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- W330836223 abstract "Following the approach used in earlier studies, we first determined that the DWBC (σ0 >27.80) baroclinic transport (TBC) referenced to 1000 m depth increased by ∼2 Sv between the mid-1990s (1994–1997) and 2000s (2000– 2007). In the next step, we quantified velocity changes at the reference level (1000 m) by combining estimates of the hydrography-derived velocity changes in the water column and the altimetry-derived velocity changes at the sea surface. The inferred increase in the southward velocity at 1000 m above the DWBC in 1994–2007 indicates that the increase in the DWBC absolute transport was larger than the 2-Sv increase in the DWBC TBC . This result and the observed coherence of the DWBC absolute and baroclinic transport changes between individual observations imply that the DWBC absolute transport variability in the region is underestimated but qualitatively well represented by its baroclinic component on decadal and shorter time scales." @default.
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- W330836223 date "2010-05-01" @default.
- W330836223 modified "2023-09-27" @default.
- W330836223 title "The Deep Western Boundary Current southeast of Cape Farewell, Greenland: decadal transport variability from repeat hydrography and satellite altimetry" @default.
- W330836223 hasPublicationYear "2010" @default.
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