Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data

Various methods are used to determine soil moisture information from synthetic aperture radar (SAR) data, but none specific to High Arctic regions and their unique physical characteristics. This research presents a method for determining, at high spatial and temporal resolutions, surface soil moistu...

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Main Authors: Adam Collingwood, François Charbonneau, Chen Shang, Paul Treitz
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/5712046
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spelling doaj-96c1559fee4d40f89a9b1106ee8b496e2020-11-24T23:08:57ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/57120465712046Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR DataAdam Collingwood0François Charbonneau1Chen Shang2Paul Treitz3Department of Geography and Planning, Queen’s University, Kingston, ON, K7L 3N6, CanadaCanada Centre for Mapping and Earth Observation, Natural Resources Canada, 560 Rochester Street, Ottawa, ON, K1A 0E4, CanadaDepartment of Geography and Planning, Queen’s University, Kingston, ON, K7L 3N6, CanadaDepartment of Geography and Planning, Queen’s University, Kingston, ON, K7L 3N6, CanadaVarious methods are used to determine soil moisture information from synthetic aperture radar (SAR) data, but none specific to High Arctic regions and their unique physical characteristics. This research presents a method for determining, at high spatial and temporal resolutions, surface soil moisture and its changes through time in the Canadian High Arctic. An artificial neural network (ANN) is implemented using input variables derived from RADARSAT-2 SAR data and previously modelled surface roughness information. The model is applied to SAR data collected at various incidence angles and acquisition dates across two study sites on Melville Island, Nunavut. The model results in absolute soil moisture errors of approximately 15% (r2 = 0.46) for the primary study sites and 12% (r2 = 0.26) for the verification study area. The ANN model is accurate for modelling (i) the spatial distribution of soil moisture and (ii) the changes in moisture through time across the study areas, two characteristics that are very important for inputs to hydrologic or climate models. In addition, the models appear to be scalable when applied at coarser spatial resolutions, showing potential for large-area mapping or modelling.http://dx.doi.org/10.1155/2018/5712046
collection DOAJ
language English
format Article
sources DOAJ
author Adam Collingwood
François Charbonneau
Chen Shang
Paul Treitz
spellingShingle Adam Collingwood
François Charbonneau
Chen Shang
Paul Treitz
Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
Advances in Meteorology
author_facet Adam Collingwood
François Charbonneau
Chen Shang
Paul Treitz
author_sort Adam Collingwood
title Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
title_short Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
title_full Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
title_fullStr Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
title_full_unstemmed Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data
title_sort spatiotemporal variability of arctic soil moisture detected from high-resolution radarsat-2 sar data
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2018-01-01
description Various methods are used to determine soil moisture information from synthetic aperture radar (SAR) data, but none specific to High Arctic regions and their unique physical characteristics. This research presents a method for determining, at high spatial and temporal resolutions, surface soil moisture and its changes through time in the Canadian High Arctic. An artificial neural network (ANN) is implemented using input variables derived from RADARSAT-2 SAR data and previously modelled surface roughness information. The model is applied to SAR data collected at various incidence angles and acquisition dates across two study sites on Melville Island, Nunavut. The model results in absolute soil moisture errors of approximately 15% (r2 = 0.46) for the primary study sites and 12% (r2 = 0.26) for the verification study area. The ANN model is accurate for modelling (i) the spatial distribution of soil moisture and (ii) the changes in moisture through time across the study areas, two characteristics that are very important for inputs to hydrologic or climate models. In addition, the models appear to be scalable when applied at coarser spatial resolutions, showing potential for large-area mapping or modelling.
url http://dx.doi.org/10.1155/2018/5712046
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AT francoischarbonneau spatiotemporalvariabilityofarcticsoilmoisturedetectedfromhighresolutionradarsat2sardata
AT chenshang spatiotemporalvariabilityofarcticsoilmoisturedetectedfromhighresolutionradarsat2sardata
AT paultreitz spatiotemporalvariabilityofarcticsoilmoisturedetectedfromhighresolutionradarsat2sardata
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