Research Article
Identification of the Aerosol Types over Athens, Greece: The Influence of Air-Mass Transport
Table 4
As in Table
1, but for the DD aerosols.
| | Trajectory altitude | | FM | Year | Winter | Spring | Summer | Autumn |
| | 500 m | A | | | 88 (26%) | 11% | 22% | 33% | 34% | | B | | | 26 (8%) | 4% | 8% | 58% | 31% | | C | | | 120 (36%) | 1% | 8% | 61% | 30% | | D | | | 69 (20%) | 1% | 7% | 70% | 22% | | E | | | 34 (10%) | 3% | 15% | 44% | 38% |
| | 1000 m | A | | | 101 (30%) | 9% | 19% | 38% | 35% | | B | | | 46 (14%) | 2% | 11% | 52% | 35% | | C | | | 107 (32%) | 2% | 7% | 59% | 32% | | D | | | 56 (16%) | 0% | 5% | 80% | 14% | | E | | | 27 (8%) | 7% | 22% | 37% | 33% |
| | 4000 m | A | | | 118 (35%) | 8% | 25% | 38% | 29% | | B | | | 141 (42%) | 3% | 6% | 56% | 35% | | C | | | 54 (17%) | 0% | 4% | 70% | 26% | | D | | | 12 (3%) | 0% | 8% | 58% | 33% | | E | | | 12 (3%) | 0% | 8% | 92% | 0% |
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