CHEMICAL AND PHYSICAL-PROPERTIES OF PLUMES OF ANTHROPOGENIC POLLUTANTS TRANSPORTED OVER THE NORTH-ATLANTIC DURING THE NORTH-ATLANTIC REGIONAL EXPERIMENT
Ph. Daum et al., CHEMICAL AND PHYSICAL-PROPERTIES OF PLUMES OF ANTHROPOGENIC POLLUTANTS TRANSPORTED OVER THE NORTH-ATLANTIC DURING THE NORTH-ATLANTIC REGIONAL EXPERIMENT, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D22), 1996, pp. 29029-29042
Plumes of photochemical pollutants transported from the industrialized
regions of the northeast United States and Canada were sampled over t
he North Atlantic Ocean at distances up to 1000 km from the coast. The
plumes were found in well defined layers up to 1 km thick and were us
ually isolated from the surface by a low altitude inversion. Plume com
position was consistent with the occurrence of extensive photochemical
processing during transit from source regions as indicated by high O-
3 concentrations (O-3 maximum similar to 150 parts per billion by volu
me (ppbv)), generally high fractional conversion (>85%) of NOx to its
oxidation products, and high peroxide concentrations (median 3.6 ppbv;
maximum 11 ppbv). These observations are in accord with processing ti
mes estimated from back trajectory analysis. CO and O-3 Concentrations
were well correlated (r(2) = 0.64) with a slope (0.26) similar to pre
vious measurements in photochemically aged air. Good correlations were
also observed between CO and accumulation mode particle number densit
ies (r(2) = 0.64), and CO and NOy (r(2) = 0.67). O-3 was found to depe
nd nonlinearly on the NOx oxidation product concentration. At low valu
es of (NOy-NOx), the slope (14) was within the range of values measure
d previously in photochemically aged air masses, at higher concentrati
ons the slope was much lower (4.6). The low slope at high concentratio
ns is attributed to minimization of losses of NOx oxidation products i
n spatially well-defined plumes during transport. A strong linear corr
elation (r(2) = 0.73) was found between O-3, and the concentration of
radical sink species as represented by the quantity ((NOy-NOx) + 2H(2)
O(2)).