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Volumn 35, Issue 6, 2008, Pages

Contribution of particle formation to global cloud condensation nuclei concentrations

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC COMPOSITION; ATMOSPHERIC STRUCTURE; CLOUDS; GEOPHYSICS; PARTICLE SIZE ANALYSIS;

EID: 44349106990     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2007GL033038     Document Type: Article
Times cited : (337)

References (33)
  • 1
    • 0030811481 scopus 로고    scopus 로고
    • Atmospheric sulfur and cloud condenstaion nuclei in marine air in the southern hemisphere
    • Ayers, G., et al. (1997), Atmospheric sulfur and cloud condenstaion nuclei in marine air in the southern hemisphere, Philos. Trans. R. Soc. London Ser. B, 352, 203-211.
    • (1997) Philos. Trans. R. Soc. London Ser. B , vol.352 , pp. 203-211
    • Ayers, G.1
  • 2
    • 39349102623 scopus 로고    scopus 로고
    • Birmili, W., et al. (2003), The Hohenpeissenberg aerosol formation experiment (HAFEX): A long-term study including size-resolved aerosol, H2S04, OH, and monoterpenes measurements, Atmos. Chem. Phys., 3, 361-376.
    • Birmili, W., et al. (2003), The Hohenpeissenberg aerosol formation experiment (HAFEX): A long-term study including size-resolved aerosol, H2S04, OH, and monoterpenes measurements, Atmos. Chem. Phys., 3, 361-376.
  • 3
    • 0033783877 scopus 로고    scopus 로고
    • J. Geophys. Res., 105
    • 15, 320
    • Cantrell, W., et al. (2000), Relationships between cloud condensation nuclei spectra and aerosol particles on a south-north transect of the Indian Ocean, J. Geophys. Res., 105, 15, 313-15, 320.
    • (2000) , pp. 313-315
    • Cantrell, W.1
  • 4
    • 33746239470 scopus 로고    scopus 로고
    • New version of the TOMCAT/SLIMCAT off-line chemical transport model: Intercomparison of stratospheric tracer experiments
    • Chipperfield, M. (2006), New version of the TOMCAT/SLIMCAT off-line chemical transport model: Intercomparison of stratospheric tracer experiments, Q. J. R. Meteorol. Soc., 132(617), 1179-1203.
    • (2006) Q. J. R. Meteorol. Soc , vol.132 , Issue.617 , pp. 1179-1203
    • Chipperfield, M.1
  • 5
    • 33847609559 scopus 로고    scopus 로고
    • Known and unexplored organic constituents in the Earth's atmosphere
    • Goldstein, A., and I. Galbally (2007), Known and unexplored organic constituents in the Earth's atmosphere, Environ. Sci. Technol., 41(5), 1514-1521.
    • (2007) Environ. Sci. Technol , vol.41 , Issue.5 , pp. 1514-1521
    • Goldstein, A.1    Galbally, I.2
  • 6
    • 0029412344 scopus 로고
    • A global model of natural volatile organic compound emissions
    • Guenther, A., et al. (1995), A global model of natural volatile organic compound emissions, J. Geophys. Res., 100, 8873-8892.
    • (1995) J. Geophys. Res , vol.100 , pp. 8873-8892
    • Guenther, A.1
  • 7
    • 34848821151 scopus 로고    scopus 로고
    • Boundary layer concentrations and landscape scale emissions of volatile organic compounds in early spring
    • Haapanala, S., et al. (2007), Boundary layer concentrations and landscape scale emissions of volatile organic compounds in early spring, Atmos. Chem. Phys., 7, 1869-1878.
    • (2007) Atmos. Chem. Phys , vol.7 , pp. 1869-1878
    • Haapanala, S.1
  • 8
    • 0018655035 scopus 로고
    • Measurement of the size distribution and CCN supersaturation spectrum of submicron aerosols over the ocean
    • Hoppel, W. (1979), Measurement of the size distribution and CCN supersaturation spectrum of submicron aerosols over the ocean, J. Atmos. Sci., 36, 2006-2015.
