Xl. Zhou et al., TROPOSPHERIC FORMALDEHYDE CONCENTRATION AT THE MAUNA-LOA-OBSERVATORY DURING THE MAUNA-LOA-OBSERVATORY PHOTOCHEMISTRY EXPERIMENT 2, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D9), 1996, pp. 14711-14719
The concentration of formaldehyde at Mauna Loa Observatory, Hawaii, wa
s determined during four Mauna Loa Observatory Photochemistry Experime
nt 2 (MLOPEX 2) measurement intensives between September 1991 and Augu
st 1992. The observed diurnal variations, 200-900 parts per trillion b
y volume (pptv) during daytime and 60-200 pptv during nighttime, resul
ted mainly from the local air circulation pattern whereby island modif
ied marine boundary layer air prevailed during the day and free tropos
pheric air dominated during the night. A seasonal variation was also o
bserved; the median/mean values of all data points are: 149/196, 129/1
49, 143/178, and 181/211 pptv for autumn, winter, spring, and summer i
ntensives, respectively. During nighttime downslope flow periods which
brought in free tropospheric air to the measurement site, the formald
ehyde concentrations (median/mean) were 122/123, 110/112, 120/125, and
140/137 pptv for autumn, winter, spring, and summer, respectively. Th
is seasonal dependence may be attributable to changes in solar insolat
ion and NO concentrations. A simple box model calculation constrained
by the experimentally determined concentrations of CH3OOH yielded a fo
rmaldehyde concentration (without/with heterogeneous removal) for free
tropospheric air, at 7 degrees C, of 155/140, 125/115, 210/195, and 2
20/205 pptv for autumn, winter, spring and summer, respectively. The c
alculated values are in good agreement with the measured concentration
s for winter (within 27/15%, without/with heterogeneous removal) and f
all (within 14/5%), but are significantly higher for spring (75/63%) a
nd summer (57/46%).