Summary Purportedly

large Douglas-fir trees in the American Pacific Northwest use water stored in bole tissues to ameliorate the effects of seasonal summer drought, the water content of bole tissues being drawn down over the summer months and replenished during the winter. Continuous moni-toring of bole relative water content (RWC) in two 110– 120-year-old Douglas-fir trees with ThetaProbe impedance de-vices provided an integrated measure of phloem–sapwood wa-ter content over 4 years. Seasonal changes in RWC closely tracked cambial activity and wood formation, but lagged changes in soil water content by 2–3 months. The RWC in the combined phloem and sapwood markedly increased during earlywood production in the late spring and early summer to maximum values of 64–77 % as plant available soil water (ASW) decreased by ~60%. With transition and latewood for-mation, RWC decreased to minimum values of 59–72%, even as ASW increased in the fall. The difference between mini-mum RWC in the fall and maximum RWC in midsummer was only ~5%. Seasonal changes in bole RWC corresponded to cambial phenology, although decreasing AWS appeared to trigger the shift from earlywood to latewood formation