File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: An Integrated Time-Series Relative Soil Moisture Monitoring Method Based on a SAR Backscattering Model

TitleAn Integrated Time-Series Relative Soil Moisture Monitoring Method Based on a SAR Backscattering Model
Authors
KeywordsBackscatter
Climate change
Landsat
Landsat 8
Moisture
Monitoring
relative surface soil moisture
Scattering
Sentinel-1
Sentinel-1A/B
Soil moisture
Synthetic aperture radar
Synthetic aperture radar (SAR)
time-series retrieval
Vegetation mapping
Issue Date13-Jun-2024
PublisherInstitute of Electrical and Electronics Engineers
Citation
IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2024, p. 1-22 How to Cite?
AbstractTime-series monitoring of relative surface soil moisture (RSSM) with remote sensing observation is crucial for guiding agricultural irrigation management and monitoring global climate change. However, existing SAR soil moisture retrieval algorithms suffer from insufficient decoupling of surface scattering characteristics and poor RSSM time-series monitoring capabilities. Therefore, this paper proposes an integrated time-series relative soil moisture monitoring method based on a SAR backscattering model (SBM). Initially, the SBM is introduced, categorizing land cover into built-up areas, water bodies, vegetation-covered areas, and soil. Addressing the inconsistency in spatiotemporal resolution between optical vegetation indices and SAR data, we establish a unique SAR water cloud model (SWCM) in conjunction with the dual-polarization SAR vegetation index (DRVIs). By employing the SWCM to eliminate vegetation's influence, a high-quality soil backscatter coefficient is obtained. Ultimately, the dry and wet reference values of soil backscatter are calculated to retrieve the relative RSSM time series. Based on Sentinel-1 data, we select three representative experimental areas, namely the Qarhan Salt Lake in dry regions, the Tibetan Plateau Naqu in high-cold regions, and Inner Mongolia Xilinhot in grassland regions, conducting RSSM spatiotemporal monitoring for three years. Experimental results demonstrate that the RSSM exhibits seasonal variations in these three regions. The correlation coefficient between the RSSM monitoring results and the in-situ data exceeds 0.64, with a maximum of 0.84. Consequently, the proposed method underscores the advantages of simplicity in parameters, high estimation precision, and robust adaptability, thereby augmenting the potential for large-scale global monitoring applications.
Persistent Identifierhttp://hdl.handle.net/10722/348141
ISSN
2023 Impact Factor: 4.7
2023 SCImago Journal Rankings: 1.434

 

DC FieldValueLanguage
dc.contributor.authorBao, Xin-
dc.contributor.authorZhang, Rui-
dc.contributor.authorHe, Xu-
dc.contributor.authorShama, Age-
dc.contributor.authorYin, Gaofei-
dc.contributor.authorChen, Jie-
dc.contributor.authorZhang, Hongsheng-
dc.contributor.authorLiu, Guoxiang-
dc.date.accessioned2024-10-05T00:30:47Z-
dc.date.available2024-10-05T00:30:47Z-
dc.date.issued2024-06-13-
dc.identifier.citationIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2024, p. 1-22-
dc.identifier.issn1939-1404-
dc.identifier.urihttp://hdl.handle.net/10722/348141-
dc.description.abstractTime-series monitoring of relative surface soil moisture (RSSM) with remote sensing observation is crucial for guiding agricultural irrigation management and monitoring global climate change. However, existing SAR soil moisture retrieval algorithms suffer from insufficient decoupling of surface scattering characteristics and poor RSSM time-series monitoring capabilities. Therefore, this paper proposes an integrated time-series relative soil moisture monitoring method based on a SAR backscattering model (SBM). Initially, the SBM is introduced, categorizing land cover into built-up areas, water bodies, vegetation-covered areas, and soil. Addressing the inconsistency in spatiotemporal resolution between optical vegetation indices and SAR data, we establish a unique SAR water cloud model (SWCM) in conjunction with the dual-polarization SAR vegetation index (DRVIs). By employing the SWCM to eliminate vegetation's influence, a high-quality soil backscatter coefficient is obtained. Ultimately, the dry and wet reference values of soil backscatter are calculated to retrieve the relative RSSM time series. Based on Sentinel-1 data, we select three representative experimental areas, namely the Qarhan Salt Lake in dry regions, the Tibetan Plateau Naqu in high-cold regions, and Inner Mongolia Xilinhot in grassland regions, conducting RSSM spatiotemporal monitoring for three years. Experimental results demonstrate that the RSSM exhibits seasonal variations in these three regions. The correlation coefficient between the RSSM monitoring results and the in-situ data exceeds 0.64, with a maximum of 0.84. Consequently, the proposed method underscores the advantages of simplicity in parameters, high estimation precision, and robust adaptability, thereby augmenting the potential for large-scale global monitoring applications.-
dc.languageeng-
dc.publisherInstitute of Electrical and Electronics Engineers-
dc.relation.ispartofIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.subjectBackscatter-
dc.subjectClimate change-
dc.subjectLandsat-
dc.subjectLandsat 8-
dc.subjectMoisture-
dc.subjectMonitoring-
dc.subjectrelative surface soil moisture-
dc.subjectScattering-
dc.subjectSentinel-1-
dc.subjectSentinel-1A/B-
dc.subjectSoil moisture-
dc.subjectSynthetic aperture radar-
dc.subjectSynthetic aperture radar (SAR)-
dc.subjecttime-series retrieval-
dc.subjectVegetation mapping-
dc.titleAn Integrated Time-Series Relative Soil Moisture Monitoring Method Based on a SAR Backscattering Model-
dc.typeArticle-
dc.identifier.doi10.1109/JSTARS.2024.3413673-
dc.identifier.scopuseid_2-s2.0-85196061893-
dc.identifier.spage1-
dc.identifier.epage22-
dc.identifier.eissn2151-1535-
dc.identifier.issnl1939-1404-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats