{"id":{"repo_id":"odu","oai_identifier":"oai:digitalcommons.odu.edu:oeas_etds-1043"},"canonical_url":"https://search.dev.ndltd.org/etd/odu/oai:digitalcommons.odu.edu:oeas_etds-1043","repository":{"repo_id":"odu","name":"Old Dominion University","base_url":"https://digitalcommons.odu.edu/do/oai/"},"display":{"title":"Modeling Plankton Community Structure Under Environmental Forcing on the Southeastern United States Continental Shelf","abstract":"<p>A system of coupled ordinary differential equations was developed to investigate the time-dependent behavior of phytoplankton, copepod, and doliolid populations associated with upwelling features on the outer southeastern U.S. continental shelf. Model equations describe the interactions of nitrate, ammonium, two phytoplankton size fractions, five copepod developmental stages, doliolids, and a detrital pool. Model dynamics are based primarily upon data obtained from field and laboratory experiments made for southeastern U.S. continental shelf plankton populations. Numerous simulations were performed to investigate the effects of environmental variability on the temporal distribution of the structure of resident plankton populations. Variations on a reference simulation, which represents average upwelling conditions without doliolids, were done to determine the effect of inclusion of doliolids, different feeding strategies, temperature and nutrient variations, and variations in ambient food concentrations on the basic plankton community structure. These simulations provide a measure of the role of environmental versus biological interactions in structuring the planktonic food web on the southeastern U.S. continental shelf. Simulations show that, when present, doliolids reach maximum concentrations 5-7 days after the onset of the phytoplankton bloom resulting from an upwelling event, which is consistent with observations from bottom intrusion upwelling events. The presence of doliolids results in a rapid decrease in copepod concentrations, with the doliolids eventually displacing the copepods. Additional simulations show that ambient temperature conditions modify the rate of increase of the doliolids and copepod populations and hence the relative abundance of these populations.</p>","abstract_html":"&lt;p&gt;A system of coupled ordinary differential equations was developed to investigate the time-dependent behavior of phytoplankton, copepod, and doliolid populations associated with upwelling features on the outer southeastern U.S. continental shelf. Model equations describe the interactions of nitrate, ammonium, two phytoplankton size fractions, five copepod developmental stages, doliolids, and a detrital pool. Model dynamics are based primarily upon data obtained from field and laboratory experiments made for southeastern U.S. continental shelf plankton populations. Numerous simulations were performed to investigate the effects of environmental variability on the temporal distribution of the structure of resident plankton populations. Variations on a reference simulation, which represents average upwelling conditions without doliolids, were done to determine the effect of inclusion of doliolids, different feeding strategies, temperature and nutrient variations, and variations in ambient food concentrations on the basic plankton community structure. These simulations provide a measure of the role of environmental versus biological interactions in structuring the planktonic food web on the southeastern U.S. continental shelf. Simulations show that, when present, doliolids reach maximum concentrations 5-7 days after the onset of the phytoplankton bloom resulting from an upwelling event, which is consistent with observations from bottom intrusion upwelling events. The presence of doliolids results in a rapid decrease in copepod concentrations, with the doliolids eventually displacing the copepods. Additional simulations show that ambient temperature conditions modify the rate of increase of the doliolids and copepod populations and hence the relative abundance of these populations.&lt;/p&gt;","abstract_has_math":false,"creators":["Haskell, Andrew Glenn Edward"],"institution":null,"degree_name":"Master of Science (MS)","degree_level":"Thesis","degree_discipline":"Ocean & Earth Sciences","degree_department":null,"school":null,"contributors":["Eileen Hofmann","Larry Atkinson","John Klinck","Gustav-Adolf Paffenhofer","Peter Verity"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1997,"date_issued":"1997-01-01T08:00:00Z","date_published":"1997-01-01T08:00:00Z","updated_at":"2026-07-24T03:34:39Z","subjects":["Plankton","Continental shelf","United States","Modeling","Upwelling","Ecology and Evolutionary Biology","Oceanography"],"languages":[],"rights":["<p>In Copyright. URI: <a href=\"http://rightsstatements.org/vocab/InC/1.0/\">http://rightsstatements.org/vocab/InC/1.0/</a> This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).