2009
DOI: 10.1016/j.dsr.2009.07.008
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Physical controls and mesoscale variability in the Labrador Sea spring phytoplankton bloom observed by Seaglider

Abstract: We investigate the 2005 spring phytoplankton bloom in the Labrador Sea using a Seaglider equipped with hydrographic, bio-optical and oxygen sensors. The Labrador Sea blooms in distinct phases, two of which were observed by Seaglider: the north bloom and the central Labrador

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Cited by 61 publications
(42 citation statements)
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“…The influence of upwelling has also been documented in temperature and salinity observations along the sea ice margin off the Newfoundland coast49. Recent observations indicate that upwelling of nutrients and downwelling of biomass occurs at the Labrador shelf-break front50, the watermass boundary which separates the inshore branch of the Labrador Current on the shelf from the central Labrador Sea and the deep boundary current.…”
Section: Discussionmentioning
confidence: 87%
“…The influence of upwelling has also been documented in temperature and salinity observations along the sea ice margin off the Newfoundland coast49. Recent observations indicate that upwelling of nutrients and downwelling of biomass occurs at the Labrador shelf-break front50, the watermass boundary which separates the inshore branch of the Labrador Current on the shelf from the central Labrador Sea and the deep boundary current.…”
Section: Discussionmentioning
confidence: 87%
“…A third explanation for our results and those of McGillicuddy et al (2003) could be that eddies in this region do not supply additional nutrients, but rather aid in the haline stratification of the region, since these eddies tend to be fresh at the surface (Frajka-Williams et al, 2009).…”
Section: Discussionmentioning
confidence: 88%
“…For example, isopycnal shoaling caused by eddies drove the production observed by gliders in the subtropical North Pacific (Nicholson et al 2008). Frajka-Williams et al (2009) used gliders to determine that the spring bloom in the Labrador Sea is associated with eddies and fronts. A glider was used to investigate the distribution of biogeochemical variables in a warm-core eddy off Australia (Baird et al 2011).…”
Section: The Mesoscale and Submesoscalementioning
confidence: 99%