Variations in the physical properties of surf generated aerosols with altitude

• Autorzy: Zieliński T.
• Języki publikacji: EN

Abstrakty

EN

Vertical profiles of marine aerosol size distribution and concentration in the marine boundary layer over surf zones depend strongly on wind speed, direction and duration as well as the sea bottom profile. The measurements in the present study were carried out in various seasons of the year with all these factors being taken into consideration. The data with respect to offshore winds were neglected in the calculations, since in such cases the major aerosol contribution was from terrigenous and anthropogenic particles. It was confirmed that in the range of wind speeds from 1 m s-1 to 12 m s-1 there were measurable differences in the concentrations, particularly in the size distribution of marine aerosol particles at two stations differing with respect to their sea bottom profiles.

Słowa kluczowe

EN

surf zone; marine aerosol; vertical profile; concentration gradient

• Wydawca: Polish Academy of Sciences, Institute of Oceanology ; Elsevier
• Czasopismo: Oceanologia
• Rocznik: 2003
• Tom: No. 45 (4)
• Strony: 643--653
• Opis fizyczny: Bibliogr. 23 poz., rys., wykr.

Twórcy

autor

Zieliński T.

• Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland,

Bibliografia

• [1] Blanchard D. C., Syzdek L. D., 1988, Film drop production as a function of bubble size, J. Geophys. Res., 93, 3649-3654.
• [2] Burk S. D., 1986, The generation, transport and deposition of marine aerosols; a turbulent modeling study, [in:] Oceanic whitecaps and their role in air-sea exchange processes, E. C. Monahan & G. Mac Niocaill (eds.), D. Reidel, Norwell, Mass., 267-268.
• [3] Carruthers D. J., Choularton T. C., 1986, The microstructure of hill cap clouds, Quart. J. Roy. Meteor. Soc., 112, 113-129.
• [4] Chomka M., Petelski T., 1997, Modelling the sea aerosol emission in the coastal zone, Oceanologia, 39 (3), 211-225.
• [5] Fairall C. W., Davidson K. L., 1986, Dynamics and modelling of aerosols in the marine atmosphere boundary layer, [in:] Oceanic whitecaps and their role in air-sea exchange processes, E. C. Monahan & G. Mac Niocaill (eds.), D. Reidel, Norwell, Mass., 195-208.
• [6] Fitzgerald J. M., 1992, Numerical simulation of the evolution of the aerosol size distribution in a remote marine boundary layer, [in:] Nucleation and atmospheric aerosols, N. Fukuta & P. E. Wagner (eds.), A. Depak, Hampton, Va., 157-160.
• [7] Gong L. S., Barrie A. L., Blanchet P. J., 1997, Modelling sea-salt aerosols in the atmosphere. 1. Model development, J. Geophys. Res., 102, 3805-3818.
• [8] Massel S. R., 2001, On the relationship between wave breaking and marine aerosol concentration in deep sea areas, Arch. Hydro-Eng. Environ. Mech., 48 (2), 31-45.
• [9] Monahan E. C., Mac Niocaill G., 1986, Oceanic whitecaps and their role in air-sea exchange processes, D. Reidel, Dortrecht, 129 pp.
• [10] Monahan E. C., Spil D. E., Davidson K. L., 1983, Model of marine aerosol generation via whitecaps and wave distribution, Preprint vol., pp. 147-158, 9th Conference on Aerospace and Aeronautical Meteorology of the AMS, Omaha.
• [11] Panin G. N., Krivickiy C. W., 1992, Aerodinamicheskaya sherohovodnost poverhnosti vodoyema, IWP RAN, Moskva, 134 pp.
• [12] Potter J., 1987, Two-frequency lidar inversion technique, Appl. Opt., 26 (7), 1250-1256.
• [13] Resch F. J., 1986, Influence of wind generated spray on evaporation, J. Geophys. Res., 94, 909-918.
• [14] Resch F. J., Darozzes S. J., Afeti G. M., 1986, Marine liquid aerosol production from bursting of air bubbles, J. Geophys. Res., 91, 1019-1029.
• [15] Van Eijk A., de Leeuw G., 1992, Modelling aerosol size distribution over the North Sea, J. Geophys. Res., 97, 14417-14429.
• [16] Wells W. C., Gal G., Munn T. W., 1977, Aerosol distribution in maritime air and predicted scattering coefficients in infrared, Appl. Opt., 16 (3), 634-659.
• [17] Wu J., 1988, Bubbles in the near-surface ocean. A general description, J. Geophys. Res., 93, 587-590.
• [18] Wu J., 1990, Comment on film drop production as a function of bubble size by D. C. Blanchard and Syzdek, J. Geophys. Res., 95, 7389-7391.
• [19] Wu J., 1992, Bubble flux and marine aerosol spectra under various wind velocities, J. Geophys. Res., 97, 2327-2333.
• [20] Zieliński T., 1997, Aerosol masses and mass gradients in the marine boundary layer over the breaker zone, Oceanologia, 39 (3), 201-209.
• [21] Zieliński A., Zieliński T., 1996, Aerosol fluxes and their gradients in the marine boundary layer over the coastal zone, Bull. PAS, Earth Sci., 44 (4), 203-211.
• [22] Zieliński T., Zieliński A., 2002, Aerosol extinction and aerosol optical thickness in the atmosphere over the Baltic Sea determined with lidar, J. Aerosol Sci., 33 (6), 47-61.
• [23] Zieliński A., Zieliński T., Piskozub J., 1997, Aerosol size distribution function in the coastal area, J. Aerosol Sci., 28, Suppl. 1, 41-42.