2015
DOI: 10.5194/hess-19-4765-2015
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Evaluation of soil moisture downscaling using a simple thermal-based proxy – the REMEDHUS network (Spain) example

Abstract: Abstract. Soil moisture retrieved from satellite microwave remote sensing normally has spatial resolution on the order of tens of kilometers, which are too coarse for many regional hydrological applications such as agriculture monitoring and drought prediction. Therefore, various downscaling methods have been proposed to enhance the spatial resolution of satellite soil moisture products. The aim of this study is to investigate the validity and robustness of the simple vegetation temperature condition index (VT… Show more

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Cited by 61 publications
(29 citation statements)
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“…The CCI SM has comparable performance to ERA-Interim. The accuracy levels are also similar to that reported by validation studies over other regions [59,61,62]. Additionally, the seasons and land use have little effect on the performance of these products.…”
Section: Discussionsupporting
confidence: 84%
“…The CCI SM has comparable performance to ERA-Interim. The accuracy levels are also similar to that reported by validation studies over other regions [59,61,62]. Additionally, the seasons and land use have little effect on the performance of these products.…”
Section: Discussionsupporting
confidence: 84%
“…Over the past few years, vegetation index and surface temperature have been widely used for downscaling satellite soil moisture data (Fang & Lakshmi, 2014;Im et al, 2016;Merlin et al, 2008Merlin et al, , 2015Peng et al, 2015;Piles et al, 2011;Song et al, 2014;Srivastava et al, 2013). These land surface parameters are available from Moderate Resolution Imaging Spectroradiometer (MODIS) instrument.…”
Section: Modis Land Surface Temperature (Lst) and Normalized Differenmentioning
confidence: 99%
“…In addition to the general investigation of sub-grid heterogeneity for identifying adequate (homogeneous) validation sites and evaluating the representativeness of single soil moisture sensors for large areas covered by a satellite pixel, the estimated σ θ θ function in the final data set can be used for soil moisture disaggregation using proxy information which describes the spatial patterns within each coarse scale satellite pixel. Proxy data can be higher resolution Earth observation data with a proven relationship to soil moisture variability such as surface temperature [101,102], vegetation [103], a combination of both [104], radar backscatter [84], or even soil texture [105]. The proxy data need to be normalized for each individual grid cell.…”
Section: How To Use the Estimated Sub-grid Soil Moisture Variability mentioning
confidence: 99%