Aerosol number size distributions from 3 to 500 nm diameter in the arctic marine boundary layer during summer and autumn

References

• Albrecht, B. A. 1989. Aerosols, cloud microphysics, and fractional cloudiness. Science 245, 1227–1230.
   PubMed Web of Science ®Google Scholar
• Bigg, E. K., Leck, C. and Nilsson, E. D. 1996. Sudden changes in arctic atmospheric aerosol concentrations during summer and autumn. Tellus 48B, this issue.
   Google Scholar
• Charlson, R. J., Langner, J. and Rodhe, H. 1991. Pertur-bation of the northern hemisphere radiative balance by backscattering of anthropogenic sulfate aerosols. Tellus 43AB, 152–163.
   Google Scholar
• Charlson, R. J., Schwartz, S. E., Hales, J. M., Cess, R. D., Coakley, J. A., Hansen, J. E. and Hofmann, D. J. 1992. Climate forcing by anthropogenic aerosols. Science 256, 423–430.
   Web of Science ®Google Scholar
• Clarke, A. D. 1993. Atmospheric nuclei in the Pacific mid-troposphere: Their nature, concentration and evolution. J. Geophys Res. 98D, 20633–20647.
   Web of Science ®Google Scholar
• Covert, D. S. and Heintzenberg, J. 1993. Size distribution and chemical properties of aerosol at Ny-Alesund, Svalbard. Atmos: Environ. 27A, 2989–2997.
   Web of Science ®Google Scholar
• Covert, D. S., Kapustin, V. N., Quinn, P. K. and Bates, T. S. 1992. New particle formation in the marine boundary layer. J. Geophys. Res. 97, 20581–20589.
   Web of Science ®Google Scholar
• Davidson, C. I. and Schnell, R. 1993. Arctic air and snow chemistry. Atmos. Environ. 27A, 2695–2703.
   Web of Science ®Google Scholar
• Durkee, P. A., Pfeil, F., Frost, E. and Shema, R. 1991. Global analysis of aerosol particle characteristics. Atmos. Environ. 25A, 2457–2471.
   Web of Science ®Google Scholar
• Easter, R. C. and Peters, L. K. 1994. Binary homo-geneous nucleation: temperature and relative humidity fluctuations, non-linearity and aspects of new particle production in the atmosphere. J. Appl. Meteor. 33, 775–784.
   Google Scholar
• Hegg, D. A., Radke, L. F. and Hobbs, P. V. 1990. Particle production associated with marine clouds. J. Geophys. Res. 95, 13917–13926.
   Web of Science ®Google Scholar
• Heintzenberg, J. and Leck, C. 1994. Seasonal variation of the atmospheric aerosol near the top of the marine boundary layer over Spitsbergen related to the Arctic sulphur cycle. Tellus 46B, 52–67.
   Google Scholar
• Hoppel, W. A., Frick, G. M., Fitzgerald, J. W. and Larson, R. E. 1994a. Marine boundary layer measurements of new particle formation and the effects nonprecipitating clouds have on aerosol size distribu-tion. J. Geophys. Res. 99, 14443–14459.
   Web of Science ®Google Scholar
• Hoppel, W. A., Frick, G. M., Fitzgerald, J. W. and Wattle, B. J. 1994b. A cloud chamber study of the effect that nonprecipitating water clouds have on the aerosol size distribution. Aerosol Sci. Tech. 20, 1–30.
   Web of Science ®Google Scholar
• Ito, T. 1993. Size distribution of Antarctic submicron aerosols. Tellus 45B, 145–159.
   Google Scholar
• Junge, C. 1972. Our knowledge of the physico-chemistry of aerosols in the undisturbed marine environment. J. Geophys. Res. 77, 5183–5200.
   Web of Science ®Google Scholar
• Knutson, E. O. and Whitby, K. T. 1975. Aerosol classification by electric mobility: apparatus, theory, and applications. J. Aerosol Sci. 6, 443–451.
   Google Scholar
• Lannefors, H., Heintzenberg, J. and Hansson, H.-C. 1983. A comprehensive study of physical and chemical parameters of the Arctic summer aerosol; results from the Swedish expedition Ymer-80. Tellus 35B, 40–54.
