2016
DOI: 10.1016/j.jag.2015.09.002
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Recent advances in (soil moisture) triple collocation analysis

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Cited by 266 publications
(312 citation statements)
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“…Indeed, ρ 2 represents the unbiased signal to noise ratio, scaled between 0 and 1, which provides a measure of the relative similarity between two signals, independently from their phase differences. This was also underlined by Gruber et al (2016), who showed that ρ 2 is the complement of the f RMSE = σ 2 ε /σ 2 introduced by Draper et al (2013) (ρ 2 = 1−f RMSE), which was used previously to remove the dependency of the error variance pattern on the spatial climatology of the chosen ref-erence. Gruber et al (2016) also pointed out that the absolute error variance provides only limited information about the true data set quality because a certain amount of noise can be either acceptable or unacceptable depending on the strength of the underlying signal (i.e.…”
Section: Performance Scoresmentioning
confidence: 81%
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“…Indeed, ρ 2 represents the unbiased signal to noise ratio, scaled between 0 and 1, which provides a measure of the relative similarity between two signals, independently from their phase differences. This was also underlined by Gruber et al (2016), who showed that ρ 2 is the complement of the f RMSE = σ 2 ε /σ 2 introduced by Draper et al (2013) (ρ 2 = 1−f RMSE), which was used previously to remove the dependency of the error variance pattern on the spatial climatology of the chosen ref-erence. Gruber et al (2016) also pointed out that the absolute error variance provides only limited information about the true data set quality because a certain amount of noise can be either acceptable or unacceptable depending on the strength of the underlying signal (i.e.…”
Section: Performance Scoresmentioning
confidence: 81%
“…When dealing with error variances, the products have to be rescaled to a common reference data space. However, such a rescaling imposes spatial patterns within the derived error metric which reflects the climatology of the chosen reference (Gruber et al, 2016). To this end, McColl et al (2014) noted that correlation coefficients can provide important new information about the performance of the measurement systems with respect to the absolute error variances obtained via Eq.…”
Section: Performance Scoresmentioning
confidence: 99%
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“…TC is a method to estimate the RMSE (and, if desired, correlation coefficients) of three spatially and temporally collocated measurements by assuming a linear error model between the measurements (McColl et al, 2014;Stoffelen, 1998). This methodology has been widely used in error estimation of land and ocean parameters, such as wind speed, sea surface temperature, soil moisture, evaporation, precipitation, f APAR, and in the rescaling of measurement systems to reference system for data assimilation purposes (Alemohammad et al, 2015;D'Odorico et al, 2014;Gruber et al, 2016;Hain et al, 2011;Lei et al, 2015;Miralles et al, 2010Miralles et al, , 2011bParinussa et al, 2011), as well as in validating categorical variables such as the soil freeze-thaw state (McColl et al, 2016). The relationship between each measurement and the true value is assumed to follow a linear model:…”
Section: Target Dataset: a Bayesian Prior Using Triple Collocationmentioning
confidence: 99%
“…For surface soil wetness, verification McColl et al (2014) have developed the Extended Triple Collocation (ETC) method to estimate the temporal correlation between a model or observation system and the unknown truth. The ETC method makes the same assumptions as the more widely known Triple Collocation (TC; Scipal et al 2008;Vogelzang and Stoffelen 2012;Zwieback et al 2012;Dorigo et al 2010;Yilmaz and Crow 2014;Gruber et al 2016;Draper et al 2013) method. ETC and TC require three mutually independent time-series estimates of the same quantity.…”
Section: Ozfluxmentioning
confidence: 99%