Dynamics of circulation of the Japan Sea

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ID: 296694
1995
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Abstract
Including mean flow forcing due to eddy-topography interaction in a numerical model of the Japan Sea appears to improve defects identified in previous modelling studies. Characteristic western boundary current overshoot (by the East Korea Warm Current) is reduced or eliminated while a southward undercurrent brings colder, fresher water along the Korean coast. Cyclonic circulation in the north includes a strengthened Liman Current. A more nearly continuous Nearshore Branch follows the Honshu shelf break with northward-flowing undercurrent. Interannual variability persists under fixed (seasonally repeating or annual mean) external forcing.
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openalex_W2008713698 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Greg Holloway, Tessa Sou, Michael Eby
Journal journal of marine research
Year 1995
DOI
10.1357/0022240953213106
URL
https://doi.org/10.1357/0022240953213106
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