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2014 | OriginalPaper | Buchkapitel

3. The Impact of Biogenic SOA on Particle and Cloud Condensation Nuclei Concentration

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Abstract

As described in Chap. 1, the presence of biogenic SOA affects the number and size of particles in the atmosphere. Organic oxidation products may condense onto existing particles and aid their growth to larger sizes (e.g., [30]), enhance particle solubility [27], and contribute to new particle formation (e.g., [25]).

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Literatur
1.
Zurück zum Zitat Andreae MO et al (2004) Smoking rain clouds over the amazon. Science 303(5662):1337–1342CrossRef Andreae MO et al (2004) Smoking rain clouds over the amazon. Science 303(5662):1337–1342CrossRef
2.
Zurück zum Zitat Delene DJ, Deshler T (2001) Vertical profiles of cloud condensation nuclei above Wyoming. J Geophys Res Atmos 106(D12):12579–12588CrossRef Delene DJ, Deshler T (2001) Vertical profiles of cloud condensation nuclei above Wyoming. J Geophys Res Atmos 106(D12):12579–12588CrossRef
3.
Zurück zum Zitat Dentener F et al (2006) Emissions of primary aerosol and precursor gases in the years 2000 and 1750 prescribed data-sets for AeroCom. Atmos Chem Phys 6(12):4321–4344CrossRef Dentener F et al (2006) Emissions of primary aerosol and precursor gases in the years 2000 and 1750 prescribed data-sets for AeroCom. Atmos Chem Phys 6(12):4321–4344CrossRef
4.
Zurück zum Zitat Goldstein AH, Galbally IE (2007) Known and unexplored organic constituents in the earth’s atmosphere. Environ Sci Technol 41(5):1514–1521CrossRef Goldstein AH, Galbally IE (2007) Known and unexplored organic constituents in the earth’s atmosphere. Environ Sci Technol 41(5):1514–1521CrossRef
5.
Zurück zum Zitat Griffin RJ et al (1999) Estimate of global atmospheric organic aerosol from oxidation of biogenic hydrocarbons. Geophys Res Lett 26(17):2721–2724CrossRef Griffin RJ et al (1999) Estimate of global atmospheric organic aerosol from oxidation of biogenic hydrocarbons. Geophys Res Lett 26(17):2721–2724CrossRef
6.
Zurück zum Zitat Guenther A et al (1995) A global model of natural volatile organic compound emissions. J Geophys Res 100(D5):8873–8892CrossRef Guenther A et al (1995) A global model of natural volatile organic compound emissions. J Geophys Res 100(D5):8873–8892CrossRef
7.
Zurück zum Zitat Hatakka J et al (2003) Overview of the atmospheric research activities and results at Pallas GAW station. Boreal Environ Res 8:365–383 Hatakka J et al (2003) Overview of the atmospheric research activities and results at Pallas GAW station. Boreal Environ Res 8:365–383
8.
Zurück zum Zitat Heald CL et al (2010) Satellite observations cap the atmospheric organic aerosol budget. Geophys Res Lett 37(24):L24808CrossRef Heald CL et al (2010) Satellite observations cap the atmospheric organic aerosol budget. Geophys Res Lett 37(24):L24808CrossRef
9.
Zurück zum Zitat Heald CL et al (2011) Exploring the vertical profile of atmospheric organic aerosol: comparing 17 aircraft field campaigns with a global model. Atmos Chem Phys 11(24):12673–12696CrossRef Heald CL et al (2011) Exploring the vertical profile of atmospheric organic aerosol: comparing 17 aircraft field campaigns with a global model. Atmos Chem Phys 11(24):12673–12696CrossRef
10.
Zurück zum Zitat Hudson JG, Frisbie PR (1991) Surface cloud condensation nuclei and condensation nuclei measurements at Reno, Nevada. Atmos Environ Part A Gen Top 25(10):2285–2299CrossRef Hudson JG, Frisbie PR (1991) Surface cloud condensation nuclei and condensation nuclei measurements at Reno, Nevada. Atmos Environ Part A Gen Top 25(10):2285–2299CrossRef
11.
