Go with the flow: Timescales of biogeochemical and ecological ocean connectivity

Ocean circulation can govern relationships between physical, biogeochemical and ecological processes and determines the connectivity between regions. As such, a variety of oceanographic problems can be addressed using a Lagrangian modelling approach. This thesis utilises velocity output from a high...

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Main Author: Robinson-Parker, Josie
Format: Thesis
Language:English
Published: 2017
Subjects:
Online Access:https://eprints.soton.ac.uk/415524/
https://eprints.soton.ac.uk/415524/1/Robinson_Josie_PhD_Thesis_Oct_17.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:415524 2023-07-30T04:03:07+02:00 Go with the flow: Timescales of biogeochemical and ecological ocean connectivity Robinson-Parker, Josie 2017-10-23 text https://eprints.soton.ac.uk/415524/ https://eprints.soton.ac.uk/415524/1/Robinson_Josie_PhD_Thesis_Oct_17.pdf en English eng https://eprints.soton.ac.uk/415524/1/Robinson_Josie_PhD_Thesis_Oct_17.pdf Robinson-Parker, Josie (2017) Go with the flow: Timescales of biogeochemical and ecological ocean connectivity. University of Southampton, Doctoral Thesis, 285pp. uos_thesis Thesis NonPeerReviewed 2017 ftsouthampton 2023-07-09T22:18:49Z Ocean circulation can govern relationships between physical, biogeochemical and ecological processes and determines the connectivity between regions. As such, a variety of oceanographic problems can be addressed using a Lagrangian modelling approach. This thesis utilises velocity output from a high resolution ocean general circulation model and a Lagrangian particle tracking programme to address three topics: the global-scale efficiency of regional geoengineering by iron fertilisation; the role of natural iron fertilisation in phytoplankton blooms; and the connectivity of Marine Protected Areas (MPAs) to upstream anthropogenic impacts. Artificial ocean iron fertilization (OIF) enhances phytoplankton productivity and is being explored as a means of sequestering anthropogenic carbon within the deep ocean for an extended period (e.g., the Intergovernmental Panel on Climate Change's standard 100 year time horizon). This study assessed the impact of deep circulation on sequestered carbon in the Southern Ocean, a high-nutrient low-chlorophyll region known to be iron stressed. The Lagrangian particle tracking approach was employed to analyze water mass trajectories over a 100 year simulation. By the end of the experiment, for a sequestration depth of 1000 m, 66% of the carbon had been re-exposed to the atmosphere, taking an average of 37.8 years. These results emphasized that successful OIF is dependent on the physical circulation, as well as the biogeochemistry. Following on from the long-term impact of the wider Southern Ocean circulation, the local circulation around three Southern Ocean islands was considered. In exception to the typically High Nutrient, Low Chlorophyll conditions of the Southern Ocean, phytoplankton blooms occur annually downstream of the Kerguelen Plateau, Crozet Islands, and South Georgia, fertilized by iron-rich shelf waters. The Lagrangian particle tracking approach was used to investigate if advection could explain the inter-annual variability observed in the blooms in satellite ocean colour ... Thesis Crozet Islands Southern Ocean University of Southampton: e-Prints Soton Kerguelen Southern Ocean
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Ocean circulation can govern relationships between physical, biogeochemical and ecological processes and determines the connectivity between regions. As such, a variety of oceanographic problems can be addressed using a Lagrangian modelling approach. This thesis utilises velocity output from a high resolution ocean general circulation model and a Lagrangian particle tracking programme to address three topics: the global-scale efficiency of regional geoengineering by iron fertilisation; the role of natural iron fertilisation in phytoplankton blooms; and the connectivity of Marine Protected Areas (MPAs) to upstream anthropogenic impacts. Artificial ocean iron fertilization (OIF) enhances phytoplankton productivity and is being explored as a means of sequestering anthropogenic carbon within the deep ocean for an extended period (e.g., the Intergovernmental Panel on Climate Change's standard 100 year time horizon). This study assessed the impact of deep circulation on sequestered carbon in the Southern Ocean, a high-nutrient low-chlorophyll region known to be iron stressed. The Lagrangian particle tracking approach was employed to analyze water mass trajectories over a 100 year simulation. By the end of the experiment, for a sequestration depth of 1000 m, 66% of the carbon had been re-exposed to the atmosphere, taking an average of 37.8 years. These results emphasized that successful OIF is dependent on the physical circulation, as well as the biogeochemistry. Following on from the long-term impact of the wider Southern Ocean circulation, the local circulation around three Southern Ocean islands was considered. In exception to the typically High Nutrient, Low Chlorophyll conditions of the Southern Ocean, phytoplankton blooms occur annually downstream of the Kerguelen Plateau, Crozet Islands, and South Georgia, fertilized by iron-rich shelf waters. The Lagrangian particle tracking approach was used to investigate if advection could explain the inter-annual variability observed in the blooms in satellite ocean colour ...
format Thesis
author Robinson-Parker, Josie
spellingShingle Robinson-Parker, Josie
Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
author_facet Robinson-Parker, Josie
author_sort Robinson-Parker, Josie
title Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
title_short Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
title_full Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
title_fullStr Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
title_full_unstemmed Go with the flow: Timescales of biogeochemical and ecological ocean connectivity
title_sort go with the flow: timescales of biogeochemical and ecological ocean connectivity
publishDate 2017
url https://eprints.soton.ac.uk/415524/
https://eprints.soton.ac.uk/415524/1/Robinson_Josie_PhD_Thesis_Oct_17.pdf
geographic Kerguelen
Southern Ocean
geographic_facet Kerguelen
Southern Ocean
genre Crozet Islands
Southern Ocean
genre_facet Crozet Islands
Southern Ocean
op_relation https://eprints.soton.ac.uk/415524/1/Robinson_Josie_PhD_Thesis_Oct_17.pdf
Robinson-Parker, Josie (2017) Go with the flow: Timescales of biogeochemical and ecological ocean connectivity. University of Southampton, Doctoral Thesis, 285pp.
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