Figure 2.

Annual 2018 anomalies of sensible heat flux (H) (a), latent heat flux (λET) (b), and evaporative fraction (λET (H + λET)⁻¹) (c) as a function of precipitation P and grass reference ET₀ deficits. Diagonal isolines indicate P-ET₀ anomalies of 0, ±100 and ±300 mm (figure 1).