An Investigation of Active Microwave Remote Sensing of Summer Sea Ice in the Western Canadian Arctic

dc.contributor.authorWarner, Kerri
dc.contributor.examiningcommitteePapakyriakou, Tim (Environment and Geography) Sydor, Kevin (Manitoba Hydro)en_US
dc.contributor.supervisorBarber, David (Environment and Geography)en_US
dc.date.accessioned2012-12-18T15:15:46Z
dc.date.available2012-12-18T15:15:46Z
dc.date.issued2012-12-18
dc.degree.disciplineEnvironment and Geographyen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractActive microwave remote sensing is an important tool for classification of sea ice in polar regions. The aim of this research is to improve the understanding of microwave scattering that occurs during the advanced melt season, with a focus on multiyear ice (MYI). This was done using a combination of in situ C-Band scatterometer measurements, geophysical characteristics of ice, and Radarsat-2 data. Results indicate that it is difficult to differentiate between first year ice (FYI) and MYI during advanced melt but combinations of incidence angle and polarization exist that assist with this. It is known that the presence of liquid water governs microwave scattering, therefore further research investigating the variation of microwave backscattered signatures over a diurnal time period was conducted. These results indicate an inverse relationship between temperatures and microwave signatures. The overall results from this research show that summer MYI signatures are extremely variable and difficult to classify.en_US
dc.description.noteFebruary 2013en_US
dc.identifier.urihttp://hdl.handle.net/1993/13699
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.subjectactive microwave remote sensingen_US
dc.subjectsea iceen_US
dc.titleAn Investigation of Active Microwave Remote Sensing of Summer Sea Ice in the Western Canadian Arcticen_US
dc.typemaster thesisen_US
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