Abstract
An accumulation mode (AM) was present in all particle data and was characterized by a lognormal size distribution with parameters N cm-3 (total number concentration), rg μm (geometric mean radius) and σg (geometric standard deviation). For aerosol associated with the "cleanest' Northeast Atlantic maritime and Arctic air masses, the AM parameters were found to be 16 cm-3 ≤N≤48 cm-3, 1.32≤σg≤1.46, and 0.08 μm < rg < 0.09 μm, leading to AM masses of between 0.20 μg m-3 and 0.38 μg m-3. Clean background levels of soot carbon mass for maritime and Arctic air were estimated to be around 20 ng m-3 and were associated with particle size radii r ≤ 0.15 μm. Soot carbon mass showed an excellent correlation with AM number concentration (cc=0.93). By comparison, radon exhibited a significantly poorer correlation (cc=0.60) for this region. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1123-1135 |
| Number of pages | 13 |
| Journal | Journal of Geophysical Research |
| Volume | 98 |
| Issue number | D1 |
| DOIs | |
| Publication status | Published - 1993 |