   Google Scholar
• Leck, C. and Persson, C. 1996a. The central Arctic Ocean as a source of Dimethyl Sulfide, Seasonal variability in relation to biological activity. Tellus 48B, this issue.
   Google Scholar
• Leck, C. and Persson, C. 1996b. Seasonal and short-term variability in dimethyl sulfide, sulfur dioxide and biogenic sulfur and sea salt aerosol particles in the arctic marine boundary layer during summer and autumn. Tellus 48B, this issue.
   Google Scholar
• Leck, C., Bigg, E. K., Covert, D. S., Heintzenberg, J., Maenhaut, W., Nilsson, E. D. and Wiedensohler, A. 1996. Overview of the Atmospheric research program during the International Arctic Ocean Expedition of 1991 ( IAOE-91 ) and its scientific results. Tellus 48B, this issue.
   Google Scholar
• Liu, B. Y. H. and Pui, D. Y. H. 1974. A submicron aerosol standard and the primary, absolute calibration of the condensation nuclei counter. J. Colloid and Interface Sci. 47, 155–171.
   Web of Science ®Google Scholar
• Nilsson, E. D. 1996. Planetary boundary layer structure and air-mass transport during the International Arctic Ocean Expedition, 1991. Tellus 48B, this issue.
   Google Scholar
• Nilsson, E. D. and Bigg, E. K. 1996. Influences on forma-tion and dissipation of high arctic fogs during summer and autumn and their interaction with aerosol. Tellus 48B, this issue.
   Google Scholar
• Penner, J. E., Dickinson, R. E. and O'Neill, C. A. 1992. Effects of aerosol from biomass burning and the global radiation budget. Science 256, 1432–1434.
   PubMed Web of Science ®Google Scholar
• Pruppacher, H. R. and Klett, J. D. 1978. Microphysics of clouds and precipitation. Reidel Publishing Co., Dortrecht 714 pp.
   Google Scholar
• Radke, L. F., Coakley, J. A. and King, M. D. 1989. Direct and remote sensing observations of the effects of ships on clouds. Science 246, 1146–1149.
   PubMed Web of Science ®Google Scholar
• Raes, F. and Van Dingenen, R. 1992. Simulations of condensation and cloud condensation nuclei from biogenic SO2 in the remote marine boundary layer. J. Geophys. Res. 97, 12901–12912.
   Web of Science ®Google Scholar
• Raes, F., Van Dingenen, R., Wilson, J. and Saltelli, A. 1993. Cloud condensation nuclei from dimethyl sulphide in the natural marine boundary layer. Remote versus in-situ production. Kluwer Academic Publisher, Dortrecht: 311–322.
   Google Scholar
• Rahn, K. A. 1981. Atmospheric, riverine and oceanic sources of seven trace constituents to the Arctic ocean. Atrnos. Environ. 15, 1507–1516.
   Web of Science ®Google Scholar
• Twomey, S. 1977. Atmospheric aerosols. Elsevier Scien-tific Publishing Co., Amsterdam, 302 pp.
   Google Scholar
• Whitby, E. R., McMurry, P. H., Shankar, U. and Binkowski, F. S. 1991. Modal aerosol dynamics modeling. U. S. Environmental Protection Agency, Atmospheric Research and Exposure Assessment Laboratory, 68-01-7365.
   Google Scholar
• Wiedensohler, A. 1988. An approximation of the bipolar charge distribution for particles in the submicron size range. J. Aerosol Sci. 19, 387.
   Web of Science ®Google Scholar
• Wiedensohler, A., Aalto, P., Covert, D., Heintzenberg, J. and McMurry, P. H. 1994. Intercomparison of four methods to determine size distributions of low concentration ( ˜ 100 cm-3), ultrafine aerosols (3Dp 10 nm) with illustrative data from the Arctic. Aerosol Sci. Technol. 21, 95–109.
   Web of Science ®Google Scholar
• Winklmayr, W., Reischl, G. P., Lindner, A. O. and Berner, A. 1991. A new electromobility spectrometer for the measurement of aerosol size distributions in the size range from 1 to 1000 nm. J. Aerosol. Sci. 22, 289–296.
   Web of Science ®Google Scholar