SEASONAL MEASUREMENTS OF NONMETHANE HYDROCARBONS AND CARBON-MONOXIDE AT THE MAUNA-LOA-OBSERVATORY DURING THE MAUNA-LOA-OBSERVATORY PHOTOCHEMISTRY EXPERIMENT 2
Jp. Greenberg et al., SEASONAL MEASUREMENTS OF NONMETHANE HYDROCARBONS AND CARBON-MONOXIDE AT THE MAUNA-LOA-OBSERVATORY DURING THE MAUNA-LOA-OBSERVATORY PHOTOCHEMISTRY EXPERIMENT 2, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D9), 1996, pp. 14581-14598
Measurements of carbon monoxide and nonmethane hydrocarbons were made
in situ at the Mauna Loa Observatory from September 1991 through Augus
t 1992. A distinct seasonal cycle in concentrations was observed for C
O and most NMHCs, with higher average concentrations from January thro
ugh April and much lower average concentrations from mid-May through O
ctober. The sources of CO and NMHCs appeared to vary with season and a
ppeared more homogeneous in winter (urban/industrial) and spring (unid
entified). The ocean around Hawaii did not pen appear to be a major so
urce of CO and most NMHCs, but was the major source of ethane and prop
ene. Ethene and propene were always present in free tropospheric air s
ampled, indicating daily exchange between the free troposphere and the
marine boundary layer. Air arriving at MLO during free tropospheric f
low periods had seasonally similar photochemical age (approximately 20
days), with no significant fresh source inputs of NMHCs (except ethen
e and propene) within at least 10 days. The influence of atmospheric d
ilution processes on atmospheric concentrations was weakest in the spr
ing period, when the influence of chemical loss processes was greatest
. Aircraft measurements made during the spring agreed in trends and ab
solute concentrations with ground-based measurement made at MLO. The t
emporal trends in concentrations of NMHCs within altitude ranges were
similar. These trends varied with altitude and characterized a layered
atmosphere with differing chemical composition. Acetone and methyl et
hyl ketone were detected in most samples. N-alkyl aldehydes were also
detected but may be artifacts formed from organic aerosols collected i
n the sampling process.