Zurück zum Zitat Kanakidou M et al (2005) Organic aerosol and global climate modelling: a review. Atmos Chem Phys 5(4):1053–1123CrossRef Kanakidou M et al (2005) Organic aerosol and global climate modelling: a review. Atmos Chem Phys 5(4):1053–1123CrossRef
12.
Zurück zum Zitat Kanawade VP et al (2011) Isoprene suppression of new particle formation in a mixed deciduous forest. Atmos Chem Phys 11(12):6013–6027CrossRef Kanawade VP et al (2011) Isoprene suppression of new particle formation in a mixed deciduous forest. Atmos Chem Phys 11(12):6013–6027CrossRef
13.
Zurück zum Zitat Kiendler-Scharr A et al (2009) New particle formation in forests inhibited by isoprene emissions. Nature 461(7262):381–384CrossRef Kiendler-Scharr A et al (2009) New particle formation in forests inhibited by isoprene emissions. Nature 461(7262):381–384CrossRef
14.
Zurück zum Zitat Kirkby J et al (2011) Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation. Nature 476(7361):429–433CrossRef Kirkby J et al (2011) Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation. Nature 476(7361):429–433CrossRef
15.
Zurück zum Zitat Komppula M et al (2003) Observations of new particle formation and size distributions at two different heights and surroundings in subarctic area in northern Finland. J Geophys Res Atmos 108(D9):4295CrossRef Komppula M et al (2003) Observations of new particle formation and size distributions at two different heights and surroundings in subarctic area in northern Finland. J Geophys Res Atmos 108(D9):4295CrossRef
16.
Zurück zum Zitat Kroll JH et al (2005) Secondary organic aerosol formation from isoprene photooxidation under high-NOx conditions. Geophys Res Lett 32(18):L18808CrossRef Kroll JH et al (2005) Secondary organic aerosol formation from isoprene photooxidation under high-NOx conditions. Geophys Res Lett 32(18):L18808CrossRef
17.
Zurück zum Zitat Kroll JH et al (2006) Secondary organic aerosol formation from isoprene photooxidation. Environ Sci Technol 40(6):1869--1877CrossRef Kroll JH et al (2006) Secondary organic aerosol formation from isoprene photooxidation. Environ Sci Technol 40(6):1869--1877CrossRef
18.
Zurück zum Zitat Kulmala M et al (1998) Parameterisations for sulphuric acid/water nucleation rates. J Geophys Res Atmos 103(D7):8301–8307CrossRef Kulmala M et al (1998) Parameterisations for sulphuric acid/water nucleation rates. J Geophys Res Atmos 103(D7):8301–8307CrossRef
19.
Zurück zum Zitat Kulmala M et al (1998) Analysis of the growth of nucleation mode particles observed in Boreal forest. Tellus B 50(5):449–462CrossRef Kulmala M et al (1998) Analysis of the growth of nucleation mode particles observed in Boreal forest. Tellus B 50(5):449–462CrossRef
20.
Zurück zum Zitat Kulmala M et al (2001) Overview of the international project on biogenic aerosol formation in the boreal forest (BIOFOR). Tellus B 53(4):324–343CrossRef Kulmala M et al (2001) Overview of the international project on biogenic aerosol formation in the boreal forest (BIOFOR). Tellus B 53(4):324–343CrossRef
21.
Zurück zum Zitat Kulmala M et al (2006) Cluster activation theory as an explanation of the linear dependence between formation rate of 3 nm particles and sulphuric acid concentration. Atmos Chem Phys 6:787–793CrossRef Kulmala M et al (2006) Cluster activation theory as an explanation of the linear dependence between formation rate of 3 nm particles and sulphuric acid concentration. Atmos Chem Phys 6:787–793CrossRef
22.
Zurück zum Zitat Lee LA et al (2013) The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei. Atmos Chem Phys 13:8879–8914CrossRef Lee LA et al (2013) The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei. Atmos Chem Phys 13:8879–8914CrossRef
23.
