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2003 | 45 | 3 |

Tytuł artykułu

Dependence of the surf zone aerosol on wind direction and wind speed at a coastal site on the Baltic Sea

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Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Since 1992 lidar-based measurements have been carried out under various meteorological conditions and at various times of the year. The aerosol optical properties were determined in the marine boundary layer as a function of altitude using such factors as wind direction, duration and velocity and aerosol size distribution and concentration. It was confirmed that in all cases, the total aerosol concentration, size distribution and aerosol extinction increase with wind speed but decrease with altitude. In the range of wind velocities from 1 to 15 m s−1 the mean aerosol optical thickness of the atmosphere (VIS) obtained from the lidar varied from 0.1 to 0.38 for offshore winds and from 0.01 to about 0.1 for onshore winds, while the ˚Angstr¨om parameter for VIS oscillated around 0.65 for onshore winds and around 1 for offshore winds. Both parameters depended strongly on the history of the air mass above the Baltic Sea. Such aerosol optical thicknesses are in agreement with those obtained by other researchers in the Baltic Sea area.

Słowa kluczowe

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-

Czasopismo

Rocznik

Tom

45

Numer

3

Opis fizyczny

p.359-371,fig.,ref.

Twórcy

autor
  • Polish Academy of Sciences, Powstancow Warszawy 55, 81-712 Sopot, Poland

Bibliografia

  • Bokoye A. L., de la Cosiniere A., Cabot T., 1997, Angstrom turbidity parameters and aerosol optical thickness: A study over 500 solar beam spectra, J.Geophys. Res., 102 (D18), 21905–21914.
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  • Hoyningen-Huene W., Wendisch M., 1994, Variability of aerosol optical parameters by advective processes, Atmos. Environ., 28, 923–933.
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  • Kuśmierczyk-Michulec J., Darecki M., 1996, The aerosol optical thickness over the Baltic Sea, Oceanologia, 38 (4), 423–435.
  • Kuśmierczyk-Michulec J., Rozwadowska A., 1999, Seasonal changes of the aerosol optical thickness for the atmosphere over the Baltic Sea-preliminary results, Oceanologia, 41 (2), 127–145.
  • Persson T., 1999, Solar radiation climate in Sweden, Phys. Geochem. Earth (B), 24 (3), 275–279.
  • Potter J., 1987, Two-frequency lidar inversion technique, Appl. Opt., 26 (7), 1250 –1256.
  • Smirnov A., Villevalde Y., O’Neill N. T., Royer A., Tarussov A., 1995, Aerosol optical depth over the oceans: analysis in terms of synoptic air mass types, J. Geophys. Res., 100 (D8), 16639–16650.
  • Villevalde Y.V., Yakovlev V.V., Smyshlayev S.P., 1989, Measurements of atmospheric optical parameters in the Baltic Sea and Atlantic Ocean, [in:] Studies of the southern part of the Norwegian Sea, Y.Y. Kluikov (ed.), Gidrometeoizadat, Moskva, 105–110, (in Russian).
  • Weller M., Leiterer U., 1988, Experimental data on spectral aerosol optical thickness and its global distribution, Beitr. Phys. Atmos., 61 (1), 1–9.
  • Zieliński T., 1998, Changes in aerosol concentration with altitude in the marine boundary layer in coastal areas of the southern Baltic Sea, Bull. PAS, Earth Sci., 46 (3–4), 133–139.
  • Zieliński T., Chomka M., Piskozub J., Petelski T., 1998, Verification of different techniques for the measurement of marine aerosols in coastal areas, J. Aerosol Sci., 29, Suppl. 1, 853–854.
  • Zieliński T., Zieliński A., 2002, Aerosol extinction and optical thickness in the atmosphere over the Baltic Sea determined with lidar, J. Aerosol Sci., 33 (6), 47–61.
  • Zieliński T., Zieliński A., Piskozub J., Drozdowska V., Irczuk M., 1999, Aerosol optical thickness over the coastal area of the southern Baltic Sea, Opt. Appl., 29 (4), 439–447.
  • Zilitinkevitch S., Monin A., Chalikov S., 1976, Sea and atmosphere interactions, Stud. i Mater. Oceanol., 22, 282–293, (in Polish).

Typ dokumentu

Bibliografia

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Identyfikator YADDA

bwmeta1.element.agro-article-b8e00ad8-ffbc-4984-8cd3-aa3c5f56a7d5
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