Abstract
Maximum DMS concentrations between 100 and 240 ppm were observed when the measurement site (480 m above sea level) was embedded in clouds and air from the marine boundary layer was flowing upslope to the site. DMS levels measured in continental air and/or above the mixed layer were typically less than 20 pptv. The sulfur gases DMSO, H2SO4, and MSA(g) were measured in real time on a continuous basis (once every 60-150 s) using selected ion chemical ionization mass spectrometry. Corresponding concentrations ranged between <0.5-3.2 pptv, 0.001-1.19 pptv, and 0.002-0.19 pptv, respectively. All three sulfur gases showed significant diel variations mostly in phase with each other. Their corresponding lifetimes in the marine atmosphere are estimated to be of the order of a few hours. The results indirectly support a relationship between DMS and CCN concentrations. However, other observations also suggest that at higher supersaturations (0.9%), compounds less soluble than sulfate may become important in marine CCN formation. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 12,701-12,711 |
| Journal | Journal of Geophysical Research |
| Volume | 98 |
| Issue number | D7 |
| DOIs | |
| Publication status | Published - 1993 |
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