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. Author manuscript; available in PMC: 2019 Feb 1.
Published in final edited form as: J Hydrometeorol. 2018 Feb 12;19(No 2):375–392. doi: 10.1175/JHM-D-17-0152.1

Figure 5.

Figure 5

Propagation of errors estimated from their rank correlations among precipitation (P), height of the lifting condensation level (LCL), evaporative fraction (EF), sensible and latent heat flux (SH & LH), surface albedo (α) and net radiation (RNet) across FLUXNET2015 stations. Ratios show the number of models out of 11 (correlations involving α) or 12 (other variables) with p-values below 0.10; p-value shown is based on the average of correlations across all models. Widths of arrows follow significance of correlations and no arrows are drawn where p-values are large. The wide double arrows between EF and heat fluxes denote p-values < 10−12.