“…A recent commentary has suggested that a key gap in the ability to generalize findings from paired watershed studies is the lack of understanding of subsurface catchment storage and how factors such as hydroclimate, topography, geology, and soil type conspire with catchment storage to define the watershed response to forest treatment (McDonnell, 2017). We know that in many cases, the establishment of forest plantations on former agricultural land reduces flow rates, especially during the dry season (Iroumé & Palacios, 2013, Moore & Wondzell, 2005, reducing not only water yield but also water storage availability (Andréassian, Perrin, & Michel, 2004;Silveira, Gamazo, Alonso, & Martinez, 2016). A decrease in the annual water yield, summer runoff, and peak flows is associated with higher transpiration rates caused by an increased proportion of the catchment being covered by forest and with the establishment, growth, species composition, or age of the forest (Andréassian, 2004;Best et al, 2003;Bosch & Hewlett, 1982;Brown, Zhang, McMahon, Western, & Vertessy, 2005).…”