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One-dimensional modelling of the plankton ecosystem of the north-western Corsican coastal area in relation to meteorological constraints

One-dimensional modelling of the plankton ecosystem of the north-western Corsican coastal area in relation to meteorological constraints
One-dimensional modelling of the plankton ecosystem of the north-western Corsican coastal area in relation to meteorological constraints
In order to study the influence of wind mixing on the spring variability of the plankton production of the north western Corsican coastal area, a one-dimensional (1D), vertical, coupled hydrodynamic/biological model (ECOHYDROMV) is used. A hydrodynamic 1D model of the water column with a k–l turbulent closure is applied. The biological model comprises six state variables, representing the plankton ecosystem in the spring period: phytoplankton, copepods, nitrate, ammonium, particulate organic matter of phytoplanktonic origin and particulate organic matter of zooplanktonic origin. The system is influenced by turbulence (expressed by the vertical eddy diffusivity), temperature and irradiance. The model takes into account momentum and heat surface fluxes computed from meteorological data in order to simulate a typical spring atmospheric forcing for the considered area. Results show that primary production vertical structure is characterised by a subsurface maximum which deepens with time and is regulated by the opposite gradients of nitrate concentration and irradiance. Surface plankton productivity is mainly controlled by turbulent vertical transport of nutrients into the mixed layer. The short time scale variability of turbulent mixing generated by the wind appears to be responsible for the plurimodal shape of plankton blooms, observed in the considered area. Furthermore, the model is applied to the study of the spring evolution of the plankton communities off the bay of Calvi (Corsica) for the years 1986 and 1988. In order to initiate and validate the model, time series of hydrological, chemical and biological data have been used. The model reproduces accurately the spring evolution of the phytoplankton biomass measured in situ and illustrates that its strong variability in those years was in close relation to the variability of the wind intensity.
coupled hydrodynamic/biological model, north-western Corsican coast, plankton ecosystem, vertical mixing
0924-7963
337-362
Skliris, N.
07af7484-2e14-49aa-9cd3-1979ea9b064e
Elkalay, K.
22c2dfd6-f996-45d6-94eb-d0c3fc32d79e
Goffart, A.
35c08b9c-5376-4173-bccf-d77d279f3d45
Frangoulis, C.
5cc251be-22b2-403a-8787-94f5d458c8e7
Hecq, J.H.
089d8ea1-eb46-4102-b33a-6b6a28c81df8
Skliris, N.
07af7484-2e14-49aa-9cd3-1979ea9b064e
Elkalay, K.
22c2dfd6-f996-45d6-94eb-d0c3fc32d79e
Goffart, A.
35c08b9c-5376-4173-bccf-d77d279f3d45
Frangoulis, C.
5cc251be-22b2-403a-8787-94f5d458c8e7
Hecq, J.H.
089d8ea1-eb46-4102-b33a-6b6a28c81df8

Skliris, N., Elkalay, K., Goffart, A., Frangoulis, C. and Hecq, J.H. (2001) One-dimensional modelling of the plankton ecosystem of the north-western Corsican coastal area in relation to meteorological constraints. Journal of Marine Systems, 27 (4), 337-362. (doi:10.1016/S0924-7963(00)00078-6).

Record type: Article

Abstract

In order to study the influence of wind mixing on the spring variability of the plankton production of the north western Corsican coastal area, a one-dimensional (1D), vertical, coupled hydrodynamic/biological model (ECOHYDROMV) is used. A hydrodynamic 1D model of the water column with a k–l turbulent closure is applied. The biological model comprises six state variables, representing the plankton ecosystem in the spring period: phytoplankton, copepods, nitrate, ammonium, particulate organic matter of phytoplanktonic origin and particulate organic matter of zooplanktonic origin. The system is influenced by turbulence (expressed by the vertical eddy diffusivity), temperature and irradiance. The model takes into account momentum and heat surface fluxes computed from meteorological data in order to simulate a typical spring atmospheric forcing for the considered area. Results show that primary production vertical structure is characterised by a subsurface maximum which deepens with time and is regulated by the opposite gradients of nitrate concentration and irradiance. Surface plankton productivity is mainly controlled by turbulent vertical transport of nutrients into the mixed layer. The short time scale variability of turbulent mixing generated by the wind appears to be responsible for the plurimodal shape of plankton blooms, observed in the considered area. Furthermore, the model is applied to the study of the spring evolution of the plankton communities off the bay of Calvi (Corsica) for the years 1986 and 1988. In order to initiate and validate the model, time series of hydrological, chemical and biological data have been used. The model reproduces accurately the spring evolution of the phytoplankton biomass measured in situ and illustrates that its strong variability in those years was in close relation to the variability of the wind intensity.

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More information

Published date: January 2001
Keywords: coupled hydrodynamic/biological model, north-western Corsican coast, plankton ecosystem, vertical mixing
Organisations: Physical Oceanography

Identifiers

Local EPrints ID: 365222
URI: http://eprints.soton.ac.uk/id/eprint/365222
ISSN: 0924-7963
PURE UUID: 92e32ddd-97b0-4848-8866-5e89ad911b3c
ORCID for N. Skliris: ORCID iD orcid.org/0000-0002-2473-2586

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Date deposited: 28 May 2014 09:40
Last modified: 15 Mar 2024 03:39

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Contributors

Author: N. Skliris ORCID iD
Author: K. Elkalay
Author: A. Goffart
Author: C. Frangoulis
Author: J.H. Hecq

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