Dr. Miller et al., SOME ATMOSPHERIC-TURBULENCE AND STABILITY EFFECTS ON AERIAL SPRAY PENETRATION INTO HARDWOOD FOREST CANOPIES, Forest science, 42(1), 1996, pp. 93-101
Vertical profiles of wind, turbulence, and stability were measured in
and above a partially foliated 16 m tall, oak forest during a series o
f single-swath, aerial spray trials. The distribution of cross-swath s
pray deposits was sampled after each application at the top of the can
opy and below the canopy. Spray penetration to the canopy top and thro
ugh the canopy was highly dependent on the relative intensity of mecha
nically generated turbulence (due to wind across a rough surface) to t
hat of thermally generated turbulence (due to warm air rising) in the
unstable roughness sublayer above the canopy. In conditions with mecha
nical turbulence dominant, termed mixed convection conditions (u > 1
m s(-1) and -0.01 > Ri > -1), the amount and consistency of material r
eaching the canopy top was higher than during periods with thermal tur
bulence dominant, termed free convection conditions (u < 1 m s(-1) an
d Ri < -1). A greater proportion of the material penetrated through th
e canopy in the free convection conditions. The relationship of the st
ructure of the Reynolds stress in the roughness sublayer to the spray
behavior is discussed.