    • (1979) J. Atmos. Sci , vol.36 , pp. 2006-2015
    • Hoppel, W.1
  • 9
    • 0036184644 scopus 로고    scopus 로고
    • Analytical formulae connecting the 'real' and the apparent nucleation rate and the nuclei number concentration for atmospheric nucleation events
    • Kerminen, V.-M., and M. Kulmala (2002), Analytical formulae connecting the 'real' and the apparent nucleation rate and the nuclei number concentration for atmospheric nucleation events, J. Aerosol Sci., 33, 609-622.
    • (2002) J. Aerosol Sci , vol.33 , pp. 609-622
    • Kerminen, V.-M.1    Kulmala, M.2
  • 10
    • 25444471344 scopus 로고    scopus 로고
    • Direct observational evidence linking atmospheric aerosol formation and cloud droplet activation
    • doi:10.1029/2005GL023130
    • Kerminen, V.-M., H. Lihavainen, M. Komppula, Y. Viisanen, and M. Kulmala (2005), Direct observational evidence linking atmospheric aerosol formation and cloud droplet activation, Geophys. Res. Lett., 32, L14803, doi:10.1029/2005GL023130.
    • (2005) Geophys. Res. Lett , vol.32
    • Kerminen, V.-M.1    Lihavainen, H.2    Komppula, M.3    Viisanen, Y.4    Kulmala, M.5
  • 11
    • 33645213655 scopus 로고    scopus 로고
    • Secondary organic aerosol formation from isoprene photooxidation
    • Kroll, J., et al. (2006), Secondary organic aerosol formation from isoprene photooxidation, Environ. Sci. Technol., 40(6), 1869-1877.
    • (2006) Environ. Sci. Technol , vol.40 , Issue.6 , pp. 1869-1877
    • Kroll, J.1
  • 12
    • 0031867339 scopus 로고    scopus 로고
    • Parameterizations for sulfuric acid/water nucleation rates
    • Kulmala, M., A. Laaksonen, and L. Pirjola (1998), Parameterizations for sulfuric acid/water nucleation rates, J. Geophys. Res., 103, 8301-8307.
    • (1998) J. Geophys. Res , vol.103 , pp. 8301-8307
    • Kulmala, M.1    Laaksonen, A.2    Pirjola, L.3
  • 13
    • 3242695341 scopus 로고    scopus 로고
    • A new feedback mechanism linking forests, aerosol and climate
    • Kulmala, M., et al. (2004a), A new feedback mechanism linking forests, aerosol and climate, Atmos. Chem. Phys., 4, 557-562.
    • (2004) Atmos. Chem. Phys , vol.4 , pp. 557-562
    • Kulmala, M.1
  • 14
    • 1642492862 scopus 로고    scopus 로고
    • Formation and growth rates of ultrafine atmospheric particles: A review of observations
    • Kulmala, M., et al. (2004b), Formation and growth rates of ultrafine atmospheric particles: A review of observations, J. Aerosol Sci., 35, 143-176.
    • (2004) J. Aerosol Sci , vol.35 , pp. 143-176
    • Kulmala, M.1
  • 15
    • 33645807623 scopus 로고    scopus 로고
    • Cluster activation theory as an explanation of the linear dependence between formation rate of 3 nm particles and sulfuric acid concentration
    • Kulmala, M., et al. (2006), Cluster activation theory as an explanation of the linear dependence between formation rate of 3 nm particles and sulfuric acid concentration, Atmos. Chem. Phys., 6, 787-793.
    • (2006) Atmos. Chem. Phys , vol.6 , pp. 787-793
    • Kulmala, M.1
  • 16
    • 35148873573 scopus 로고    scopus 로고
    • Toward direct measurement of atmospheric nucleation
    • Kulmala, M., et al. (2007), Toward direct measurement of atmospheric nucleation, Science, 318, 89-92.
