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Long-term variability of downward particle flux in the deep northeast Atlantic: Causes and trends

Long-term variability of downward particle flux in the deep northeast Atlantic: Causes and trends
Long-term variability of downward particle flux in the deep northeast Atlantic: Causes and trends
At 3000 m depth the downward flux of particulate matter shows substantial seasonal and interannual variation. Complete annual records for eight of the past 14 years have been examined in the light of mixing depths derived from the OCCAM general circulation model and euphotic zone chlorophyll concentration and productivity, which were derived from the SeaWiFS satellite colour sensor. The annual flux was particularly high in 2001 due to a late summer deposition exceeding previous records several fold and this year was also characterised by very early shoaling of the mixing depth in spring and a very high surface spring chlorophyll concentration. Other years that were somewhat unusual in having either high or low flux at depth were not in general associated with unusual patterns of mixing or productivity. The percentage of the annual organic carbon primary production which reaches 3000 m varies from 0.6 to 1.2% except in 2001 when it reached 3.4%. A mechanistic relationship between upper-ocean processes and deep-ocean particle flux remains elusive and various explanations are suggested for this which need now to be addressed. In the spring, the timing of first shoaling of mixing, enhancement of productivity and increased particle flux at depth have all advanced during the 14 years of study by about 2 days per year, suggesting a similar trend as has been observed for surface phytoplankton, mesozooplankton, fish and seabirds probably caused by wide-scale environmental changes.
0967-0645
1346-1361
Lampitt, R.S.
dfc3785c-fc7d-41fa-89ee-d0c6e27503ad
Salter, I.
805cba99-e754-417b-aac1-cee3a259aced
de Cuevas, B.A.
01cc697c-2832-4de6-87bf-bf9f16c1f906
Hartman, S.
2f74a439-395a-4ee7-89a2-eff4cc8d9481
Larkin, K.E.
f359bbaa-8a50-4972-9a01-2a9d4c428ba6
Pebody, C.A.
2aa9ccad-ac79-4ad2-b367-aba3dfc94a53
Lampitt, R.S.
dfc3785c-fc7d-41fa-89ee-d0c6e27503ad
Salter, I.
805cba99-e754-417b-aac1-cee3a259aced
de Cuevas, B.A.
01cc697c-2832-4de6-87bf-bf9f16c1f906
Hartman, S.
2f74a439-395a-4ee7-89a2-eff4cc8d9481
Larkin, K.E.
f359bbaa-8a50-4972-9a01-2a9d4c428ba6
Pebody, C.A.
2aa9ccad-ac79-4ad2-b367-aba3dfc94a53

Lampitt, R.S., Salter, I., de Cuevas, B.A., Hartman, S., Larkin, K.E. and Pebody, C.A. (2010) Long-term variability of downward particle flux in the deep northeast Atlantic: Causes and trends. [in special issue: Water Column and Seabed Studies at the PAP Sustained Observatory in the Northeast Atlantic] Deep Sea Research Part II: Topical Studies in Oceanography, 57 (15), 1346-1361. (doi:10.1016/j.dsr2.2010.01.011).

Record type: Article

Abstract

At 3000 m depth the downward flux of particulate matter shows substantial seasonal and interannual variation. Complete annual records for eight of the past 14 years have been examined in the light of mixing depths derived from the OCCAM general circulation model and euphotic zone chlorophyll concentration and productivity, which were derived from the SeaWiFS satellite colour sensor. The annual flux was particularly high in 2001 due to a late summer deposition exceeding previous records several fold and this year was also characterised by very early shoaling of the mixing depth in spring and a very high surface spring chlorophyll concentration. Other years that were somewhat unusual in having either high or low flux at depth were not in general associated with unusual patterns of mixing or productivity. The percentage of the annual organic carbon primary production which reaches 3000 m varies from 0.6 to 1.2% except in 2001 when it reached 3.4%. A mechanistic relationship between upper-ocean processes and deep-ocean particle flux remains elusive and various explanations are suggested for this which need now to be addressed. In the spring, the timing of first shoaling of mixing, enhancement of productivity and increased particle flux at depth have all advanced during the 14 years of study by about 2 days per year, suggesting a similar trend as has been observed for surface phytoplankton, mesozooplankton, fish and seabirds probably caused by wide-scale environmental changes.

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More information

Published date: 1 August 2010
Organisations: Marine Systems Modelling, Marine Biogeochemistry

Identifiers

Local EPrints ID: 158539
URI: http://eprints.soton.ac.uk/id/eprint/158539
ISSN: 0967-0645
PURE UUID: 43556bc2-104a-4827-b7c0-95c6e6a4dc90

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Date deposited: 21 Jun 2010 14:17
Last modified: 14 Mar 2024 01:51

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Contributors

Author: R.S. Lampitt
Author: I. Salter
Author: B.A. de Cuevas
Author: S. Hartman
Author: K.E. Larkin
Author: C.A. Pebody

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