Spring-neap modulation of internal tide mixing and vertical nitrate fluxes at a shelf edge in summer
Spring-neap modulation of internal tide mixing and vertical nitrate fluxes at a shelf edge in summer
Measurements of the intra-tidal and spring–neap variation in the vertical flux of nitrate into the base of the
sub-surface chlorophyll maximum (SCM) were made at the shelf edge of the Celtic Sea, a region with strong
internal mixing driven by an internal tide. The neap tide daily mean nitrate flux was 1.3 (0.9–1.8, 95% confidence
interval) mmol m22 d21. The spring tide flux was initially estimated as 3.5 (2.3–5.2, 95% confidence interval)
mmol m22 d21. The higher spring tide nitrate flux was the result of turbulent dissipation occurring within the
base of the SCM as compared to deeper dissipation during neap tides and was dominated by short events
associated with the passage of internal solitons. Taking into account the likely under-sampling of these short
mixing events raised the spring tide nitrate flux estimate to about 9 mmol m22 d21. The neap tide nitrate flux was
sufficient to support substantial new production and a considerable fraction of the observed rates of carbon
fixation. Spring tide fluxes were potentially in excess of the capacity of the phytoplankton community to uptake
nitrate. This potential excess nitrate flux during spring tides may be utilized to support new production during the
lower mixing associated with the transition toward neap tide. The shelf edge is shown to be a region with
a significantly different phytoplankton community as compared to the adjacent Celtic Sea and northeast Atlantic
Ocean, highlighting the role of gradients in physical processes leading to gradients in ecosystem structure.
1735-1747
Sharples, J.
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Tweddle, J.F.
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Green, J.A.M.
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Palmer, Matthew R.
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Kim, Y-N.
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Hickman, A.E.
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Holligan, P.M.
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Moore, C.M.
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Rippeth, T.P.
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Simpson, J.H.
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Krivtsov, V.
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September 2007
Sharples, J.
ec7edc0d-5f09-4b12-a832-0c7bf6a4b3ff
Tweddle, J.F.
1a89370d-8407-482f-91fd-a471022c0bbf
Green, J.A.M.
245d364e-6e9f-4aec-89c9-58cde92f41f4
Palmer, Matthew R.
fd46da6e-cc19-4e8d-a37d-1a0d709f50f7
Kim, Y-N.
507c2f5e-9843-496b-b198-f9b38e742803
Hickman, A.E.
a99786c6-65e6-48c8-8b58-0d3b5608be92
Holligan, P.M.
4c1d9d64-dfa7-49bf-9e15-37f891d59b7c
Moore, C.M.
7ec80b7b-bedc-4dd5-8924-0f5d01927b12
Rippeth, T.P.
a772c9bb-a497-4881-8847-795785d836f2
Simpson, J.H.
5319d01d-458d-4b93-a99e-3e779c2ae399
Krivtsov, V.
29aa1b20-e62f-408f-a417-d16771464f65
Sharples, J., Tweddle, J.F., Green, J.A.M., Palmer, Matthew R., Kim, Y-N., Hickman, A.E., Holligan, P.M., Moore, C.M., Rippeth, T.P., Simpson, J.H. and Krivtsov, V.
(2007)
Spring-neap modulation of internal tide mixing and vertical nitrate fluxes at a shelf edge in summer.
Limnology and Oceanography, 52 (5), .
(doi:10.4319/lo.2007.52.5.1735).
Abstract
Measurements of the intra-tidal and spring–neap variation in the vertical flux of nitrate into the base of the
sub-surface chlorophyll maximum (SCM) were made at the shelf edge of the Celtic Sea, a region with strong
internal mixing driven by an internal tide. The neap tide daily mean nitrate flux was 1.3 (0.9–1.8, 95% confidence
interval) mmol m22 d21. The spring tide flux was initially estimated as 3.5 (2.3–5.2, 95% confidence interval)
mmol m22 d21. The higher spring tide nitrate flux was the result of turbulent dissipation occurring within the
base of the SCM as compared to deeper dissipation during neap tides and was dominated by short events
associated with the passage of internal solitons. Taking into account the likely under-sampling of these short
mixing events raised the spring tide nitrate flux estimate to about 9 mmol m22 d21. The neap tide nitrate flux was
sufficient to support substantial new production and a considerable fraction of the observed rates of carbon
fixation. Spring tide fluxes were potentially in excess of the capacity of the phytoplankton community to uptake
nitrate. This potential excess nitrate flux during spring tides may be utilized to support new production during the
lower mixing associated with the transition toward neap tide. The shelf edge is shown to be a region with
a significantly different phytoplankton community as compared to the adjacent Celtic Sea and northeast Atlantic
Ocean, highlighting the role of gradients in physical processes leading to gradients in ecosystem structure.
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Published date: September 2007
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Local EPrints ID: 48839
URI: http://eprints.soton.ac.uk/id/eprint/48839
ISSN: 0024-3590
PURE UUID: 9d9fd966-8429-44c4-8732-4332bc36aaf5
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Date deposited: 15 Oct 2007
Last modified: 16 Mar 2024 04:11
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Contributors
Author:
J. Sharples
Author:
J.F. Tweddle
Author:
J.A.M. Green
Author:
Matthew R. Palmer
Author:
Y-N. Kim
Author:
P.M. Holligan
Author:
T.P. Rippeth
Author:
J.H. Simpson
Author:
V. Krivtsov
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