Zurück zum Zitat Mann GW et al (2012) Intercomparison of modal and sectional aerosol microphysics representations within the same 3-D global chemical transport model. Atmos Chem Phys 12(10):4449–4476CrossRef Mann GW et al (2012) Intercomparison of modal and sectional aerosol microphysics representations within the same 3-D global chemical transport model. Atmos Chem Phys 12(10):4449–4476CrossRef
24.
Zurück zum Zitat Merikanto J et al (2009) Impact of nucleation on global CCN. Atmos Chem Phys 9:8601–8616CrossRef Merikanto J et al (2009) Impact of nucleation on global CCN. Atmos Chem Phys 9:8601–8616CrossRef
25.
Zurück zum Zitat Metzger A et al (2010) Evidence for the role of organics in aerosol particle formation under atmospheric conditions. Proc Natl Acad Sci 107(15):6646–6651CrossRef Metzger A et al (2010) Evidence for the role of organics in aerosol particle formation under atmospheric conditions. Proc Natl Acad Sci 107(15):6646–6651CrossRef
26.
Zurück zum Zitat Paasonen P et al (2010) On the roles of sulphuric acid and low-volatility organic vapours in the initial steps of atmospheric new particle formation. Atmos Chem Phys 10(22):11223–11242CrossRef Paasonen P et al (2010) On the roles of sulphuric acid and low-volatility organic vapours in the initial steps of atmospheric new particle formation. Atmos Chem Phys 10(22):11223–11242CrossRef
27.
Zurück zum Zitat Petters MD et al (2006) Chemical aging and the hydrophobic-to-hydrophilic conversion of carbonaceous aerosol. Geophys Res Lett 33(24):L24806CrossRef Petters MD et al (2006) Chemical aging and the hydrophobic-to-hydrophilic conversion of carbonaceous aerosol. Geophys Res Lett 33(24):L24806CrossRef
28.
Zurück zum Zitat Reddington CL et al (2011) Primary versus secondary contributions to particle number concentrations in the European boundary layer. Atmos Chem Phys 11(23):12007–12036CrossRef Reddington CL et al (2011) Primary versus secondary contributions to particle number concentrations in the European boundary layer. Atmos Chem Phys 11(23):12007–12036CrossRef
29.
Zurück zum Zitat Riccobono F et al (2014) Oxidation products of biogenic emissions contribute to nucleation of atmospheric particles. Science 344(6185):717–721CrossRef Riccobono F et al (2014) Oxidation products of biogenic emissions contribute to nucleation of atmospheric particles. Science 344(6185):717–721CrossRef
30.
Zurück zum Zitat Riipinen I et al (2011) Organic condensation: a vital link connecting aerosol formation to cloud condensation nuclei (CCN) concentrations. Atmos Chem Phys 11(8):3865–3878CrossRef Riipinen I et al (2011) Organic condensation: a vital link connecting aerosol formation to cloud condensation nuclei (CCN) concentrations. Atmos Chem Phys 11(8):3865–3878CrossRef
31.
Zurück zum Zitat Roberts GC et al (2001) Cloud condensation nuclei in the Amazon Basin: “marine” conditions over a continent? Geophys Res Lett 28(14):2807–2810CrossRef Roberts GC et al (2001) Cloud condensation nuclei in the Amazon Basin: “marine” conditions over a continent? Geophys Res Lett 28(14):2807–2810CrossRef
32.
Zurück zum Zitat Spracklen DV et al (2005) A global off-line model of size-resolved aerosol microphysics: II. Identification of key uncertainties. Atmos Chem Phys 5(12):3233–3250CrossRef Spracklen DV et al (2005) A global off-line model of size-resolved aerosol microphysics: II. Identification of key uncertainties. Atmos Chem Phys 5(12):3233–3250CrossRef
33.
Zurück zum Zitat Spracklen DV (2005) Development and application of a global model of aerosol processes, University of Leeds. UK, PhD Spracklen DV (2005) Development and application of a global model of aerosol processes, University of Leeds. UK, PhD
34.
