The mixing ratio of formaldehyde (HCHO) has been determined for air samples collected at a moderately polluted continental site (Jtilich, Federal Republic of Germany) and for samples collected at coastal sites in Ireland and New Zealand. In addition the HCHO mixing ratio has been determined for air samples collected in the North and South Atlantic during a cruise of the F/S Meteor from Hamburg at 55øN to Montevideo at 35øS in October and November 1980. The HCHO mixing ratio in clean tropical marine air is of the order of 0.2 parts per billion by volume, about 50% lower than predicted by current photochemical models that include CH,• oxidation as the only source for HCHO. In the mid-Atlantic, diurnal variations of the HCHO mixing ratio showing weak maxima during the early afternoon were occasionally observed. These variations may be attributed to the diurnal behavior of the photochemical and physical processes which determine the mixing ratio of HCHO during stable weather conditions. The results are discussed with regard to the currently accepted theory of the photochemistry of HCHO in the clean troposphere. It appears that the yield of HCHO formation through hydrocarbon photooxidation in the background marine troposphere is less than assumed from model considerations, most probably because of the lack of sufficiently high NO concentrations.
HCHOin clean air are summarized in Table 1. The results display a considerable amount of scatter and are difficult to interpret in terms of current photochemical models. In addition, indirect methods have been used to estimate the HCHO mixing ratio in clean air, and these also show large variations. Junge [1963] first used HCHO measurements made in rain and dew by Dhar and Ram [1933] to deduce a tropospheric HCHO mixing ratio of 0.75 ppbv. A similar approach was used by McConnel et al. [1971] to estimate a tropospheric HCHO mixing ratio of 1.3 ppbv for summer conditions, and more recently, Warneck et al. [1978] have predicted mixing ratios ranging from 0.12 ppbv to 0.39 ppbv from rain data gathered at the west coast of Ireland by Klippel [1978]. Various photochemical models have also been used to predict HCHO distributions in the clean troposphere, but the computed values are difficult to compare because of the different assumptions used to generate the models. Graedel [1979] used a kinetic photochemical model to predict HCHO mixing ratios ranging from 0.06 to 0.2 ppbv at the surface in a marine atmosphere. Calvert [1980] published results from a photochemical model developed by D. Wuebbles predicting HCHO mixing ratios ranging from 0.45 ppbv at the ground to 0.04 ppbv at 10 km in a clean troposphere at 30øN during the solar equinox at noon. More recently, Logan et al. [[981] used a tropospheric photochemical model to compute HCHO profiles with mixing ratios at the surface ranging from 0.35 ppbv in equatorial regions to 0.10 ppbv at the poles. PRODUCTION AND REMOVAL OF HCHO IN THE CLEAN TROPOSPHERE Of the hydrocarbons found in the clean troposphere, methane has the highest con...