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- W2043796519 abstract "Abstract Two climatologies, one using an isopycnic approach and the other employing a more classical geopotential approach, are produced for the Labrador Sea region. These differ from existing climatologies through the use of smaller search radii, more data and a carefully chosen depth dependent correction scheme. This results in the preservation of the strong fronts that exist between cold, fresh boundary currents and warmer, more saline interior waters and, in general, less smoothing of features. The waters of the West Greenland Current, the Labrador Current and the interior are well represented, especially Labrador Sea Water and the Deep Western Boundary Current. We consider that our ‘best’ results are produced by the isopycnal climatology. Isopycnal averaging gives more realistic results by reducing artificial mixing of water properties and preserving the baroclinicity of the flow. We estimate the total transport, using the results from the isopycnal climatology in a diagnostic model driven by climatological winds. For the Labrador Current/subpolar gyre at 53°N we find a transport of 46.6 Sv southward, with 9.7 Sv of that being Labrador Sea Water, 12.1 Sv being Gibbs Fracture Zone Water and 8.0 Sv being Denmark Strait Overflow Water. Transport into the Labrador Sea is 41.2 Sv with 6.6 Sv of Labrador Sea Water exported back to the Irminger Sea. Total southward freshwater transport by the Labrador Current (including slope and ‘gyre’ branches) is 239 mSv at 53°N, with almost 60% of this carried in the upper layer. Import of fresh water to the Labrador Sea from the east in the East Greenland Current is 129 mSv, which is divided almost equally among all layers. Our estimate of the long‐term mean formation rate of Labrador Sea Water is between 3.6 and 3.8 Sv." @default.
- W2043796519 created "2016-06-24" @default.
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- W2043796519 date "2009-03-01" @default.
- W2043796519 modified "2023-10-18" @default.
- W2043796519 title "Comparing two climatologies of the Labrador Sea: Geopotential and isopycnal" @default.
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- W2043796519 doi "https://doi.org/10.3137/oc281.2009" @default.
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