    • (2007) Science , vol.318 , pp. 89-92
    • Kulmala, M.1
  • 17
    • 0348197099 scopus 로고    scopus 로고
    • Estimation of different forest-related contributions to the radiative balance using observations in southern Finland
    • Kurten, T., et al. (2003), Estimation of different forest-related contributions to the radiative balance using observations in southern Finland, Boreal Environ. Res., 8, 275-285.
    • (2003) Boreal Environ. Res , vol.8 , pp. 275-285
    • Kurten, T.1
  • 19
    • 1642416735 scopus 로고    scopus 로고
    • Production of "potential" cloud condensation nuclei associated with atmospheric new-particle formation in northern Finland
    • doi:10.1029/ 2003JD003887
    • Lihavainen, H., V.-M. Kerminen, M. Komppula, J. Hatakka, V. Aaltonen, M. Kulmala, and Y. Viisanen (2003), Production of "potential" cloud condensation nuclei associated with atmospheric new-particle formation in northern Finland, J. Geophys. Res., 108(D24), 4782, doi:10.1029/ 2003JD003887.
    • (2003) J. Geophys. Res , vol.108 , Issue.D24 , pp. 4782
    • Lihavainen, H.1    Kerminen, V.-M.2    Komppula, M.3    Hatakka, J.4    Aaltonen, V.5    Kulmala, M.6    Viisanen, Y.7
  • 20
    • 34247382562 scopus 로고    scopus 로고
    • A single parameter representation of hygroscopic growth and cloud condensation nucleus activity
    • Petters, M. D., and S. M. Kreidenweis (2007), A single parameter representation of hygroscopic growth and cloud condensation nucleus activity, Atmos. Chem. Phys., 7, 1961-1971.
    • (2007) Atmos. Chem. Phys , vol.7 , pp. 1961-1971
    • Petters, M.D.1    Kreidenweis, S.M.2
  • 21
    • 33847679389 scopus 로고    scopus 로고
    • Efficiency of cloud condensation nuclei formation from ultrafine particles
    • Pierce, J. R., and P. J. Adams (2007), Efficiency of cloud condensation nuclei formation from ultrafine particles, Atmos. Chem. Phys., 7, 1367-1379.
    • (2007) Atmos. Chem. Phys , vol.7 , pp. 1367-1379
    • Pierce, J.R.1    Adams, P.J.2
  • 22
    • 34247216149 scopus 로고    scopus 로고
    • Connections between atmospheric sulphuric acid and new particle formation during QUEST III-IV campaigns in Heidelberg and Hyytiälä
    • Riipinen, I., et al. (2007), Connections between atmospheric sulphuric acid and new particle formation during QUEST III-IV campaigns in Heidelberg and Hyytiälä, Atmos. Chem. Phys., 7, 1899-1914.
    • (2007) Atmos. Chem. Phys , vol.7 , pp. 1899-1914
    • Riipinen, I.1
  • 23
    • 0347899424 scopus 로고    scopus 로고
    • Impact of biomass burning on cloud properties in the Amazon Basin
    • doi:10.1029/2001JD000985
    • Roberts, G. C., A. Nenes, J. H. Seinfeld, and M. O. Andreae (2003), Impact of biomass burning on cloud properties in the Amazon Basin, J. Geophys. Res., 108(D2), 4062, doi:10.1029/2001JD000985.
    • (2003) J. Geophys. Res , vol.108 , Issue.D2 , pp. 4062
    • Roberts, G.C.1    Nenes, A.2    Seinfeld, J.H.3    Andreae, M.O.4
  • 24
    • 0742270198 scopus 로고    scopus 로고
    • Spatial and seasonal variations in CCN distribution and the aerosol-CCN relationship over southern Africa
    • doi:10.1029/2002JD002384
    • Ross, K. E., S. J. Piketh, R. T. Bruintjes, R. P. Burger, R. J. Swap, and H. J. Annegam (2003), Spatial and seasonal variations in CCN distribution and the aerosol-CCN relationship over southern Africa, J. Geophys. Res., 108(D13), 8481, doi:10.1029/2002JD002384.
