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Reviews and syntheses: Turning the challenges of partitioning ecosystem evaporation and transpiration into opportunities

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Figure

Figure 1. The mean monthly latent heat flux (λE) – the energy used for evapotranspiration – from eddy covariance measurements from fourresearch sites (“MEASURED”) and 13 ecosystem models from the North American Carbon Program Site-Level Interim Synthesis (S
Table 1. A summary of recent approaches for estimating transpiration (T ) and/or for partitioning evapotranspiration (ET) into evaporation (E)and T at the ecosystem scale
Figure 2. The relationship between above-canopy vapor pressuredeficit (D) and evapotranspiration (ET in millimeters per half hour,hh) visualized using kernel density estimation (Botev et al., 2010)for more than 1.5 million half-hourly eddy covariance observ
Figure 3. The Priestley–Taylor Jet Propulsion Lab (PT-JPL) esti-mate of transpiration (T ) in energy flux units compared againstT estimated using eddy covariance measurements and models ofsoil evaporation in a loblolly pine forest for 2001–2005 from Stoyet
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