A study of gas exchange during the transition from deep winter mixing to spring bloom in the Bay of Biscay measured by continuous observation from a ship of opportunity
A study of gas exchange during the transition from deep winter mixing to spring bloom in the Bay of Biscay measured by continuous observation from a ship of opportunity
Monitoring from ships of opportunity allows a wide range of parameters to be measured, thereby extending the coverage of operational oceanographic studies. Observation of dissolved oxygen using new sensors offers an effective way of monitoring changes in biological production. The limits of the application were tested following the transition from winter storms to the spring bloom (2007). Calculation of dissolved nitrogen enables changes in gas saturation due to physical and biological processes to be separated. By combining these measurements with data from numerical models and Argo floats the critical role of subsurface processes in determining rates of change at the surface can be assessed.
41-59
Hydes, D.J .
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Hartman, M.C.
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Bargeron, C.P.
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Campbell, J.M.
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Cure, M.S.
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Woolf, D.K.
aeb210e8-5fd5-4dd4-903e-6d4ef2df9abe
August 2008
Hydes, D.J .
ac7371d4-c2b9-4926-bb77-ce58480ecff7
Hartman, M.C.
cdd63b60-f89a-4ef8-842d-7803f8213c18
Bargeron, C.P.
14a61c9c-b684-450c-b127-340e6cbe734f
Campbell, J.M.
ccdf3dec-f651-4d59-96d7-41859f78abe5
Cure, M.S.
719e00ba-a4a5-4f7f-aeb1-57926814f540
Woolf, D.K.
aeb210e8-5fd5-4dd4-903e-6d4ef2df9abe
Hydes, D.J ., Hartman, M.C., Bargeron, C.P., Campbell, J.M., Cure, M.S. and Woolf, D.K.
(2008)
A study of gas exchange during the transition from deep winter mixing to spring bloom in the Bay of Biscay measured by continuous observation from a ship of opportunity.
Journal of Operational Oceanography, 1 (2), .
Abstract
Monitoring from ships of opportunity allows a wide range of parameters to be measured, thereby extending the coverage of operational oceanographic studies. Observation of dissolved oxygen using new sensors offers an effective way of monitoring changes in biological production. The limits of the application were tested following the transition from winter storms to the spring bloom (2007). Calculation of dissolved nitrogen enables changes in gas saturation due to physical and biological processes to be separated. By combining these measurements with data from numerical models and Argo floats the critical role of subsurface processes in determining rates of change at the surface can be assessed.
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Published date: August 2008
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Local EPrints ID: 63155
URI: http://eprints.soton.ac.uk/id/eprint/63155
ISSN: 1755-876X
PURE UUID: 34854e04-3312-47c3-a13f-1a7b135e142e
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Date deposited: 15 Sep 2008
Last modified: 09 Jan 2022 07:24
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Contributors
Author:
D.J . Hydes
Author:
M.C. Hartman
Author:
C.P. Bargeron
Author:
J.M. Campbell
Author:
M.S. Cure
Author:
D.K. Woolf
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