Similar to the previous measurement days the values of the AOD and the
Ängström exponent are an order of magnitude lower in Birkenes than in Lubiatowo.
The fine (0.033) to coarse mode ratio (0.007) for that day shows the presence of
small particles in the air, which is again in total opposition to the situation at the
CRS study station.
Fig. 9 The AOD (500 nm)
and Ängström exponent
(440–870 nm) on 21 July
2012 at the CRS station in
Lubiatowo
Fig. 10 The level 2.0 AOD (a) and the Ängström exponent (440–870 nm) (b) at the AERONET
Birkenes station on 20 July 2012
Impact of Breaking Waves on Sea Salt Production …
19
Ängström exponent are an order of magnitude lower in Birkenes than in Lubiatowo.
The fine (0.033) to coarse mode ratio (0.007) for that day shows the presence of
small particles in the air, which is again in total opposition to the situation at the
CRS study station.
Fig. 9 The AOD (500 nm)
and Ängström exponent
(440–870 nm) on 21 July
2012 at the CRS station in
Lubiatowo
Fig. 10 The level 2.0 AOD (a) and the Ängström exponent (440–870 nm) (b) at the AERONET
Birkenes station on 20 July 2012
Impact of Breaking Waves on Sea Salt Production …
19