and Polar Research",

issn = "1598-141X",

publisher = "Korea Ocean Research and Development Institute",

number = "2",

}

TY - JOUR

T1 - Volume transport through the La-Perouse (Soya) Strait between the East Sea (Sea of Japan) and the Sea of Okhotsk

AU - Saveliev, Aleksandr Vladimirovich

AU - Danchenkov, Mikhail Alekseevich

AU - Hong, Gi Hoon

PY - 2002

Y1 - 2002

N2 - 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.

AB - 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.

KW - Multiyear variability

KW - Sea level

KW - The East Sea (Sea of Japan)

KW - The La-Perouse (Soya) strait

KW - The Sea of Okhotsk

KW - Volume transport

UR - https://www.scopus.com/pages/publications/0036321353

U2 - 10.4217/OPR.2002.24.2.147

DO - 10.4217/OPR.2002.24.2.147

M3 - 文章

AN - SCOPUS:0036321353

SN - 1598-141X

VL - 24

SP - 147

EP - 152

JO - Ocean and Polar Research

JF - Ocean and Polar Research

IS - 2

ER -

Volume transport through the La-Perouse (Soya) Strait between the East Sea (Sea of Japan) and the Sea of Okhotsk

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Keywords

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