2009
DOI: 10.1109/tgrs.2008.2004711
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Using ENVISAT ASAR Global Mode Data for Surface Soil Moisture Retrieval Over Oklahoma, USA

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Cited by 179 publications
(189 citation statements)
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“…However, the correlations for ASAR against the in-situ measurements were generally weaker than for the ECV SM dataset, despite the scale gap between measurements being less pronounced. Similar findings were observed by Pathe et al (2009) when comparing ASAR-GM derived soil moisture to ERS scatterometer and in-situ soil moisture measurements (Oklahoma MESONET. Zribi et al (2014) also found similar results for ASAR-WS derived soil moisture (resampled to 1km resolution) and ERS/ASCAT products covering a semi-arid region in central Tunisia.…”
Section: Time Series Temporal Analysissupporting
confidence: 80%
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“…However, the correlations for ASAR against the in-situ measurements were generally weaker than for the ECV SM dataset, despite the scale gap between measurements being less pronounced. Similar findings were observed by Pathe et al (2009) when comparing ASAR-GM derived soil moisture to ERS scatterometer and in-situ soil moisture measurements (Oklahoma MESONET. Zribi et al (2014) also found similar results for ASAR-WS derived soil moisture (resampled to 1km resolution) and ERS/ASCAT products covering a semi-arid region in central Tunisia.…”
Section: Time Series Temporal Analysissupporting
confidence: 80%
“…This technique was originally developed for ERS scatterometer and Advanced Scatterometer (ASCAT) data but has been successfully adapted to both ASAR WS and GM data (e.g. Pathe et al, 2009;Mladenova et al, 2010;Doubková et al, 2012;Peters et al, 2012;Dostálová et al, 2014;Zribi et al, 2014). The TU Wien change detection approach derives relative changes in surface soil moisture and indirectly accounts for surface roughness and vegetation by assuming changes in these parameters will generally occur at longer temporal scales than soil moisture changes.…”
Section: Asar Soil Moisture Observationsmentioning
confidence: 99%
“…This is a collection of routines which manages SAR geocoding and radiometric calibration by calling other non-commercial and commercial software packages. By incorporating orbit information (DORIS (Doppler Orbitography and Radiopositioning Integrated by Satellite) orbit files) and digital elevation data (US Geological Survey GTOPO30 digital elevation model, improved by Shuttle Radar Topography Mission data), geocoded images were produced with sub-pixel accuracy (Park et al, 2011;Pathe et al, 2009). The data are resampled into a fixed 15 arcsec grid (datum WGS-84), within 0.5 • by 0.5 • tiles, to allow for efficient spatial and temporal analysis.…”
Section: Sar Data Processingmentioning
confidence: 99%
“…A challenge is the complexity of the interaction of the signal with the Earth surface. Water content of the near-surface soil contributes to the backscatter during unfrozen periods (Wagner et al, 1999;Pathe et al, Figure 1. Location of field sites with high-resolution land-coverbased soil organic carbon maps (Table 1) and area covered by the Circumpolar Arctic Vegetation Map (CAVM; Walker et al, 2002) as well as ENVISAT ASAR GM data (medium grey) 2009) as well as snow grains in the wintertime (Ulaby et al, 1982).…”
Section: Introductionmentioning
confidence: 99%
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