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Preprints
https://doi.org/10.5194/osd-6-2085-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/osd-6-2085-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  11 Sep 2009

11 Sep 2009

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This preprint was under review for the journal OS. A revision for further review has not been submitted.

Upper Labrador Sea Water in the Irminger Sea during a weak convection period (2002–2006)

E. Louarn1,*, H. Mercier3, P. Morin1,2, E. de Boisseson3, and S. Bacon4 E. Louarn et al.
  • 1Laboratoire de Chimie Marine, Institut Universitaire Européen de la Mer, Plouzané, France
  • 2UMR CNRS UPMC 7144, Station Biologique de Roscoff, Place Georgers Teissier, Roscoff, France
  • 3Laboratoire de Physique des Océans, CNRS Ifremer IRD UBO, Ifremer centre de Brest, Plouzané, France
  • 4National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, Southampton, UK
  • *now at: Laboratoire de Chimie Physique, Université Paris Sud XI, Orsay, France

Abstract. Four cruises between 2002 and 2006 sampled physical and chemical tracers in the southern Irminger Sea during the period of weak convection in the North Atlantic Subpolar Gyre. The upper Labrador Sea Water (uLSW) shows complex and time variable patterns reflecting different formation sites: Irminger Sea, South Greenland and Labrador Sea.

E. Louarn et al.

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Status: closed (peer review stopped)
Status: closed (peer review stopped)
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E. Louarn et al.

E. Louarn et al.

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