Shugar, Daniel H.Sharp, Meghan2021-09-282021-09-282021-09Sharp, M. (2021). Amplification of surface topography during surges of Tweedsmuir Glacier (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.http://hdl.handle.net/1880/113988The recent development and improvement of remote sensing sensor technology and processing techniques has expanded the spatiotemporal basis of glacier monitoring, where in situ measurements are limited. With these developments, this thesis aims to identify periods of enhanced basal sliding from glacier surface digital elevation models (DEMs) of Tweedsmuir Glacier, a surge-type glacier in the St. Elias Mountains, Canada. We divide this problem into two study objectives: 1) reconstruct surface elevations on a multidecadal timescale, and 2) identify signatures of surges in the surface topography of Tweedsmuir Glacier. Structure-from-Motion with Multiview Stereo photogrammetry, an emerging technique in glaciology, was employed to reconstruct surface DEMs using historical imagery from 1950 to 1987. The photogrammetric DEMs were combined with more recent satellite DEMs acquired between 2000 and 2018 to calculate surface elevation changes throughout two complete surge cycles. An increase in surface elevation is observed in the terminus region between 1950 and 1969, which is interpreted to represent a previously undocumented surge in the early years of the interval. In addition, surface-elevation lowering along longitudinal profiles between surge cycles indicates that Tweedsmuir Glacier has sustained a net negative mass balance on an inter-surge timescale. To address the second objective, variations in surface topography along nine longitudinal profiles were quantified using a one-dimensional Fourier transform and continuous wavelet transform. The glacier surface following known surges (1974, 2010) and within an active surge phase (2007) exhibits an increase in amplitude of surface features with longitudinal wavelengths between 3 to 8 ice thicknesses. Subsequently, the amplitude of surface topography decreased during both quiescent phases (1987-2000, 2010-2018). The amplified wavelengths are in agreement with previous theoretical work that suggests that these features may represent spatial variability in basal topography or the basal slip ratio. Overall, spectral analysis of glacier surface DEMs may be developed to estimate basal slip ratios remotely, which are inherently difficult to measure directly and a poorly constrained parameter in modern ice flow models.engUniversity 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.GlacierWavelet TransformFourier TransformPhotogrammetryStructure from MotionGeographyGeologyGeophysicsPhysical GeographyRemote Sensingmaster thesishttp://dx.doi.org/10.11575/PRISM/39300