North Atlantic Deep Water Formation in the Labrador Sea, Recirculation Through the Subpolar Gyre, and Discharge to the Subtropics

  • Thomas Haine
  • Claus Böning
  • Peter Brandt
  • Jürgen Fischer
  • Andreas Funk
  • Dagmar Kieke
  • Erik Kvaleberg
  • Monika Rhein
  • Martin Visbeck

North Atlantic Deep Water (NADW) is a water mass that is central to the oceanography of the deep Atlantic, the global meridional overturning circulation (MOC), and the climate of the Earth itself. The subpolar Atlantic is an especially important place for these phenomena because of the large changes wrought on NADW in these basins. Indeed, once it is discharged past 45°N, NADW temperature and salinity are altered at substantially slower rates before encountering Circumpolar Deep Waters in the subpolar ocean of the southern hemisphere (McCartney and Talley 1984; Reid et al. 1977). Formation of NADW, recirculation through the subpolar gyre, and injection into the subtropical ocean past Newfoundland are therefore central issues to ASOF science and are discussed here.


Mooring Line North Atlantic Deep Water Subpolar Gyre Labrador Current Deep Western Boundary Current 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer Science + Business Media B.V 2008

Authors and Affiliations

  • Thomas Haine
    • 1
  • Claus Böning
    • 2
  • Peter Brandt
    • 2
  • Jürgen Fischer
    • 2
  • Andreas Funk
    • 2
  • Dagmar Kieke
    • 3
  • Erik Kvaleberg
    • 1
  • Monika Rhein
    • 3
  • Martin Visbeck
    • 2
  1. 1.Department of Earth and Planetary SciencesThe Johns Hopkins UniversityBaltimoreUSA
  2. 2.IfM-GEOMARGermany
  3. 3.Institut für UmweltphysikUniversität BremenGermany

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