Stemflow, throughfall and precipitation data were collected for 30 consecut
ive months in a helm-oak forest dominated by Quercus ilex, Arbutus unedo an
d Phyllirea media. These flux data were obtained from 50 randomly distribut
ed no-roving throughfall collectors and 20 stemflow measuring devices (ten
on Q. ilex and five on each of the other species). The stemflow was highly
influenced by tree size and amount of rainfall, showing a significant corre
lation for each tree. Throughfall results showed a high spatial variability
for each storm, with a significant independence of collectors. At forest s
cale, stemflow and throughfall represented 12.1 and 75 % of precipitation,
respectively, and interception was estimated as 12.9 % of precipitation. Pa
rtitioning of rainfall between stemflow and throughfall created a high spat
ial heterogeneity of water distribution under the canopy. Stemflow increase
d more than 30 times the mean amount of water received per unit soil area a
round tree trunks. Finally, the effect of a change in the amount of precipi
tation according to a regional scenario was analyzed. It was shown that the
increase in high rainfall events rather than small events increased the st
emflow percentage. (C) Inra/Elsevier, Paris.