A. Guenther et al., ESTIMATES OF REGIONAL NATURAL VOLATILE ORGANIC-COMPOUND FLUXES FROM ENCLOSURE AND AMBIENT MEASUREMENTS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D1), 1996, pp. 1345-1359
Natural volatile organic compound (VOC) emissions were investigated at
two forested sites in the southeastern United States. A variety of VO
C compounds including methanol, 2-methyl-3-buten-2-ol, 6-methyl-5-hept
en-2-one, isoprene and 15 monoterpenes were emitted from vegetation at
these sites. Diurnal variations in VOC emissions were observed and re
lated to light and temperature. Variations in isoprene emission from i
ndividual branches are well correlated with light intensity and leaf t
emperature while variations in monoterpene emissions can be explained
by variations in leaf temperature alone. Isoprene emission rates for i
ndividual leaves tend to be about 75% higher than branch average emiss
ion rates due to shading on the lower leaves of a branch. Average dayt
ime mixing ratios of 13.8 and 6.6 ppbv C isoprene and 5.0 and 4.5 ppbv
C monoterpenes were observed at heights between 40 m and 1 km above g
round level the two sites. Isoprene and monoterpenes account for 30% t
o 40% of the total carbon in the ambient non-methane VOC quantified in
the mixed layer at these sites and over 90% of the VOC reactivity wit
h OH. Ambient mixing ratios were used to estimate isoprene and monoter
pene fluxes by applying box model and mixed-layer gradient techniques,
Although the two techniques estimate fluxes averaged over different s
patial scales, the average fluxes calculated by the two techniques agr
ee within a factor of two. The ambient mixing ratios were used to eval
uate a biogenic VOC emission model that uses field measurements of pla
nt species composition, remotely sensed vegetation distributions, leaf
level emission potentials determined from vegetation enclosures, and
light and temperature dependent emission activity factors. Emissions e
stimated for a temperature of 30 degrees C and above canopy photosynth
etically active radiation flux of 1000 mu mol m(-2) s(-1) are around 4
mg C m(-2) h(-1) of isoprene and 0.7 mg C m(-2) h(-1) of monoterpenes
at the ROSE site in western Alabama and 3 mg C m(-2) h(-1) of isopren
e and 0.5 mg C m(-2) h(-1) of monoterpenes at the SOS-M site in easter
n Georgia. Isoprene and monoterpene emissions based on land characteri
stics data and emission enclosure measurements are within a factor of
two of estimates based on ambient measurements in most cases. This rep
resents reasonable agreement due to the large uncertainties associated
with these models and because the observed differences are at least p
artially due to differences in the size and location of the source reg
ion (''flux footprint'') associated with each flux estimate.