    • (2003) J. Geophys. Res , vol.108 , Issue.D13 , pp. 8481
    • Ross, K.E.1    Piketh, S.J.2    Bruintjes, R.T.3    Burger, R.P.4    Swap, R.J.5    Annegam, H.J.6
  • 25
    • 33748526526 scopus 로고    scopus 로고
    • Atmospheric sulphuric acid and aerosol formation: Implications from atmospheric measurements for nucleation and early growth mechanisms
    • Sihto, S.-L., et al. (2006), Atmospheric sulphuric acid and aerosol formation: Implications from atmospheric measurements for nucleation and early growth mechanisms, Atmos. Chem. Phys., 6, 4079-4091.
    • (2006) Atmos. Chem. Phys , vol.6 , pp. 4079-4091
    • Sihto, S.-L.1
  • 26
    • 84991666269 scopus 로고    scopus 로고
    • Modeling new particle formation during air pollution episodes: Impacts on aerosol and cloud condensation nuclei
    • doi:10.1080/02786820600714346
    • Sotiropoulou, R., et al. (2006), Modeling new particle formation during air pollution episodes: Impacts on aerosol and cloud condensation nuclei, Aerosol Sci. Technol., 40(1), 557-572, doi:10.1080/02786820600714346.
    • (2006) Aerosol Sci. Technol , vol.40 , Issue.1 , pp. 557-572
    • Sotiropoulou, R.1
  • 27
    • 26944433239 scopus 로고    scopus 로고
    • A global off-line model of size-resolved aerosol microphysics: I. Model development and prediction of aerosol properties
    • Spracklen, D., et al. (2005a), A global off-line model of size-resolved aerosol microphysics: I. Model development and prediction of aerosol properties, Atmos. Chem. Phys., 5, 2227-2252.
    • (2005) Atmos. Chem. Phys , vol.5 , pp. 2227-2252
    • Spracklen, D.1
  • 28
    • 30844458408 scopus 로고    scopus 로고
    • A global off-line model of size-resolved aerosol microphysics: II. Identification of key uncertainties
    • Spracklen, D., et al. (2005b), A global off-line model of size-resolved aerosol microphysics: II. Identification of key uncertainties, Atmos. Chem. Phys., 5, 3233-3250.
    • (2005) Atmos. Chem. Phys , vol.5 , pp. 3233-3250
    • Spracklen, D.1
  • 29
    • 33845296333 scopus 로고    scopus 로고
    • The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales
    • Spracklen, D., et al. (2006), The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales, Atmos. Chem. Phys., 6, 7323-7368.
    • (2006) Atmos. Chem. Phys , vol.6 , pp. 7323-7368
    • Spracklen, D.1
  • 30
    • 3242677755 scopus 로고    scopus 로고
    • One year boundary layer aerosol size distribution data from five nordic background stations
    • Tunved, P., et al. (2003), One year boundary layer aerosol size distribution data from five nordic background stations, Atmos. Chem. Phys., 3, 2183-2205.
    • (2003) Atmos. Chem. Phys , vol.3 , pp. 2183-2205
    • Tunved, P.1
  • 31
    • 33644861242 scopus 로고    scopus 로고
    • Is nucleation capable of explaining observed aerosol integral number increase during southerly transport over Scandinavia?
    • Tunved, P., et al. (2006), Is nucleation capable of explaining observed aerosol integral number increase during southerly transport over Scandinavia?, Tellus, 58B, 129-140.
    • (2006) Tellus , vol.58 B , pp. 129-140
    • Tunved, P.1
  • 33
    • 21044441962 scopus 로고    scopus 로고
    • Springtime cloud condensation nuclei concentrations on the west coast of Korea
    • doi:10.1029/2005GL022641
    • Yum, S. S., J. G. Hudson, K. Y. Song, and B.-C. Choi (2005), Springtime cloud condensation nuclei concentrations on the west coast of Korea, Geophys. Res. Lett., 32, L09814, doi:10.1029/2005GL022641.
    • (2005) Geophys. Res. Lett , vol.32
    • Yum, S.S.1    Hudson, J.G.2    Song, K.Y.3    Choi, B.-C.4


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