Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset

Synthetic aperature radar (SAR) remote sensing offers a technology potentially capable of capturing information about soil moisture at high spatial and temporal resolutions. This method has been shown to be effective in lower latitude environments however there has been a lack of investigation in ar...

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Main Authors: Humphrey, Rachel E., Adams, Justin R., Berg, Aaron A., Marsh, Philip
Other Authors: Soil Moisture Research Group. Department of Geography. College of Social and Applied Human Sciences. University of Guelph.
Format: Other/Unknown Material
Language:English
Published: Borealis 2014
Subjects:
Ice
Online Access:https://doi.org/10.5683/SP/GSFLE3
id ftborealisdata:doi:10.5683/SP/GSFLE3
record_format openpolar
spelling ftborealisdata:doi:10.5683/SP/GSFLE3 2023-05-15T14:44:36+02:00 Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset Humphrey, Rachel E. Adams, Justin R. Berg, Aaron A. Marsh, Philip Soil Moisture Research Group. Department of Geography. College of Social and Applied Human Sciences. University of Guelph. 2014-06-29 https://doi.org/10.5683/SP/GSFLE3 English eng Borealis https://doi.org/10.5683/SP/GSFLE3 Earth and Environmental Sciences soil moisture soil freeze/thaw tundra depth of soil freeze permafrost ice table hydrological processes active layer scaling Experimental 2014 ftborealisdata https://doi.org/10.5683/SP/GSFLE3 2022-10-10T05:50:33Z Synthetic aperature radar (SAR) remote sensing offers a technology potentially capable of capturing information about soil moisture at high spatial and temporal resolutions. This method has been shown to be effective in lower latitude environments however there has been a lack of investigation in arctic environments, particularly in organic permafrost soils. A preliminary analysis was performed at Trail Valley Creek, Northwest Territories, where an investigation of the statistical spatial variability of soil moisture and processes controlling soil moisture was completed. Both of these are key steps required for modeling soil moisture retrievals from satellites. Second, an assessment of the sensitivity of RADARSAT-2 backscatter to surface soil moisture conditions was completed to examine whether SAR can provide a much needed method to map soil moisture across the arctic. Results showed a strong relationship between backscatter and soil moisture (R2 =0.688) and demonstrate the potential for SAR soil moisture retrieval in arctic ecosystems. Other/Unknown Material Arctic Ice Northwest Territories permafrost Tundra Borealis Arctic Northwest Territories Canada Valley Creek ENVELOPE(-138.324,-138.324,63.326,63.326) Trail Valley Creek ENVELOPE(-133.415,-133.415,68.772,68.772)
institution Open Polar
collection Borealis
op_collection_id ftborealisdata
language English
topic Earth and Environmental Sciences
soil moisture
soil freeze/thaw
tundra
depth of soil freeze
permafrost
ice table
hydrological processes
active layer
scaling
spellingShingle Earth and Environmental Sciences
soil moisture
soil freeze/thaw
tundra
depth of soil freeze
permafrost
ice table
hydrological processes
active layer
scaling
Humphrey, Rachel E.
Adams, Justin R.
Berg, Aaron A.
Marsh, Philip
Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
topic_facet Earth and Environmental Sciences
soil moisture
soil freeze/thaw
tundra
depth of soil freeze
permafrost
ice table
hydrological processes
active layer
scaling
description Synthetic aperature radar (SAR) remote sensing offers a technology potentially capable of capturing information about soil moisture at high spatial and temporal resolutions. This method has been shown to be effective in lower latitude environments however there has been a lack of investigation in arctic environments, particularly in organic permafrost soils. A preliminary analysis was performed at Trail Valley Creek, Northwest Territories, where an investigation of the statistical spatial variability of soil moisture and processes controlling soil moisture was completed. Both of these are key steps required for modeling soil moisture retrievals from satellites. Second, an assessment of the sensitivity of RADARSAT-2 backscatter to surface soil moisture conditions was completed to examine whether SAR can provide a much needed method to map soil moisture across the arctic. Results showed a strong relationship between backscatter and soil moisture (R2 =0.688) and demonstrate the potential for SAR soil moisture retrieval in arctic ecosystems.
author2 Soil Moisture Research Group. Department of Geography. College of Social and Applied Human Sciences. University of Guelph.
format Other/Unknown Material
author Humphrey, Rachel E.
Adams, Justin R.
Berg, Aaron A.
Marsh, Philip
author_facet Humphrey, Rachel E.
Adams, Justin R.
Berg, Aaron A.
Marsh, Philip
author_sort Humphrey, Rachel E.
title Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
title_short Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
title_full Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
title_fullStr Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
title_full_unstemmed Soil moisture over Canadian Arctic tundra: Trail Valley Creek, Northwest Territories [Canada] dataset
title_sort soil moisture over canadian arctic tundra: trail valley creek, northwest territories [canada] dataset
publisher Borealis
publishDate 2014
url https://doi.org/10.5683/SP/GSFLE3
long_lat ENVELOPE(-138.324,-138.324,63.326,63.326)
ENVELOPE(-133.415,-133.415,68.772,68.772)
geographic Arctic
Northwest Territories
Canada
Valley Creek
Trail Valley Creek
geographic_facet Arctic
Northwest Territories
Canada
Valley Creek
Trail Valley Creek
genre Arctic
Ice
Northwest Territories
permafrost
Tundra
genre_facet Arctic
Ice
Northwest Territories
permafrost
Tundra
op_relation https://doi.org/10.5683/SP/GSFLE3
op_doi https://doi.org/10.5683/SP/GSFLE3
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