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Volume 10, issue 6
Atmos. Chem. Phys., 10, 2765-2776, 2010
https://doi.org/10.5194/acp-10-2765-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 10, 2765-2776, 2010
https://doi.org/10.5194/acp-10-2765-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  24 Mar 2010

24 Mar 2010

Model of optical response of marine aerosols to Forbush decreases

T. Bondo et al.
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Cited articles  
Arnold, F.: Multi-ion complexes in the stratosphere – Implications for trace gases and aerosol, Nature, 284, 610–611, 1980.
Cane, H.: Coronal mass ejections and forbush decreases, Space Sci. Rev., 93, 55–77, 2000.
Clarke, A. D. and Kapustin, V. N.: A pacific aerosol survey. part I: A decade of data on particle production, transport, evolution, and mixing in the troposphere, J. Atmos. Sci., 52, 363–382, 2002.
Clarke, A., Owens, S., and Zhou, J.: An ultrafine sea-salt flux from breaking waves: Implications for cloud condensation nuclei in the remote marine atmosphere, J. Geophys. Res.-Atmos., 111, D06202, https://doi.org/10.1029/2005JD006565, 2006.
Eck, T. F., Holben, B. N., Reid, J. S., Dubovik, O., Smirnov, A., O'Neill, N. T., Slutsker, I., and Kinne, S.: Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols, J. Geophys. Res., 104, 31333–31349, 1999
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