The two main resistances in the exchange of gases between plants and the at
mosphere are stomatal and boundary layer resistances. We modeled boundary l
ayer dynamics over glabrous and pubescent leaves (assuming non-exchanging t
richomes) with leaf lengths varying from 0.01 to 0.2m, and windspeeds of 0.
1-5.0ms(-1). Results from theoretical and semi-empirical formulae were comp
ared. As expected, boundary layer thickness decreased with decreasing leaf
length and increasing windspeed. The presence of trichomes increased leaf s
urface roughness, resulting in lowered Reynolds numbers at which the bounda
ry layer became turbulent. This effect is especially important at low winds
peeds and over small leaves, where the Reynolds number over glabrous surfac
es would be low. We derived a new simple dimensionless number, the trip fac
tor, to distinguish field conditions that would lead to a turbulent boundar
y layer based on the influence of trichomes. Because modeled rates Of CO2 a
nd H2Onu exchange over turbulent boundary layers are one or more orders of
magnitude faster than over laminar boundary layers, a turbulent boundary la
yer may lead to increased carbon uptake by plants. The biological trade-off
is potentially increased transpirational water loss. However, in understor
y habitats characterized by low windspeeds, even a few trichomes may increa
se turbulence in the boundary layer, thus facilitating photosynthetic gas e
xchange. Preliminary field data show that critical trip factors are exceede
d for several plant species, both in understory and open habitats. (C) 2001
Academic Press.