We used three methods to measure boundary layer conductance to heat transfe
r (g(bH)) and water vapor transfer (g(bV)) in foliated branches of Abies am
abilis Dougl, ex J. Forbes, a subalpine forest tree that produces clumped s
hoot morphology on sun-formed branches. Boundary layer conductances estimat
ed in the field from energy balance measurements increased linearly from ap
proximately 10 mm s(-1) at low wind speeds (< 0.1 m s(-1)) to over 150 mm s
(-1) at wind speeds of 2.0 m s(-1). Boundary layer conductances measured on
shoot models in a wind tunnel were consistently higher than field measurem
ents. The difference between wind tunnel values and field measurements was
attributable to variation in path length between the two experimental envir
onments. Boundary layer conductance estimated by subtracting stomatal resis
tance (r(sV)) measured with a porometer from the total branch vapor phase r
esistance were unusually small. Sensitivity analysis demonstrated that this
method is not suitable for coniferous foliage or when stomatal conductance
(g(sV)) is small compared with g(bV). Analysis of the relative magnitudes
of g(sV) and g(bV) revealed that, under most conditions, A. amabilis branch
es are well coupled (i.e., g(sV) is the dominant controller of transpiratio
n). The boundary layer conductance to heat transfer is small enough that le
af temperature can become substantially higher than air temperature when ra
diation is high and wind speed is low. Over a two-month period, the maximum
difference between leaf and air temperatures exceeded 6 degrees C. Leaf te
mperature exceeded air temperature by more than 2 degrees C on 10% of the d
aylight hours during this period. Consideration of both the photosynthetic
temperature response of A. amabilis foliage as well as the summer air tempe
rature conditions in its habitat suggests that these elevated leaf temperat
ures do not have a significant impact on carbon gain during the growing sea
son.