On the role of the mesoscale circulation on an idealized coastal upwelling ecosystem
Open accessAbstract
An idealized circulation model of coastal upwelling coupled to an ecosystem model has been built to address the impact of features such as eddies and filaments emerging from mesoscale dynamics on a marine ecosystem. The model mimics coastal upwelling along an infinite straight coast with north–south cyclic boundary conditions. Thanks to the parametrization of the geostrophic onshore flow in the thermocline, the circulation captures the typical characteristics of a coastal upwelling region: an equatorward coastal jet, a poleward undercurrent along the continental slope and mesoscale eddies and filaments. This eddying three‐dimensional simulation is compared to a two‐dimensional simulation using the averaged velocity field of the first simulation as velocity field. This approach allows us to compare simulations having similar upwelling and nutrient input but differing in the nature of the flow. An offshore spreading of the phytoplankton bloom is found in the eddying simulation. The width of the productive coastal band is increased from 80 km to 200 km by the mesoscale activity. A biogeochemical budget carried out in a 300 km‐wide coastal band provides evidence that mesoscale activity decreases the total phytoplankton content mainly by exporting a significant part of the surface phytoplankton below the euphotic layer. In presence of mesoscale activity, the downward and offshore export of phytoplankton, zooplankton and detritus significantly contributes to total export of organic matter out of the surface coastal ocean, whereas their contribution to export is weak in the two‐dimensional case.
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(Sub)mesoscale turbulence modulates offshore transport and hence the net upwelling rate.
“But (sub)mesoscale turbulence modulates offshore transport, hence the net upwelling rate.”
From Competition between Baroclinic Instability and Ekman Transport under Varying Buoyancy Forcings in Upwelling Systems: An Idealized Analog to the Southern Ocean (2021) · cites this paper as Lathuilière et al. 2010
The Summary (§5, paragraph 51; page unavailable) says mesoscale filaments export nitrate and phytoplankton offshore, supporting the transport part. But it also says the eddying and non-eddying simulations have the same upwelling mass flux, so the paper does not support the claimed change in net upwelling rate. (LLM, conf=0.91)
Experimental — accuracy not yet measuredQuasi-balanced mesoscale and submesoscale turbulence is responsible for rectified eddy transport which also tends to counteract the Ekman upwelling cell.
“quasi-balanced mesoscale and submesoscale turbulence is responsible for rectified eddy transport which also tends to counteract the Ekman upwelling cell.”
From Competition between Baroclinic Instability and Ekman Transport under Varying Buoyancy Forcings in Upwelling Systems: An Idealized Analog to the Southern Ocean (2021) · cites this paper as Lathuilière et al. 2010
The Summary (§5; page unavailable) reports that mesoscale circulation and filaments transport nitrate and phytoplankton offshore. But the Discussion (§4; page unavailable) explicitly says that rectification of the mean flow by mesoscale dynamics was not addressed. The paper does not establish that eddy transport counteracts the Ekman upwelling cell; its Physical Model (§2.1; page unavailable) attributes compensating onshore transport to an imposed alongshore pressure gradient. (LLM, conf=0.84)
Experimental — accuracy not yet measured
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Xue, T. (2021) · Biogeosciences · doi:10.5194/bg-2021-113-ac3
Xue, T. (2021) · Biogeosciences · doi:10.5194/bg-2021-113-ac2
Eddy impacts on the marine biogeochemistry of the California Current SystemPreprint
Damien, P., Bianchi, D., Kessouri, F., & McWilliams, J. C. (2023) · doi:10.22541/essoar.168926263.36943652/v1
Song, Z., Man, W., He, X., Nie, Q., Li, Z., Du, X., Jiang, Y., Zeng, Y., & Zhang, X. (2026) · Ecological Informatics · doi:10.1016/j.ecoinf.2026.103886
- Authors
- Lathuilière, C., Echevin, V., Lévy, M., & Madec, G.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- LOCEAN, Institut Pierre‐Simon Laplace Université Pierre et Marie Curie, CNRS, IRD, MNHN Paris France
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 2010-09
- Volume
- 115
- Issue
- C9
- Pages
- 09018
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W1969001328
- Cited by
- 63
- References
- 40
- Citations by year
- 2026: 1 · 2025: 1 · 2024: 5 · 2023: 5 · 2022: 2 · 2021: 6 · 2020: 3 · 2019: 1 · 2018: 5 · 2017: 4 · 2016: 10 · 2015: 7 · 2014: 2 · 2013: 3 · 2012: 4
- FWCI
- 2.58
- Type
- journal article
- Language
- en
- Open access
- green
- hal.science
- Licence
- Locations
- Journal of Geophysical Research Atmospheres (publishedVersion)
- HAL (submittedVersion, other-oa)
- ePrints Soton (University of Southampton) (submittedVersion)
- NERC Open Research Archive (Natural Environment Research Council) (submittedVersion)
- Funders
- Natural Environment Research Council (noc010010, noc010005)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Environmental Science › Global and Planetary Change › Marine and fisheries research
- Keywords
- coastal upwelling, mesoscale eddies, filaments, phytoplankton blooms, thermocline, coastal jet, undercurrent, euphotic layer, ecosystem modeling
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
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