Abstract
arising from S. Jasechko et al. Nature 496, 347–350 (2013)
How best to assess the respective importance of plant transpiration over evaporation from open waters, soils and short-term storage such as tree canopies and understories (interception) has long been debated. On the basis of data from lake catchments, Jasechko et al.1 conclude that transpiration accounts for 80–90% of total land evaporation globally (Fig. 1a). However, another choice of input data, together with more conservative accounting of the related uncertainties, reduces and widens the transpiration ratio estimation to 35–80%. Hence, climate models do not necessarily conflict with observations, but more measurements on the catchment scale are needed to reduce the uncertainty range. There is a Reply to this Brief Communications Arising by Jasechko, S. et al. Nature 506, http://dx.doi.org/10.1038/nature12926 (2014).
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Coenders-Gerrits, A., van der Ent, R., Bogaard, T. et al. Uncertainties in transpiration estimates. Nature 506, E1–E2 (2014). https://doi.org/10.1038/nature12925
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