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Figure 6 allows us to address some of the differences in the soiling rate reported in Table 2.
It is remarkable that these changes in winds did not lead to significant changes in the soiling rate.
However, it should be noted that this estimate does not fully capture the influence of seasonal changes in the soiling rate.
Indeed, due to the seasonal changes in the soiling rate, the "waiting period before next cleaning" will also show seasonal changes.
The presence of β-LGB in the soiling suspension leads to protein adsorption, but a significant amount of contaminants remains at the surface.
This means that, although lowered wind speeds likely aid to lower the dry deposition velocity in autumn and winter, significant increments in the PM mass concentration negate such changes, thereby contributing to increases in the soiling deposition rate.
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