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OHSHIMA KAY I
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Circulation and Heat/Salt Transpo吋inthe Sea of Okhotsk and Its Relation to Sea I...
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Lagrangian modelling of frazil ice in the ocean
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Particle tracking experiment on a model of the Okhotsk Sea: spreading of the Amu...
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Weakened overturning and tide control the properties of Oyashio Intermediate Wat...
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Weakened overturning and tide control the properties of Oyashio Intermediate Wat...
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Weakened overturning and tide control the properties of Oyashio Intermediate Wat...
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Particle tracking experiments on a model of the Okhotsk Sea: Toward oil spill si...
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Circumpolar Mapping of Antarctic Coastal Polynyas and Landfast Sea Ice: Relation...
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Ice‐band characteristics of the Antarctic seasonal ice zone observed using MOS M...
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Coherent sea level variation in and around the Sea of Okhotsk
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Driving the Ocean “Pump”—Formation of Dense Water in the Antarctic
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Numerical model studies on the generation and dissipation of the diurnal coastal...
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DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNIN...
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What determines the maximum sea ice extent in the Sea of Okhotsk? Importance of...
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Warming and oxygen decrease of intermediate water in the northwestern North Paci...
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Influence of Current Width Variation on the Annual Mean Transport of the East Sa...
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Enhancement of Sea Ice Drift due to the Dynamical Interaction between Sea Ice an...
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Sea-ice retreat in the Sea of Okhotsk and the ice–ocean albedo feedback effect o...
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Global view of sea-ice production in polynyas and its linkage to dense/bottom wa...
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Two-layer model of wind-driven circulation in the Antarctic Ocean
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