Seasonal variability in the optical properties of Baltic aerosols
2011 (English)In: Oceanologia, ISSN 0078-3234, Vol. 53, no 1, 7-34 p.Article in journal (Refereed) Published
A five-year dataset of spectral aerosol optical thickness was used to analyse the seasonal variability of aerosol optical properties (the aerosol optical thickness (AOT) at wavelength lambda = 500 urn, AOT(500) and the Angstrom exponent for the 440-870 urn spectral range, a(440, 870)) over the Baltic Sea and dependence of these optical properties on meteorological factors (wind direction, wind speed and relative humidity). The data from the Gotland station of the global radiometric network AERONET (Aerosol Robotic Network, http://aeronet.gsfc.nasa.gov)were taken to be representative of the Baltic Sea conditions. Meteorological observations from Farosund were also analysed. Analysis of the data from 1999 to 2003 revealed a strong seasonal cycle in AOT. (500) and alpha(440, 870). Two maxima, of monthly mean values of AOT(500) over the Baltic were observed. In April, an increase in the monthly mean aerosol optical thickness over Gotland most probably resulted from agricultural waste straw burning, mainly in northern Europe and Russia as well as in the Baltic states, Ukraine and Belarus. During July and August, the aerosol optical thickness was affected by uncontrolled fires (biomass burning). There was a local minimum of AOT(500) in June. Wind direction, a local meteorological parameter strongly related to air mass advection, is the main meteorological factor influencing the variability of aerosol optical properties in each season. The highest mean values of AOT(500) and alpha(440, 870) occurred with easterly winds in both spring and summer, but with southerly winds in autumn.
Place, publisher, year, edition, pages
2011. Vol. 53, no 1, 7-34 p.
Aerosol optical thickness, Angstrom exponent, Seasonal variability, Baltic Sea
Oceanography, Hydrology, Water Resources
IdentifiersURN: urn:nbn:se:su:diva-68653DOI: 10.5697/oc.53-1.007ISI: 000289316300001OAI: oai:DiVA.org:su-68653DiVA: diva2:473650
authorCount :32012-01-062012-01-042012-01-06Bibliographically approved