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Boundary Circulation at the Exit of the Labrador Sea

ABSTRACT

The deep circulation and related transports of the southern Labrador Sea are determined from direct current observations from ship surveys and a moored current-meter array. The measurements covered a time span from summer 1997 to 1999 and show a well-defined deep boundary current extending approximately out to the 3300-m depth contour and weak reverse currents farther offshore. The flow has a strong barotropic component, and significant baroclinic flow is only found in the shallow Labrador Current at the shelf break and associated with a deep core of Denmark Strait Overflow Water. The total deep-water transport below [sigma]^sub [Theta]^ = 27.74 kg m^sup -3^ was 26 ± 5 Sv (Sv = ...

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