WARNING : This is a preprint of an article accepted for publication in QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY ref: Q. J. R. Meteorol. Soc. 134: 497–508 (2008) see the website for final version http://www.interscience.wiley.com/International audienceThis article presents different formulae to estimate correlation length-scales, and an evaluation of their qualities for practical diagnostic applications. In particular, two new and simple formulae are introduced, which only require the computation of correlation with a single point for a given direction. It is then shown in a 1D heterogeneous context that all formulations lead to similar realistic length-scale values, and that they represent geographical variations rather well. T...
The spatial scale of soil moisture measurements is often inconsistent with the scale at which soil m...
The spatio-temporal representation of background error covariances is one of the major problems in d...
Data assimilation (DA) combines incomplete background values obtained via chemical transport model p...
WARNING : This is a preprint of an article accepted for publication in QUARTERLY JOURNAL OF THE ROYA...
Background error correlation length-scale estimates and their sampling statistics O. Pannekoucke∗, L...
Abstract. The concept of a sampling scale triplet of spacing, extent and support is used to define t...
Mainstream numerical weather prediction (NWP) centers usually estimate the standard deviations of ba...
International audienceBackground-error covariances can be estimated from an ensemble of forecast dif...
The four-dimensional variational data assimilation (4D-Var) method has been widely employed as an op...
The spatial structure of bias errors in numerical model output is valuable to both model developers ...
Optimally modeling background-error horizontal correlations is crucial in ocean data assimilation. T...
The majority of documented climatic data set biases can be divided into two categories: physical bia...
Scale coarseness is a pervasive yet ignored methodological artifact that attenuates observed correla...
• Predictions can appear overdispersive due to hindcast length sampling error • Longer hindcasts are...
Spatial statistical analyses are often used to study the link between environmental factors and the ...
The spatial scale of soil moisture measurements is often inconsistent with the scale at which soil m...
The spatio-temporal representation of background error covariances is one of the major problems in d...
Data assimilation (DA) combines incomplete background values obtained via chemical transport model p...
WARNING : This is a preprint of an article accepted for publication in QUARTERLY JOURNAL OF THE ROYA...
Background error correlation length-scale estimates and their sampling statistics O. Pannekoucke∗, L...
Abstract. The concept of a sampling scale triplet of spacing, extent and support is used to define t...
Mainstream numerical weather prediction (NWP) centers usually estimate the standard deviations of ba...
International audienceBackground-error covariances can be estimated from an ensemble of forecast dif...
The four-dimensional variational data assimilation (4D-Var) method has been widely employed as an op...
The spatial structure of bias errors in numerical model output is valuable to both model developers ...
Optimally modeling background-error horizontal correlations is crucial in ocean data assimilation. T...
The majority of documented climatic data set biases can be divided into two categories: physical bia...
Scale coarseness is a pervasive yet ignored methodological artifact that attenuates observed correla...
• Predictions can appear overdispersive due to hindcast length sampling error • Longer hindcasts are...
Spatial statistical analyses are often used to study the link between environmental factors and the ...
The spatial scale of soil moisture measurements is often inconsistent with the scale at which soil m...
The spatio-temporal representation of background error covariances is one of the major problems in d...
Data assimilation (DA) combines incomplete background values obtained via chemical transport model p...