Research Article
Identification of the Aerosol Types over Athens, Greece: The Influence of Air-Mass Transport
Table 3
As in Table
1, but for the CM aerosols.
| Trajectory altitude | | FM | Year | Winter | Spring | Summer | Autumn |
| 500 m | A | | | 27 (15%) | 48% | 4% | 0% | 48% | B | | | 47 (26%) | 55% | 11% | 0% | 34% | C | | | 77 (43%) | 52% | 10% | 13% | 25% | D | | | 17 (9%) | 35% | 12% | 18% | 35% | E | | | 14 (7%) | 29% | 64% | 7% | 0% |
| 1000 m | A | | | 30 (17%) | 53% | 7% | 0% | 40% | B | | | 50 (27%) | 54% | 6% | 2% | 38% | C | | | 81 (45%) | 47% | 14% | 14% | 26% | D | | | 13 (7%) | 46% | 0% | 8% | 46% | E | | | 8 (4%) | 25% | 0% | 13% | 63% |
| 4000 m | A | | | 22 (12%) | 59% | 9% | 0% | 32% | B | | | 127 (70%) | 50% | 8% | 5% | 37% | C | | | 26 (14%) | 38% | 15% | 23% | 23% | D | | | 5 (3%) | 40% | 0% | 40% | 20% | E | | | 2 (1%) | 0% | 0% | 0% | 100% |
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