</p>"],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["9780591631852"],"render_values":[{"text":"9780591631852","href":null,"code":true}]}]},"links":{"outbound_url":"https://digitalcommons.odu.edu/oeas_etds/42","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Eileen Hofmann","Larry Atkinson","John Klinck","Gustav-Adolf Paffenhofer","Peter Verity"]},{"key":"dc:creator","label":"Author","values":["Haskell, Andrew Glenn Edward"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.available","label":"Dc Date Available","values":["2019-04-12T07:00:00Z"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Ocean & Earth Sciences"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Thesis"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science (MS)"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Plankton","Continental shelf","United States","Modeling","Upwelling","Ecology and Evolutionary Biology","Oceanography"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:rights","label":"Dc Rights","values":["<p>In Copyright. URI: <a href=\"http://rightsstatements.org/vocab/InC/1.0/\">http://rightsstatements.org/vocab/InC/1.0/</a> This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).</p>"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["9780591631852","https://digitalcommons.odu.edu/oeas_etds/42"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["<p>A system of coupled ordinary differential equations was developed to investigate the time-dependent behavior of phytoplankton, copepod, and doliolid populations associated with upwelling features on the outer southeastern U.S. continental shelf. Model equations describe the interactions of nitrate, ammonium, two phytoplankton size fractions, five copepod developmental stages, doliolids, and a detrital pool. Model dynamics are based primarily upon data obtained from field and laboratory experiments made for southeastern U.S. continental shelf plankton populations. Numerous simulations were performed to investigate the effects of environmental variability on the temporal distribution of the structure of resident plankton populations. Variations on a reference simulation, which represents average upwelling conditions without doliolids, were done to determine the effect of inclusion of doliolids, different feeding strategies, temperature and nutrient variations, and variations in ambient food concentrations on the basic plankton community structure. These simulations provide a measure of the role of environmental versus biological interactions in structuring the planktonic food web on the southeastern U.S. continental shelf. Simulations show that, when present, doliolids reach maximum concentrations 5-7 days after the onset of the phytoplankton bloom resulting from an upwelling event, which is consistent with observations from bottom intrusion upwelling events. The presence of doliolids results in a rapid decrease in copepod concentrations, with the doliolids eventually displacing the copepods. Additional simulations show that ambient temperature conditions modify the rate of increase of the doliolids and copepod populations and hence the relative abundance of these populations.</p>"]},{"key":"dc:title","label":"Title","values":["Modeling Plankton Community Structure Under Environmental Forcing on the Southeastern United States Continental Shelf"]}]}],"canonical_facts":{"dc:contributor":["Eileen Hofmann","Larry Atkinson","John Klinck","Gustav-Adolf Paffenhofer","Peter Verity"],"dc:creator":["Haskell, Andrew Glenn Edward"],"dc:date.available":["2019-04-12T07:00:00Z"],"dc:description.abstract":["<p>A system of coupled ordinary differential equations was developed to investigate the time-dependent behavior of phytoplankton, copepod, and doliolid populations associated with upwelling features on the outer southeastern U.S. continental shelf. Model equations describe the interactions of nitrate, ammonium, two phytoplankton size fractions, five copepod developmental stages, doliolids, and a detrital pool. Model dynamics are based primarily upon data obtained from field and laboratory experiments made for southeastern U.S. continental shelf plankton populations. Numerous simulations were performed to investigate the effects of environmental variability on the temporal distribution of the structure of resident plankton populations. Variations on a reference simulation, which represents average upwelling conditions without doliolids, were done to determine the effect of inclusion of doliolids, different feeding strategies, temperature and nutrient variations, and variations in ambient food concentrations on the basic plankton community structure. These simulations provide a measure of the role of environmental versus biological interactions in structuring the planktonic food web on the southeastern U.S. continental shelf. Simulations show that, when present, doliolids reach maximum concentrations 5-7 days after the onset of the phytoplankton bloom resulting from an upwelling event, which is consistent with observations from bottom intrusion upwelling events. The presence of doliolids results in a rapid decrease in copepod concentrations, with the doliolids eventually displacing the copepods. Additional simulations show that ambient temperature conditions modify the rate of increase of the doliolids and copepod populations and hence the relative abundance of these populations.</p>"],"dc:identifier":["9780591631852","https://digitalcommons.odu.edu/oeas_etds/42"],"dc:rights":["<p>In Copyright. URI: <a href=\"http://rightsstatements.org/vocab/InC/1.0/\">http://rightsstatements.org/vocab/InC/1.0/</a> This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).</p>"],"dc:subject":["Plankton","Continental shelf","United States","Modeling","Upwelling","Ecology and Evolutionary Biology","Oceanography"],"dc:title":["Modeling Plankton Community Structure Under Environmental Forcing on the Southeastern United States Continental Shelf"],"thesis:degree_discipline":["Ocean & Earth Sciences"],"thesis:degree_level":["Thesis"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T03:34:39Z"}