Impact of wild forest fires in Eastern Europe on aerosol composition and particle optical properties

Summary In this paper the authors discuss the changes of aerosol optical depth (AOD) in the region of eastern Europe and the Baltic Sea due to wild fire episodes which occurred in the area of Belarus and Ukraine in 2002. The authors discuss how the biomass burning aerosols were advected over the Baltic area and changed the composition of aerosol ensemble for a period of several summer weeks. The air pressure situation and slow wind speeds also facilitated the development of such conditions. As a consequence very high AOD levels were recorded, by an order of 3–4 higher versus normal conditions and they significantly increased the annual averages. On particular days of August 2002 the AOD values reached a level of over 0.7. On these days fine particles fully dominated the entire ensemble of aerosol particles. They were either sulfates or smoke particles. Such situation was unique over a period of many years and it had its serious consequences for the region and especially for the Baltic Sea.

[1]  T. Eck,et al.  Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols , 1999 .

[2]  V. Ramaswamy,et al.  Spatial scales of climate response to inhomogeneous radiative forcing , 2010 .

[3]  T. Zieliński,et al.  Aerosol extinction and aerosol optical thickness in the atmosphere over the Baltic Sea determined with lidar , 2002 .

[4]  P. Levelt,et al.  Aerosols and surface UV products from Ozone Monitoring Instrument observations: An overview , 2007 .

[5]  P. Land,et al.  Aerosol optical depth over the Baltic Sea derived from AERONET and SeaWiFS measurements , 2005 .

[6]  Jesper Heile Christensen,et al.  The Danish Eulerian Hemispheric Model , 1996 .

[7]  L. Hutley,et al.  Fire impacts on surface heat, moisture and carbon fluxes from a tropical savanna in northern Australia , 2003 .

[8]  V. Ulevicius,et al.  Observations of the aerosol particle number concentration in the marine boundary layer over the south-eastern Baltic Sea , 2013 .

[9]  C. Laymon A. study , 2018, Predication and Ontology.

[10]  J. Penner,et al.  A global three‐dimensional model study of carbonaceous aerosols , 1996 .

[11]  Claudene Sproles Intergovernmental Panel on Climate Change (IPCC). Visited December 18, 2007. IPCC Secretariat, C/O World Meteorological Organization, 7bis Avenue de la Paix, CP 2300, CH - 1211 Geneva 2, Switzerland. http: //www.ipcc.ch/ , 2009, Gov. Inf. Q..

[12]  B. Poulter,et al.  Fire evolution in the radioactive forests of Ukraine and Belarus: future risks for the population and the environment , 2015 .

[13]  B. DeAngelo,et al.  Bounding the role of black carbon in the climate system: A scientific assessment , 2013 .

[14]  A. Pietruczuk,et al.  Impact of urban pollution emitted in Warsaw on aerosol properties , 2013 .

[15]  J. Randerson,et al.  Global impact of smoke aerosols from landscape fires on climate and the Hadley circulation , 2013 .

[16]  Yinon Rudich,et al.  Atmospheric HULIS : how humic-like are they ? A comprehensive and critical review , 2005 .

[17]  R. Draxler HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) Model access via NOAA ARL READY Website , 2010 .

[18]  V. Ramaswamy,et al.  Global sensitivity studies of the direct radiative forcing due to anthropogenic sulfate and black carbon aerosols , 1998 .

[19]  M. Legrand,et al.  Chemical composition of atmospheric aerosols during the 2003 summer intense forest fire period , 2008 .

[20]  Thomas W. Kirchstetter,et al.  Evidence that the spectral dependence of light absorption by aerosols is affected by organic carbon , 2004 .

[21]  B. Holben,et al.  Single-Scattering Albedo and Radiative Forcing of Various Aerosol Species with a Global Three-Dimensional Model , 2002 .

[22]  Alexander Smirnov,et al.  Maritime aerosol network as a component of AERONET - first results and comparison with global aerosol models and satellite retrievals , 2011 .

[23]  X. Tie,et al.  The potential changes of methane due to an assumed increased use of natural gas: A global three-dimensional model study , 1993 .

[24]  T. Petelski,et al.  Studies of vertical coarse aerosol fluxes in the boundary layer over the Baltic Sea , 2014 .

[25]  Tymon Zielinski Studies of Aerosol Physical Properties in Coastal Areas , 2004 .

[26]  A. Pietruczuk,et al.  Remote sensing measurements of the volcanic ash plume over Poland in April 2010 , 2012 .

[27]  J. Christensen The Danish Eulerian Hemispheric Model : A three-dimensional air pollution model used for the Arctic , 1997 .

[28]  I. Slutsker,et al.  Smoke aerosol and its radiative effects during extreme fire event over Central Russia in summer 2010 , 2011 .

[29]  A. Bokoye,et al.  Angström turbidity parameters and aerosol optical thickness: A study over 500 solar beam spectra , 1997 .

[30]  Marcin L. Witek,et al.  Global sea‐salt modeling: Results and validation against multicampaign shipboard measurements , 2007 .

[31]  P. Bhartia,et al.  Derivation of aerosol properties from satellite measurements of backscattered ultraviolet radiation , 1998 .

[32]  S. Kratzer,et al.  Seasonal variability in the optical properties of Baltic aerosols , 2011 .

[33]  J. Wilson,et al.  A global black carbon aerosol model , 1996 .

[34]  N. O'Neill,et al.  A study of the link between synoptic air mass type and atmospheric optical parameters , 1994 .