Polarimetric C-band microwave scattering from winter first-year sea ice ridges

dc.contributor.authorShields, Megan
dc.contributor.examiningcommitteePapakyriakou, Tim (Environment and Geography) Cooley, Paul (North/South Consultants Inc.)en_US
dc.contributor.supervisorBarber, David (Environment and Geography)en_US
dc.date.accessioned2015-06-04T20:11:14Z
dc.date.available2015-06-04T20:11:14Z
dc.date.issued2015-06-04
dc.degree.disciplineEnvironment and Geographyen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractMicrowave scattering from sea ice ridges is poorly understood. This thesis aims to improve the current knowledge on in situ C-band microwave scattering from first-year sea ice (FYI) pressure ridges during winter, and how C-band backscatter can vary with changes to radar and target parameters. Remotely sensed data of ridged ice were collected at a sea ice mesocosm using a LiDAR laser scanner and a fully-polarimetric C-band scatterometer. Thesis results indicate that using an incidence angle between 30 and 50° and HV polarization will best enable distinguishing between smooth and ridged ice, while using an incidence angle of 40° and HV or HH polarization will best enable detecting variations in ridge height. Overall results indicate that a significant proportion of the variance in FYI snow-free ridge C-band backscatter can be explained by incidence angle, polarization, and ridge height, with almost 88% of the variability in backscatter attributed to ridge height.en_US
dc.description.noteOctober 2015en_US
dc.identifier.urihttp://hdl.handle.net/1993/30571
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.subjectMicrowavesen_US
dc.subjectLiDARen_US
dc.subjectRidgesen_US
dc.subjectSea Iceen_US
dc.subjectC-Banden_US
dc.subjectArcticen_US
dc.titlePolarimetric C-band microwave scattering from winter first-year sea ice ridgesen_US
dc.typemaster thesisen_US
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