Analysis of MODIS-Aqua imagery to determine spring phytoplankton phenology in the Strait of Georgia, Canada

dc.contributor.authorCarswell, Tyson Kyle
dc.contributor.supervisorCosta, Maycira
dc.date.accessioned2015-12-21T18:57:05Z
dc.date.available2015-12-21T18:57:05Z
dc.date.copyright2015en_US
dc.date.issued2015-12-21
dc.degree.departmentDepartment of Geographyen_US
dc.degree.levelMaster of Science M.Sc.en_US
dc.description.abstractThe goal of this research was to construct a time series of accurate chlorophyll-a concentration for the Strait of Georgia (SoG), Canada, using an improved atmospheric correction scheme and workflow for the Moderate Resolution Imaging Spectroradiometer AQUA (MODIS) satellite instrument to describe the chla dynamics and spring bloom phenology in the SoG. In situ radiometric samples were acquired via Aerosol Robotic Network (AERONET), and hyperspectral data collected from a Hyperspectral Surface Acquisition System (HyperSAS) to assess three potential atmospheric correction schemes. Water property samples including total suspended material (TSM), chromophoric dissolved organic matter (CDOM), and chlorophyll concentrations (chla) were collected to further assess atmospheric corrections and the applied ‘Ocean Color 3 Modis’ (OC3M) standard chlorophyll algorithm. Regression, Absolute percentage difference (APD), Relative Percentage difference (RPD), and Root mean squared error (RMSE) analysis revealed the most appropriate method to be the ‘Management Unit of the North Seas Mathematical Models’ (MUMM) using the shortwave infrared spectrum (SWIR) to determine NIR-derived aerosol model. This method was used to construct a time series (July 2002-June 2014) of daily chlorophyll maps for all available imagery. Files were spatially binned into 8-day composites for the North and Central SoG where a modified threshold-based definition was used to determine the start of the spring phytoplankton bloom period, as well as timing of maxima and duration of the largest spring bloom. Results indicate Central SoG start dates range from late February to late April, with an average start date at the last week of March. These results compare favorably to Hindcast predictive modelling of bloom start dates. The Northern SoG bloom phenology starts on average 9 days earlier, and experiences lower chlorophyll-a magnitudes. Hierarchical clustering with correlation similarity of spring seasons indicate 2008 and 2007 were anomalous, while 2009 and 2012 were the most correlated for blooms occurring in the spring season.en_US
dc.description.proquestcode0366en_US
dc.description.proquestcode0416en_US
dc.description.proquestcode0752en_US
dc.description.proquestcode0368en_US
dc.description.proquestemailcarswell@uvic.caen_US
dc.description.scholarlevelGraduateen_US
dc.identifier.urihttp://hdl.handle.net/1828/6967
dc.languageEnglisheng
dc.language.isoenen_US
dc.rightsAvailable to the World Wide Weben_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/2.5/ca/*
dc.subjectChlorophyllen_US
dc.subjectOceanographyen_US
dc.subjectStrait of Georgiaen_US
dc.subjectMODISen_US
dc.subjectRemote sensingen_US
dc.subjectPhenologyen_US
dc.subjectPhytoplanktonen_US
dc.subjectGeographyen_US
dc.subjectFisheriesen_US
dc.subjectopticsen_US
dc.subjectAERONETen_US
dc.titleAnalysis of MODIS-Aqua imagery to determine spring phytoplankton phenology in the Strait of Georgia, Canadaen_US
dc.typeThesisen_US

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