Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra

In the subarctic tundra, soil moisture information can benefit permafrost monitoring and ecological studies, but fine-scale remote sensing approaches are lacking. We explore the suitability of C-band SAR, paying attention to two challenges soil moisture retrieval faces. First, the microtopography an...

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Main Authors: Zwieback, Simon, Berg, Aaron
Format: Report
Language:unknown
Published: EarthArXiv 2018
Subjects:
Online Access:https://dx.doi.org/10.17605/osf.io/kp5xd
https://eartharxiv.org/kp5xd/
id ftdatacite:10.17605/osf.io/kp5xd
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spelling ftdatacite:10.17605/osf.io/kp5xd 2023-05-15T17:58:04+02:00 Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra Zwieback, Simon Berg, Aaron 2018 https://dx.doi.org/10.17605/osf.io/kp5xd https://eartharxiv.org/kp5xd/ unknown EarthArXiv CC-By Attribution 4.0 International Physical Sciences and Mathematics Environmental Sciences Environmental Monitoring Preprint Text article-journal ScholarlyArticle 2018 ftdatacite https://doi.org/10.17605/osf.io/kp5xd 2021-11-05T12:55:41Z In the subarctic tundra, soil moisture information can benefit permafrost monitoring and ecological studies, but fine-scale remote sensing approaches are lacking. We explore the suitability of C-band SAR, paying attention to two challenges soil moisture retrieval faces. First, the microtopography and the heterogeneous organic soils impart unique microwave scattering properties, even in absence of noteworthy shrub cover. Empirically, we find the polarimetric response is highly random (entropies > 0.7). The randomness precludes the application of purely polarimetric approaches to soil moisture estimation, as it causes a tailor-made decomposition to break down. For comparison, the L-band scattering response is much more surface-like (entropies of 0.1-0.2), also in terms of its angular characteristics. The second challenge concerns the large spatial but small temporal variability of soil moisture. Accordingly, the Radarsat-2 C-band backscatter has a limited dynamic range (approx. 2 dB). However, contrary to polarimetric indicators, it shows a clear soil moisture signal. To account for the small dynamic range while retaining a 100 m spatial resolution, we embed an empirical time-series model in a Bayesian framework. This framework adaptively pools information from neighboring grid cells, thus increasing the precision. The retrieved soil moisture index achieves correlations of 0.3-0.5 with in-situ network data and, upon calibration, RMSEs of < 0.04 m3m-3. As this approach is applicable to Sentinel-1 data, it can potentially provide frequent soil moisture estimates across large regions. In the long term, L-band data hold greater promise for operational retrievals. Report permafrost Subarctic Tundra DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Physical Sciences and Mathematics
Environmental Sciences
Environmental Monitoring
spellingShingle Physical Sciences and Mathematics
Environmental Sciences
Environmental Monitoring
Zwieback, Simon
Berg, Aaron
Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
topic_facet Physical Sciences and Mathematics
Environmental Sciences
Environmental Monitoring
description In the subarctic tundra, soil moisture information can benefit permafrost monitoring and ecological studies, but fine-scale remote sensing approaches are lacking. We explore the suitability of C-band SAR, paying attention to two challenges soil moisture retrieval faces. First, the microtopography and the heterogeneous organic soils impart unique microwave scattering properties, even in absence of noteworthy shrub cover. Empirically, we find the polarimetric response is highly random (entropies > 0.7). The randomness precludes the application of purely polarimetric approaches to soil moisture estimation, as it causes a tailor-made decomposition to break down. For comparison, the L-band scattering response is much more surface-like (entropies of 0.1-0.2), also in terms of its angular characteristics. The second challenge concerns the large spatial but small temporal variability of soil moisture. Accordingly, the Radarsat-2 C-band backscatter has a limited dynamic range (approx. 2 dB). However, contrary to polarimetric indicators, it shows a clear soil moisture signal. To account for the small dynamic range while retaining a 100 m spatial resolution, we embed an empirical time-series model in a Bayesian framework. This framework adaptively pools information from neighboring grid cells, thus increasing the precision. The retrieved soil moisture index achieves correlations of 0.3-0.5 with in-situ network data and, upon calibration, RMSEs of < 0.04 m3m-3. As this approach is applicable to Sentinel-1 data, it can potentially provide frequent soil moisture estimates across large regions. In the long term, L-band data hold greater promise for operational retrievals.
format Report
author Zwieback, Simon
Berg, Aaron
author_facet Zwieback, Simon
Berg, Aaron
author_sort Zwieback, Simon
title Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
title_short Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
title_full Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
title_fullStr Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
title_full_unstemmed Fine-Scale SAR Soil Moisture Estimation in the Subarctic Tundra
title_sort fine-scale sar soil moisture estimation in the subarctic tundra
publisher EarthArXiv
publishDate 2018
url https://dx.doi.org/10.17605/osf.io/kp5xd
https://eartharxiv.org/kp5xd/
genre permafrost
Subarctic
Tundra
genre_facet permafrost
Subarctic
Tundra
op_rights CC-By Attribution 4.0 International
op_doi https://doi.org/10.17605/osf.io/kp5xd
_version_ 1766166591359156224