Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska
Despite their relatively small ice volume, mountain glaciers contributed nearly one third of global sea level rise since 2000, with one of the largest total mass loss rates (73 ± 17 Gt a-1) occurring in the Yukon-Alaska region. However, there is uncertainty surrounding how ice dynamics are being aff...
Main Author: | |
---|---|
Other Authors: | |
Format: | Thesis |
Language: | English |
Published: |
Université d'Ottawa / University of Ottawa
2024
|
Subjects: | |
Online Access: | http://hdl.handle.net/10393/45826 https://doi.org/10.20381/ruor-30030 |
id |
ftunivottawa:oai:ruor.uottawa.ca:10393/45826 |
---|---|
record_format |
openpolar |
spelling |
ftunivottawa:oai:ruor.uottawa.ca:10393/45826 2024-02-11T10:03:59+01:00 Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska Main, Brittany Copland, Luke 2024-01-11 application/pdf http://hdl.handle.net/10393/45826 https://doi.org/10.20381/ruor-30030 en eng Université d'Ottawa / University of Ottawa http://hdl.handle.net/10393/45826 http://dx.doi.org/10.20381/ruor-30030 glaciology surging glaciers ice dynamics remote sensing proglacial lakes glacier velocities Thesis 2024 ftunivottawa https://doi.org/10.20381/ruor-30030 2024-01-14T00:00:12Z Despite their relatively small ice volume, mountain glaciers contributed nearly one third of global sea level rise since 2000, with one of the largest total mass loss rates (73 ± 17 Gt a-1) occurring in the Yukon-Alaska region. However, there is uncertainty surrounding how ice dynamics are being affected by such losses and whether glacier flow instabilities, such as surges, are changing in a warming climate. The St. Elias Mountains contain a major cluster of surge-type glaciers, yet a detailed analysis of their characteristics, including surge frequency, morphology, magnitude, and propensity over time has not been undertaken on a regional basis. This thesis presents a review of surging behaviour and an updated surge event inventory in the St. Elias Mountains, and quantifies the processes influencing both surging and non-surging glacier velocity variability using a variety of remote sensing and field measurements. An updated inventory of surge-type glaciers and observed surge events (1874-2023), compiled from existing inventories, recently published articles, and velocity analysis, is used to analyze the characteristics of surge-type glaciers and velocity patterns during surge events. The modern (1985-2023) trends in annual, winter and summer velocities of selected surge-type glaciers is then used to classify dynamic instability events into 4 categories. While 231 glaciers were classified as surge-type, only 42 were observed to have experienced rapid velocity events over the period 1985-2023, through either direct measurements or remote sensing observations. For glaciers with observed rapid velocity events, these predominantly fall into two categories: Alaskan-style surges with short active and quiescent phases, and glacier pulses, which are velocity accelerations that are limited in both magnitude and extent. An unnamed former tributary to Kluane Glacier underwent a dramatic surge from 2013-18. Using a combination of air photos, remote sensing and field observations, the characteristics and changes of ‘Little ... Thesis glacier glaciers Alaska Yukon uO Research (University of Ottawa - uOttawa) Kluane Glacier ENVELOPE(-139.318,-139.318,60.883,60.883) Yukon |
institution |
Open Polar |
collection |
uO Research (University of Ottawa - uOttawa) |
op_collection_id |
ftunivottawa |
language |
English |
topic |
glaciology surging glaciers ice dynamics remote sensing proglacial lakes glacier velocities |
spellingShingle |
glaciology surging glaciers ice dynamics remote sensing proglacial lakes glacier velocities Main, Brittany Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
topic_facet |
glaciology surging glaciers ice dynamics remote sensing proglacial lakes glacier velocities |
description |
Despite their relatively small ice volume, mountain glaciers contributed nearly one third of global sea level rise since 2000, with one of the largest total mass loss rates (73 ± 17 Gt a-1) occurring in the Yukon-Alaska region. However, there is uncertainty surrounding how ice dynamics are being affected by such losses and whether glacier flow instabilities, such as surges, are changing in a warming climate. The St. Elias Mountains contain a major cluster of surge-type glaciers, yet a detailed analysis of their characteristics, including surge frequency, morphology, magnitude, and propensity over time has not been undertaken on a regional basis. This thesis presents a review of surging behaviour and an updated surge event inventory in the St. Elias Mountains, and quantifies the processes influencing both surging and non-surging glacier velocity variability using a variety of remote sensing and field measurements. An updated inventory of surge-type glaciers and observed surge events (1874-2023), compiled from existing inventories, recently published articles, and velocity analysis, is used to analyze the characteristics of surge-type glaciers and velocity patterns during surge events. The modern (1985-2023) trends in annual, winter and summer velocities of selected surge-type glaciers is then used to classify dynamic instability events into 4 categories. While 231 glaciers were classified as surge-type, only 42 were observed to have experienced rapid velocity events over the period 1985-2023, through either direct measurements or remote sensing observations. For glaciers with observed rapid velocity events, these predominantly fall into two categories: Alaskan-style surges with short active and quiescent phases, and glacier pulses, which are velocity accelerations that are limited in both magnitude and extent. An unnamed former tributary to Kluane Glacier underwent a dramatic surge from 2013-18. Using a combination of air photos, remote sensing and field observations, the characteristics and changes of ‘Little ... |
author2 |
Copland, Luke |
format |
Thesis |
author |
Main, Brittany |
author_facet |
Main, Brittany |
author_sort |
Main, Brittany |
title |
Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
title_short |
Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
title_full |
Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
title_fullStr |
Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
title_full_unstemmed |
Glacier Velocities and Ice Dynamics in the St. Elias Mountains, Yukon-Alaska |
title_sort |
glacier velocities and ice dynamics in the st. elias mountains, yukon-alaska |
publisher |
Université d'Ottawa / University of Ottawa |
publishDate |
2024 |
url |
http://hdl.handle.net/10393/45826 https://doi.org/10.20381/ruor-30030 |
long_lat |
ENVELOPE(-139.318,-139.318,60.883,60.883) |
geographic |
Kluane Glacier Yukon |
geographic_facet |
Kluane Glacier Yukon |
genre |
glacier glaciers Alaska Yukon |
genre_facet |
glacier glaciers Alaska Yukon |
op_relation |
http://hdl.handle.net/10393/45826 http://dx.doi.org/10.20381/ruor-30030 |
op_doi |
https://doi.org/10.20381/ruor-30030 |
_version_ |
1790600391674560512 |