An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.

A field experiment, involving direct manipulation of surface microclimate, was undertaken in the continuous permafrost zone to examine the influence of climatic fluctuations on solifluction rates and movements throughout the active layer. Movements and soil temperature were measured continuously fro...

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Main Author: Clarke, Shawne Arianne.
Format: Thesis
Language:unknown
Published: Université d'Ottawa / University of Ottawa 1998
Subjects:
Online Access:https://dx.doi.org/10.20381/ruor-10308
http://www.ruor.uottawa.ca/handle/10393/4538
id ftdatacite:10.20381/ruor-10308
record_format openpolar
spelling ftdatacite:10.20381/ruor-10308 2023-05-15T16:05:55+02:00 An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories. Clarke, Shawne Arianne. 1998 https://dx.doi.org/10.20381/ruor-10308 http://www.ruor.uottawa.ca/handle/10393/4538 unknown Université d'Ottawa / University of Ottawa Physical Geography. Text Thesis article-journal ScholarlyArticle 1998 ftdatacite https://doi.org/10.20381/ruor-10308 2021-11-05T12:55:41Z A field experiment, involving direct manipulation of surface microclimate, was undertaken in the continuous permafrost zone to examine the influence of climatic fluctuations on solifluction rates and movements throughout the active layer. Movements and soil temperature were measured continuously from 1993-1997 using five electro-mechanical meters and thermocouple cables on an 8$\sp\circ$ colluvial slope in Hot Weather Creek valley, Ellesmere Island. Natural variation of movement among the years and the meters was measured until summer of 1996 when surface climatic treatments (surface warming, wetting, a combination of these two, and cooling) were performed. The longer-term effects of the treatments were monitored until August 1997. Near-surface measurements alone do not provide an accurate picture of solifluction in areas with two-sided freezing ("cold" permafrost) because there can be substantial variation in movement rates at depth. In addition, multi-year average rates potentially hide a considerable range of annual variability and do not allow for the examination of a relationship between climatic fluctuations and annual movement. (Abstract shortened by UMI.) Thesis Ellesmere Island Fosheim Peninsula Northwest Territories permafrost DataCite Metadata Store (German National Library of Science and Technology) Ellesmere Island Fosheim Peninsula ENVELOPE(-83.749,-83.749,79.669,79.669) Hot Weather Creek ENVELOPE(-84.466,-84.466,79.935,79.935) Northwest Territories
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Physical Geography.
spellingShingle Physical Geography.
Clarke, Shawne Arianne.
An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
topic_facet Physical Geography.
description A field experiment, involving direct manipulation of surface microclimate, was undertaken in the continuous permafrost zone to examine the influence of climatic fluctuations on solifluction rates and movements throughout the active layer. Movements and soil temperature were measured continuously from 1993-1997 using five electro-mechanical meters and thermocouple cables on an 8$\sp\circ$ colluvial slope in Hot Weather Creek valley, Ellesmere Island. Natural variation of movement among the years and the meters was measured until summer of 1996 when surface climatic treatments (surface warming, wetting, a combination of these two, and cooling) were performed. The longer-term effects of the treatments were monitored until August 1997. Near-surface measurements alone do not provide an accurate picture of solifluction in areas with two-sided freezing ("cold" permafrost) because there can be substantial variation in movement rates at depth. In addition, multi-year average rates potentially hide a considerable range of annual variability and do not allow for the examination of a relationship between climatic fluctuations and annual movement. (Abstract shortened by UMI.)
format Thesis
author Clarke, Shawne Arianne.
author_facet Clarke, Shawne Arianne.
author_sort Clarke, Shawne Arianne.
title An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
title_short An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
title_full An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
title_fullStr An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
title_full_unstemmed An experimental study on the influence of climatic fluctuations on solifluction, Fosheim Peninsula, Ellesmere Island, Northwest Territories.
title_sort experimental study on the influence of climatic fluctuations on solifluction, fosheim peninsula, ellesmere island, northwest territories.
publisher Université d'Ottawa / University of Ottawa
publishDate 1998
url https://dx.doi.org/10.20381/ruor-10308
http://www.ruor.uottawa.ca/handle/10393/4538
long_lat ENVELOPE(-83.749,-83.749,79.669,79.669)
ENVELOPE(-84.466,-84.466,79.935,79.935)
geographic Ellesmere Island
Fosheim Peninsula
Hot Weather Creek
Northwest Territories
geographic_facet Ellesmere Island
Fosheim Peninsula
Hot Weather Creek
Northwest Territories
genre Ellesmere Island
Fosheim Peninsula
Northwest Territories
permafrost
genre_facet Ellesmere Island
Fosheim Peninsula
Northwest Territories
permafrost
op_doi https://doi.org/10.20381/ruor-10308
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