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contributor authorChanut, Jérôme
contributor authorBarnier, Bernard
contributor authorLarge, William
contributor authorDebreu, Laurent
contributor authorPenduff, Thierry
contributor authorMolines, Jean Marc
contributor authorMathiot, Pierre
date accessioned2017-06-09T16:24:55Z
date available2017-06-09T16:24:55Z
date copyright2008/08/01
date issued2008
identifier issn0022-3670
identifier otherams-67443.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208891
description abstractThe cycle of open ocean deep convection in the Labrador Sea is studied in a realistic, high-resolution (4 km) regional model, embedded in a coarser (?°) North Atlantic setup. This configuration allows the simultaneous generation and evolution of three different eddy types that are distinguished by their source region, generation mechanism, and dynamics. Very energetic Irminger Rings (IRs) are generated by barotropic instability of the West Greenland and Irminger Currents (WGC/IC) off Cape Desolation and are characterized by a warm, salty subsurface core. They densely populate the basin north of 58°N, where their eddy kinetic energy (EKE) matches the signal observed by satellite altimetry. Significant levels of EKE are also found offshore of the West Greenland and Labrador coasts, where boundary current eddies (BCEs) are spawned by weakly energetic instabilities all along the boundary current system (BCS). Baroclinic instability of the steep isopycnal slopes that result from a deep convective overturning event produces convective eddies (CEs) of 20?30 km in diameter, as observed and produced in more idealized models, with a distinct seasonal cycle of EKE peaking in April. Sensitivity experiments show that each of these eddy types plays a distinct role in the heat budget of the central Labrador Sea, hence in the convection cycle. As observed in nature, deep convective mixing is limited to areas where adequate preconditioning can occur, that is, to a small region in the southwestern quadrant of the central basin. To the east, west, and south, BCEs flux heat from the BCS at a rate sufficient to counteract air?sea buoyancy loss. To the north, this eddy flux alone is not enough, but when combined with the effects of Irminger Rings, preconditioning is effectively inhibited here too. Following a deep convective mixing event, the homogeneous convection patch reaches as deep as 2000 m and a horizontal scale on the order of 200 km, as has been observed. Both CEs and BCEs are found to play critical roles in the lateral mixing phase, when the patch restratifies and transforms into Labrador Sea Water (LSW). BCEs extract the necessary heat from the BCS and transport it to the deep convection site, where it fluxed into convective patches by CEs during the initial phase. Later in the phase, BCE heat flux maintains and strengthens the restratification throughout the column, while solar heating establishes a near-surface seasonal stratification. In contrast, IRs appear to rarely enter the deep convection region. However, by virtue of their control on the surface area preconditioned for deep convection and the interannual variability of the associated barotropic instability, they could have an important role in the variability of LSW.
publisherAmerican Meteorological Society
titleMesoscale Eddies in the Labrador Sea and Their Contribution to Convection and Restratification
typeJournal Paper
journal volume38
journal issue8
journal titleJournal of Physical Oceanography
identifier doi10.1175/2008JPO3485.1
journal fristpage1617
journal lastpage1643
treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 008
contenttypeFulltext


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