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Table 2 Statistical relationship between the monthly albedo, VWC and EVI for the ten sites in growing season

From: Changes in albedo and its radiative forcing of grasslands in East Asia drylands

 

lm

Poly

lme

Albedo ~ EVI

r = − 0.462; R2 = 0.213; p < 0.01

(AIC = − 270.9)

R2 = 0.251; p < 0.01*

(AIC = − 279.8)

R2 = 0.542; p < 0.01

(AIC = − 375.0)

EVI ~ VWC

r = 0.303; R2 = 0.09; p < 0.01

(AIC = − 137.2)

R2 = 0.121; p < 0.01*

(AIC = − 143.1)

R2 = 0.755; p < 0.01

(AIC = − 454.2)

Albedo ~ VWC

r = − 0.472; R2 = 0.223; p < 0.01

(AIC = − 275.6)

R2 = 0.259; p < 0.01*

(AIC = − 282.2)

R2 = 0.567; p < 0.01

(AIC = − 384.3)

Albedo ~ [EVI + VWC]

R2 = 0.255; p < 0.01

(AIC = − 249.4)

R2 = 0.322; p < 0.01*

(AIC = − 262.9)

R2 = 0.602; p < 0.01

AIC = − 332.0)

  1. The statistics in this study are based on three models: a linear model (lm), a cubic polynomial model (poly), and a linear mixed effects model (lme), with site as a random effect driver to consider site-to-site variability. * Indicates a significant difference between the linear model and polynomial model