Air-sea carbon dynamics in Baffin Bay: 2011-2021

dc.contributor.advisorElse, Brent
dc.contributor.authorNickoloff, Gina Mary
dc.contributor.committeememberMarshall, Shawn
dc.contributor.committeememberKimura-Hara, Susana
dc.date2023-11
dc.date.accessioned2023-08-24T20:43:29Z
dc.date.available2023-08-24T20:43:29Z
dc.date.issued2023-08
dc.description.abstractArctic waters play a disproportionately large role in oceanic CO2 uptake, but are most vulnerable to impacts of climate change. Due to the Arctic’s limited accessibility and remote nature, oceanic CO2 data is sparse to the extent that observation-based estimates of air-sea CO2 flux have only been derived for certain regions, leaving considerable uncertainty in the contribution of Arctic seas to global carbon budgets. Comprehensive description of surface-ocean CO2 dynamics in poorly-studied Arctic regions is needed to constrain Arctic and global carbon cycles, and to anticipate and document future change. In this thesis I provide such a novel description for the Baffin Bay region by examining the spatial and temporal distributions of surface-ocean partial pressure of CO2 (pCO2) while identifying its driving physical and biogeochemical controls, and by quantifying air-sea CO2 fluxes over the region during the open-water season. Utilising an extensive continuous underway ship-based pCO2 dataset accumulated over the last decade, 2011 to 2021, I report surface-ocean pCO2 over Baffin Bay (which in this definition includes Nares Strait and the Northwater Polynya) from June to October. Baffin Bay was highly favourable to uptake of atmospheric CO2 (70 to 130 μatm below saturation, depending on the year), but had substantial regional variability in pCO2 due to hydrography and ocean currents. Over the open-water season pCO2 exhibited a temporal pattern, increasing June to October but remaining undersaturated. Through comprehensive evaluation of Baffin Bay air-sea CO2 fluxes I show that it is a notably strong uptake region, even when compared to other North American Arctic regions. Baffin Bay had an average open-water-season flux of -7.3 mmol CO2 m-2 day1, which corresponds to an estimated carbon uptake of 11.9 Tg C year-1. Ice coverage in some regions served as a barrier to uptake, particularly in the northern portions of the study region. In the future, Baffin Bay is expected to remain a strong uptake region, with possible increased uptake as sea-ice loss lengthens the open-water season and summer wind speeds increase. This research fills a sizeable knowledge gap in Arctic oceanic carbon uptake, showing Baffin Bay is an exceptionally strong uptake region and providing insight into the variability of and drivers to surface-ocean pCO2.
dc.identifier.citationNickoloff, G. M. (2023). Air-sea carbon dynamics in Baffin Bay: 2011-2021 (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.
dc.identifier.urihttps://hdl.handle.net/1880/116897
dc.identifier.urihttps://dx.doi.org/10.11575/PRISM/41739
dc.language.isoen
dc.publisher.facultyGraduate Studies
dc.publisher.institutionUniversity of Calgary
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
dc.subjectair-sea CO2 fluxes
dc.subjectArctic
dc.subjectBaffin Bay
dc.subjectpCO2
dc.subject.classificationGeography
dc.subject.classificationOceanography
dc.subject.classificationBiogeochemistry
dc.titleAir-sea carbon dynamics in Baffin Bay: 2011-2021
dc.typemaster thesis
thesis.degree.disciplineGeography
thesis.degree.grantorUniversity of Calgary
thesis.degree.nameMaster of Science (MSc)
ucalgary.thesis.accesssetbystudentI do not require a thesis withhold – my thesis will have open access and can be viewed and downloaded publicly as soon as possible.
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