id	author	title	date	pages	extension	mime	words	sentences	flesch	summary	cache	txt
work_xqyxprcq7va77budlv5pymo4cy	Chris Soulsby	Influence of forest and shrub canopies on precipitation partitioning and isotopic signatures	2017.0	44	.pdf	application/pdf	14682	3499	82	In the forest stands, stemflow (StF) was a relatively small canopy flow path isotopic composition of water routing through vegetation canopies can have significant effects on the found a high correlation between canopy structure and evaporation during low intensity rainfall events. To understand intra-site differences within the forest plots, Figure 5 shows the mean weighted amount The isotopic composition in StF in forest plots was also variable over time, mostly activation of selective canopy flow paths delivering water at specific stages of events where the intraevent isotope changes in rainfall may have occurred. between I values for the two forest sites and both canopy coverage and distance to the closest tree. StF isotopic compositions were more markedly different to those compared to TF in the two forest sites. Given the limited changes in the isotopic composition of NP below the forest and heather canopies, it is 	./cache/work_xqyxprcq7va77budlv5pymo4cy.pdf	./txt/work_xqyxprcq7va77budlv5pymo4cy.txt