Assessment of Arctic sea ice properties during advanced melt using C- and L-band polarimetric synthetic aperture radar

Simple item page
dc.contributor.authorTavri, Aikaterini
dc.date.accessioned2024-01-04T01:32:56Z
dc.date.available2024-01-04T01:32:56Z
dc.date.copyright2023en_US
dc.date.issued2024-01-03
dc.degree.departmentDepartment of Geography
dc.degree.levelDoctor of Philosophy Ph.D.en_US
dc.description.abstractOver recent decades, there have been significant changes in Arctic sea ice, marked by a shift from thicker to thinner ice, and reductions in extent and volume. These changes, along with extended melt seasons, have accelerated sea ice melt and the ice-albedo feedback. This dissertation leverages Synthetic Aperture Radar (SAR) to analyze sea ice dynamics and thermodynamics at various scales. Focusing on the advanced melt season, this dissertation examines the relationships between sea ice geophysical properties and SAR backscatter signatures at C- and L-bands. Our analysis uses RADARSAT-2 (C-band) and ALOS-2/PALSAR-2 (L-band) imagery in different polarimetric modes to assess sea ice type separability and the effects of incidence angle and melt ponds on backscatter. We discover that C-band SAR is more effective early in the melt season, while L-band SAR provides clearer delineation of ice features later in the season. Additionally, the co-pol ratio (VV/HH) was found to be a consistent indicator of the melt ponds for FYI, despite environmental changes, such as wind-roughened melt ponds, for both frequencies and incidence angles in the near and far range. Utilizing our findings, we developed a dual frequency, dual-incidence angle sea ice classification approach using a random forest classifier. We achieved over 70% accuracy in sea ice type classification, validated by airborne measurements. This research underscores the value of a dual-frequency approach in improving sea ice classification, particularly for first-year and multi-year ice during advanced melt stages, while considering the evolution of deformed ice types in the advanced melt season. The findings contribute significantly to climate studies and operational services and are pertinent to future dual-frequency SAR missions.en_US
dc.description.scholarlevelGraduateen_US
dc.identifier.urihttp://hdl.handle.net/1828/15780
dc.languageEnglisheng
dc.language.isoenen_US
dc.rightsAvailable to the World Wide Weben_US
dc.subjectsea iceen_US
dc.subjectSARen_US
dc.subjectC-banden_US
dc.subjectL-banden_US
dc.subjectadvanced melten_US
dc.subjectcompact polarimetryen_US
dc.subjectfull polarimetryen_US
dc.subjectRADARSAT Constellation Missionen_US
dc.subjectseparabilityen_US
dc.subjectmelt seasonen_US
dc.subjectclassificationen_US
dc.subjectdeformed iceen_US
dc.subjectlandfast iceen_US
dc.titleAssessment of Arctic sea ice properties during advanced melt using C- and L-band polarimetric synthetic aperture radaren_US
dc.typeThesisen_US

Files

Original bundle
Now showing 1 - 1 of 1
Thumbnail Image
Name:
Disseration_Tavri_Aikaterini_2023.pdf
Size:
5.79 MB
Format:
Adobe Portable Document Format
Description:
PhD Dissertation
Download
License bundle
Now showing 1 - 1 of 1
No Thumbnail Available
Name:
license.txt
Size:
2 KB
Format:
Item-specific license agreed upon to submission
Description:
Download

Collections

Electronic Theses and Dissertations (ETD)
 
University of Victoria Libraries

We acknowledge and respect the Lək̓ʷəŋən (Songhees and Esquimalt) Peoples on whose territory the university stands, and the Lək̓ʷəŋən and W̱SÁNEĆ Peoples whose historical relationships with the land continue to this day.