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Near-ubiquity of ice-edge blooms in the Arctic

Near-ubiquity of ice-edge blooms in the Arctic
Near-ubiquity of ice-edge blooms in the Arctic
Ice-edge blooms are significant features of Arctic primary production, yet have received relatively little attention. Here we combine satellite ocean colour and sea-ice data in a pan-Arctic study. Ice-edge blooms occur in all seasonally ice-covered areas and from spring to late summer, being observed in 77–89% of locations for which adequate data exist, and usually peaking within 20 days of ice retreat. They sometimes form long belts along the ice-edge (greater than 100 km), although smaller structures were also found. The bloom peak is on average more than 1 mg m?3, with major blooms more than 10 mg m?3, and is usually located close to the ice-edge, though not always. Some propagate behind the receding ice-edge over hundreds of kilometres and over several months, while others remain stationary. The strong connection between ice retreat and productivity suggests that the ongoing changes in Arctic sea-ice may have a significant impact on higher trophic levels and local fish stocks.
1726-4170
515-524
Perrette, M.
6f40217b-11c2-42b2-b3fe-cc6410eca1df
Yool, A.
882aeb0d-dda0-405e-844c-65b68cce5017
Quartly, G.D.
3d1e4e87-f001-4d18-b95f-9bca4db6ff9d
Popova, E.E.
3ea572bd-f37d-4777-894b-b0d86f735820
Perrette, M.
6f40217b-11c2-42b2-b3fe-cc6410eca1df
Yool, A.
882aeb0d-dda0-405e-844c-65b68cce5017
Quartly, G.D.
3d1e4e87-f001-4d18-b95f-9bca4db6ff9d
Popova, E.E.
3ea572bd-f37d-4777-894b-b0d86f735820

Perrette, M., Yool, A., Quartly, G.D. and Popova, E.E. (2011) Near-ubiquity of ice-edge blooms in the Arctic. Biogeosciences, 8 (2), 515-524. (doi:10.5194/bg-8-515-2011).

Record type: Article

Abstract

Ice-edge blooms are significant features of Arctic primary production, yet have received relatively little attention. Here we combine satellite ocean colour and sea-ice data in a pan-Arctic study. Ice-edge blooms occur in all seasonally ice-covered areas and from spring to late summer, being observed in 77–89% of locations for which adequate data exist, and usually peaking within 20 days of ice retreat. They sometimes form long belts along the ice-edge (greater than 100 km), although smaller structures were also found. The bloom peak is on average more than 1 mg m?3, with major blooms more than 10 mg m?3, and is usually located close to the ice-edge, though not always. Some propagate behind the receding ice-edge over hundreds of kilometres and over several months, while others remain stationary. The strong connection between ice retreat and productivity suggests that the ongoing changes in Arctic sea-ice may have a significant impact on higher trophic levels and local fish stocks.

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More information

Published date: 2011
Organisations: Marine Systems Modelling, Marine Physics and Ocean Climate

Identifiers

Local EPrints ID: 207397
URI: http://eprints.soton.ac.uk/id/eprint/207397
ISSN: 1726-4170
PURE UUID: ffdcd156-8473-4f80-b7d7-cf526ce8c6e6

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Date deposited: 09 Jan 2012 16:56
Last modified: 14 Mar 2024 04:39

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Contributors

Author: M. Perrette
Author: A. Yool
Author: G.D. Quartly
Author: E.E. Popova

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