Zurück zum Zitat Spracklen DV et al (2006) The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales. Atmos Chem Phys 6(12):5631–5648CrossRef Spracklen DV et al (2006) The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales. Atmos Chem Phys 6(12):5631–5648CrossRef
35.
Zurück zum Zitat Spracklen DV et al (2008) Contribution of particle formation to global cloud condensation nuclei concentrations. Geophys Res Lett 35(6):L06808CrossRef Spracklen DV et al (2008) Contribution of particle formation to global cloud condensation nuclei concentrations. Geophys Res Lett 35(6):L06808CrossRef
36.
Zurück zum Zitat Spracklen DV et al (2010) Explaining global surface aerosol number concentrations in terms of primary emissions and particle formation. Atmos Chem Phys 10(10):4775–4793CrossRef Spracklen DV et al (2010) Explaining global surface aerosol number concentrations in terms of primary emissions and particle formation. Atmos Chem Phys 10(10):4775–4793CrossRef
37.
Zurück zum Zitat Spracklen DV et al (2011) Aerosol mass spectrometer constraint on the global secondary organic aerosol budget. Atmos Chem Phys 11(23):12109–12136CrossRef Spracklen DV et al (2011) Aerosol mass spectrometer constraint on the global secondary organic aerosol budget. Atmos Chem Phys 11(23):12109–12136CrossRef
38.
Zurück zum Zitat Spracklen DV et al (2011) Global cloud condensation nuclei influenced by carbonaceous combustion aerosol. Atmos Chem Phys 11(17):9067–9087CrossRef Spracklen DV et al (2011) Global cloud condensation nuclei influenced by carbonaceous combustion aerosol. Atmos Chem Phys 11(17):9067–9087CrossRef
39.
Zurück zum Zitat Stier P et al (2005) The aerosol-climate model ECHAM5-HAM. Atmos Chem Phys 5(4):1125–1156CrossRef Stier P et al (2005) The aerosol-climate model ECHAM5-HAM. Atmos Chem Phys 5(4):1125–1156CrossRef
40.
Zurück zum Zitat Tunved P et al (2004) An investigation of processes controlling the evolution of the boundary layer aerosol size distribution properties at the Swedish background station Aspvreten. Atmos Chem Phys 4(11/12):2581–2592CrossRef Tunved P et al (2004) An investigation of processes controlling the evolution of the boundary layer aerosol size distribution properties at the Swedish background station Aspvreten. Atmos Chem Phys 4(11/12):2581–2592CrossRef
41.
Zurück zum Zitat Tunved P et al (2004) A pseudo-Lagrangian model study of the size distribution properties over Scandinavia: transport from Aspvreten to Värriö. Atmos. Chem. Phys. Discuss. 4(6):7757–7794CrossRef Tunved P et al (2004) A pseudo-Lagrangian model study of the size distribution properties over Scandinavia: transport from Aspvreten to Värriö. Atmos. Chem. Phys. Discuss. 4(6):7757–7794CrossRef
42.
Zurück zum Zitat Vestin A et al (2007) Cloud-nucleating properties of the Amazonian biomass burning aerosol: cloud condensation nuclei measurements and modeling. J Geophys Res Atmos 112(D14):D14201CrossRef Vestin A et al (2007) Cloud-nucleating properties of the Amazonian biomass burning aerosol: cloud condensation nuclei measurements and modeling. J Geophys Res Atmos 112(D14):D14201CrossRef
43.
Zurück zum Zitat Williams E et al (2002) Contrasting convective regimes over the Amazon: implications for cloud electrification. J Geophys Res Atmos 107(D20):8082CrossRef Williams E et al (2002) Contrasting convective regimes over the Amazon: implications for cloud electrification. J Geophys Res Atmos 107(D20):8082CrossRef
Metadaten
Titel
The Impact of Biogenic SOA on Particle and Cloud Condensation Nuclei Concentration
verfasst von
Catherine E. Scott
Copyright-Jahr
2014
DOI
https://doi.org/10.1007/978-3-319-07851-9_3