Thermal Regime of Two Talus Slopes in Northwestern Ontario
Public Deposited- Resource Type
- Creator
- Abstract
This thesis investigates the thermal regimes of two talus slopes near lakes Superior and Nipigon, Ontario. Mean annual air temperatures in the region are periglacial, but little work has been done on whether permafrost or anomalously cold ground exist in blocky materials in the area. Air and internal talus temperatures were recorded, and the dimensions of the rocks and the temperature at the base of the snow were measured. Internal talus temperatures increased with elevation. The talus slopes at both Doghead Mountain and Ouimet Canyon experienced an unstable thermal regime with significant convection during the winter, and a stable, stratified thermal regime with significant conduction during the summer. The summertime thermal regimes of the lower sections of the slopes were dominated by zero curtains. Thaw completion depended on the length of the zero curtain, and thus on the amount of ice in the talus. Permafrost was found in Ouimet Canyon.
- Subject
- Language
- Publisher
- Thesis Degree Level
- Thesis Degree Name
- Thesis Degree Discipline
- Identifier
- Rights Notes
Copyright © 2019 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner.
- Date Created
- 2019
Relations
- In Collection:
Items
Thumbnail | Title | Date Uploaded | Visibility | Actions |
---|---|---|---|---|
bishop-legowski-thermalregimeoftwotalusslopesinnorthwestern.pdf | 2023-05-05 | Public | Download |