Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models

Marine phytoplankton growth is controlled by non-linear processes, such as the photosynthetic and photoacclimative response to irradiance. Traditional Eulerian models calculate rates of primary production using the assumption that phytoplankton have identical properties, whereas Lagrangian models si...

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Main Author: Tomkins, Melissa
Format: Thesis
Language:English
Published: 2016
Subjects:
Online Access:https://eprints.soton.ac.uk/397963/
https://eprints.soton.ac.uk/397963/1/Tomkins%252C%2520Melissa_PhD_thesis_July_2016.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:397963 2023-07-30T04:05:33+02:00 Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models Tomkins, Melissa 2016-06-06 text https://eprints.soton.ac.uk/397963/ https://eprints.soton.ac.uk/397963/1/Tomkins%252C%2520Melissa_PhD_thesis_July_2016.pdf en English eng https://eprints.soton.ac.uk/397963/1/Tomkins%252C%2520Melissa_PhD_thesis_July_2016.pdf Tomkins, Melissa (2016) Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models. University of Southampton, Ocean & Earth Science, Doctoral Thesis, 225pp. Thesis NonPeerReviewed 2016 ftsouthampton 2023-07-09T22:09:21Z Marine phytoplankton growth is controlled by non-linear processes, such as the photosynthetic and photoacclimative response to irradiance. Traditional Eulerian models calculate rates of primary production using the assumption that phytoplankton have identical properties, whereas Lagrangian models simulate phytoplankton as individual particles, tracking their trajectories through the light field. It might therefore be expected that photoacclimation in Lagrangian models would have an impact on seasonal cycles. In this thesis, I construct a Lagrangian ecosystem model, applying it to two questions: whether the individual responses of phytoplankton to their local irradiance affects the overall rates of primary production, and whether Lagrangian models are necessary for the study of the mechanisms surrounding the spring bloom, due to their representation of phytoplankton growth in response to mixing. The study begins by addressing some of the fundamental assumptions underpinning Lagrangian models, and provides novel solutions for some of the difficulties. The model was set up for Ocean Weather Station India (OWSI) in the North Atlantic, and the predicted seasonal cycles of primary production were shown to not differ from those predicted by an Eulerian equivalent, due to the phytoplankton being mixed too fast to have time to acclimate to local irradiances. Additionally, the results suggested a closer relationship between the timescales of growth and mixing, demonstrating that vertical profiles of phytoplankton could form within a well-mixed layer, resulting in changes to the overall rates of primary production. The model was next used to investigate the controls of the spring bloom at OWSI, by investigating the critical depth, critical turbulence and disturbance-recovery hypotheses. Although the use of Lagrangian model did highlight a possible source of inaccuracy when calculating critical depth with an Eulerian model, overall an Eulerian model could have performed the experiments with the same results, given ... Thesis North Atlantic University of Southampton: e-Prints Soton
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Marine phytoplankton growth is controlled by non-linear processes, such as the photosynthetic and photoacclimative response to irradiance. Traditional Eulerian models calculate rates of primary production using the assumption that phytoplankton have identical properties, whereas Lagrangian models simulate phytoplankton as individual particles, tracking their trajectories through the light field. It might therefore be expected that photoacclimation in Lagrangian models would have an impact on seasonal cycles. In this thesis, I construct a Lagrangian ecosystem model, applying it to two questions: whether the individual responses of phytoplankton to their local irradiance affects the overall rates of primary production, and whether Lagrangian models are necessary for the study of the mechanisms surrounding the spring bloom, due to their representation of phytoplankton growth in response to mixing. The study begins by addressing some of the fundamental assumptions underpinning Lagrangian models, and provides novel solutions for some of the difficulties. The model was set up for Ocean Weather Station India (OWSI) in the North Atlantic, and the predicted seasonal cycles of primary production were shown to not differ from those predicted by an Eulerian equivalent, due to the phytoplankton being mixed too fast to have time to acclimate to local irradiances. Additionally, the results suggested a closer relationship between the timescales of growth and mixing, demonstrating that vertical profiles of phytoplankton could form within a well-mixed layer, resulting in changes to the overall rates of primary production. The model was next used to investigate the controls of the spring bloom at OWSI, by investigating the critical depth, critical turbulence and disturbance-recovery hypotheses. Although the use of Lagrangian model did highlight a possible source of inaccuracy when calculating critical depth with an Eulerian model, overall an Eulerian model could have performed the experiments with the same results, given ...
format Thesis
author Tomkins, Melissa
spellingShingle Tomkins, Melissa
Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
author_facet Tomkins, Melissa
author_sort Tomkins, Melissa
title Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
title_short Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
title_full Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
title_fullStr Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
title_full_unstemmed Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models
title_sort photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in lagrangian and eulerian models
publishDate 2016
url https://eprints.soton.ac.uk/397963/
https://eprints.soton.ac.uk/397963/1/Tomkins%252C%2520Melissa_PhD_thesis_July_2016.pdf
genre North Atlantic
genre_facet North Atlantic
op_relation https://eprints.soton.ac.uk/397963/1/Tomkins%252C%2520Melissa_PhD_thesis_July_2016.pdf
Tomkins, Melissa (2016) Photoacclimation, production and critical depth: a comparison of phytoplankton dynamics in Lagrangian and Eulerian models. University of Southampton, Ocean & Earth Science, Doctoral Thesis, 225pp.
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