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Observations of pigment and particle distributions in the western North Atlantic from an autonomous float and ocean color satellite
Citation
Boss, E and Swift, D and Taylor, L and Brickley, P and Zaneveld, R and Riser, S and Perry, MJ and Strutton, PG, Observations of pigment and particle distributions in the western North Atlantic from an autonomous float and ocean color satellite, Limnology and Oceanography, 53, (5, part 2) pp. 2112-2122. ISSN 0024-3590 (2008) [Refereed Article]
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Copyright Statement
Copyright 2008 American Society of Limnology and Oceanography
DOI: doi:10.4319/lo.2008.53.5_part_2.2112
Abstract
Profiling floats with optical sensors can provide important complementary data to satellite ocean color
determinations by providing information about the vertical structure of ocean waters, as well as surface waters
obscured by clouds. Here we demonstrate this ability by pairing satellite ocean color data with records from a
profiling float that obtained continuous, high-quality optical data for 3 yr in the North Atlantic Ocean. Good
agreement was found between satellite and float data, and the relationship between satellite chlorophyll and floatderived
particulate backscattering was consistent with previously published data. Upper ocean biogeochemical
dynamics were evidenced in float measurements, which displayed strong seasonal patterns associated with
phytoplankton blooms, and depth and seasonal patterns associated with an increase in pigmentation per particle
at low light. Surface optical variables had shorter decorrelation timescales than did physical variables (unlike at
low latitudes), suggesting that biogeochemical rather than physical processes controlled much of the observed
variability. After 2.25 yr in the subpolar North Atlantic between Newfoundland and Greenland, the float crossed
the North Atlantic Current to warmer waters, where it sampled an unusual eddy for 3 months. This anticyclonic
feature contained elevated particulate material from surface to 1000-m depth and was the only such event in the
float’s record. This eddy was associated with weakly elevated surface pigment and backscattering, but depthintegrated
backscattering was similar to that previously observed during spring blooms. Such seldom-observed
eddies, if frequent, are likely to make an important contribution to the delivery of particles to depth.
Item Details
Item Type: | Refereed Article |
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Keywords: | labrador sea, bio-optical oceanography |
Research Division: | Earth Sciences |
Research Group: | Oceanography |
Research Field: | Biological oceanography |
Objective Division: | Expanding Knowledge |
Objective Group: | Expanding knowledge |
Objective Field: | Expanding knowledge in the earth sciences |
UTAS Author: | Strutton, PG (Professor Peter Strutton) |
ID Code: | 80203 |
Year Published: | 2008 |
Web of Science® Times Cited: | 97 |
Deposited By: | IMAS Research and Education Centre |
Deposited On: | 2012-10-24 |
Last Modified: | 2012-11-06 |
Downloads: | 7 View Download Statistics |
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