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The deep basins of the Bransfield Strait (BS) are ventilated by Weddell Sea (WS) waters from different origins. Depending on the source and density, these water masses follow different routes across the complex topography near the tip of the Antarctic Peninsula and thus into the Bransfield Strait abyss.Using a global setup of the Finite Element Sea-ice Ocean Model (FESOM) we show that the WS waters...
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