Physical-biological interactions in the Southern Ocean

Physical-biological interactions in the Southern Ocean were investigated using remote sensing data from several different satellite sensors. Satellite sea surface temperature data were used to study the dynamics of the Antarctic Polar Front (PF). Satellite ocean color data were used to estimate surf...

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Bibliographic Details
Main Author: Moore, Jefferson Keith
Other Authors: Abbott, Mark R., College of Oceanic and Atmospheric Sciences, Oregon State University. Graduate School
Format: Doctoral or Postdoctoral Thesis
Language:English
unknown
Published: Oregon State University
Subjects:
Online Access:https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x059c948m
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spelling ftoregonstate:ir.library.oregonstate.edu:x059c948m 2024-04-21T07:46:41+00:00 Physical-biological interactions in the Southern Ocean Moore, Jefferson Keith Abbott, Mark R. College of Oceanic and Atmospheric Sciences Oregon State University. Graduate School https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x059c948m English [eng] eng unknown Oregon State University https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x059c948m Copyright Not Evaluated Marine phytoplankton -- Ecology -- Antarctic Ocean Antarctic Ocean -- Remote sensing Dissertation ftoregonstate 2024-03-28T02:08:26Z Physical-biological interactions in the Southern Ocean were investigated using remote sensing data from several different satellite sensors. Satellite sea surface temperature data were used to study the dynamics of the Antarctic Polar Front (PF). Satellite ocean color data were used to estimate surface chlorophyll concentrations and their relation to various physical forcings within the Southern Ocean. A detailed study of phytoplankton blooms at the Antarctic Polar Front revealed that elevated chlorophyll concentrations (phytoplankton blooms) occur most often in areas where the PF interacts with large topographic features within the Southern Ocean. The physical dynamics of the PF are strongly influenced by the topography, and in turn strongly influence phytoplankton bloom dynamics. The analysis of satellite data from the modern Southern Ocean indicates that phytoplankton are limited by the availability of the micronutrient iron in most areas. This iron-limitation implies that the elevated iron inputs during glacial periods would have led to increased phytoplankton primary and export production and a stronger sink for atmospheric CO₂ in the Southern Ocean. Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctic Ocean Southern Ocean ScholarsArchive@OSU (Oregon State University)
institution Open Polar
collection ScholarsArchive@OSU (Oregon State University)
op_collection_id ftoregonstate
language English
unknown
topic Marine phytoplankton -- Ecology -- Antarctic Ocean
Antarctic Ocean -- Remote sensing
spellingShingle Marine phytoplankton -- Ecology -- Antarctic Ocean
Antarctic Ocean -- Remote sensing
Moore, Jefferson Keith
Physical-biological interactions in the Southern Ocean
topic_facet Marine phytoplankton -- Ecology -- Antarctic Ocean
Antarctic Ocean -- Remote sensing
description Physical-biological interactions in the Southern Ocean were investigated using remote sensing data from several different satellite sensors. Satellite sea surface temperature data were used to study the dynamics of the Antarctic Polar Front (PF). Satellite ocean color data were used to estimate surface chlorophyll concentrations and their relation to various physical forcings within the Southern Ocean. A detailed study of phytoplankton blooms at the Antarctic Polar Front revealed that elevated chlorophyll concentrations (phytoplankton blooms) occur most often in areas where the PF interacts with large topographic features within the Southern Ocean. The physical dynamics of the PF are strongly influenced by the topography, and in turn strongly influence phytoplankton bloom dynamics. The analysis of satellite data from the modern Southern Ocean indicates that phytoplankton are limited by the availability of the micronutrient iron in most areas. This iron-limitation implies that the elevated iron inputs during glacial periods would have led to increased phytoplankton primary and export production and a stronger sink for atmospheric CO₂ in the Southern Ocean.
author2 Abbott, Mark R.
College of Oceanic and Atmospheric Sciences
Oregon State University. Graduate School
format Doctoral or Postdoctoral Thesis
author Moore, Jefferson Keith
author_facet Moore, Jefferson Keith
author_sort Moore, Jefferson Keith
title Physical-biological interactions in the Southern Ocean
title_short Physical-biological interactions in the Southern Ocean
title_full Physical-biological interactions in the Southern Ocean
title_fullStr Physical-biological interactions in the Southern Ocean
title_full_unstemmed Physical-biological interactions in the Southern Ocean
title_sort physical-biological interactions in the southern ocean
publisher Oregon State University
url https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x059c948m
genre Antarc*
Antarctic
Antarctic Ocean
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Ocean
Southern Ocean
op_relation https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x059c948m
op_rights Copyright Not Evaluated
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