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Results reported in the first three columns were estimated using one regression run on stacked data for each of the three outcomes.
DTIs and MIs can be estimated using one of two estimators; a kernel density estimator we implemented based on the work of [ 23] and a b-spline estimator based on the work of [ 24], implemented by Boris Hayete and provided by courtesy of the Gardner Lab of the Berkeley University.
Thresholds and slopes were estimated using one out of the three estimation procedures described in the section " Threshold and slope estimation" below.
The VAR for Greece and the respective panel-VARs for the two groups are estimated using one lag.
The carbon fluxes of three contrasting ecosystem in the Sudanian Savanna in West Africa have been estimated using one year of eddy covariance CO2 flux data.
Analysis of an individual 18-h rainfall event revealed that the uncertainty in peak areal rainfall estimated using one rain gauge may range between −100% and 600%.
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Statistical significance was estimated using one-way Analysis Of Variance (ANOVA) in the DeCyder software.
*Distribution skewness was estimated using one-tailed Mann-Whitney's test.
The statistical significance between groups was estimated using one-way analysis of variance and the Fisher's protected least significant difference test.
Statistical significance was estimated using one-way ANOVA (Tukey Kramer multiple comparison test) with the Instat 2.0, Graphpad Software (San Diego, CA, USA).
Differences between groups were estimated using one-way or two-ways analysis of variance (ANOVA), followed by the Bonferroni posttest analysis.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com