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Amazon has low levels of anthropogenic emissions ..

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Amazon has low levels of anthropogenic emissions ... Estimated 2 Tg per year of (1) and (2) in Amazon Basin ... cover over the Amazon arc of deforestation, ... – PowerPoint PPT presentation

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Title: Amazon has low levels of anthropogenic emissions ..


1
The Impact of Secondary Organic Aerosol
Derivatives of Isoprene on Cloud Formation and
Albedo
  • Akua Asa-Awuku
  • EAS6410 Term Paper Presentation

2
Summary
  • Motivation
  • Biogenic Emissions
  • Sources of Isoprene
  • Sources of SOA from Isoprene
  • The impact of SOAs on Cloud Formation
  • Cloud Formation and Albedo
  • Hydrological Implications

3
The Importance of Biogenic Emissions
  • Amazon has low levels of anthropogenic emissions
  • Isoprene emissions in US larger than
    anthropogenic particulate matter
  • Eight Different Vegetation Types are major
    sources of Isoprene

4
Major Sources of NMHC
Tg C yr-1
5
What is Isoprene
  • Olefinic
  • Highly reactive Double Bonds
  • Volatile Organic Compound (VOC)
  • Non-Methane Hydrogen Carbon (NHMC)

6
Products of Isoprene Photooxidation
7
Derivatives of Photoxidation
  • Assumed to be extremely volatile (e.g
    formaldehyde)
  • Assumed Most likely not to be SOAs
  • Two newly identified species hypothesized to be
    SOAs from photooxidation of isoprene
  • Formation of SOA via acidic catalysts

8
Data Collection
  • Data Samples collected from LBA-CLAIRE campaign
    July 25 -27 Claeys, 2004
  • Assumptions
  • Very low Anthropogenic emissions
  • Tropics site of high photoxidation
  • Samples Subjected to GS-MS

9
SOA from Isoprene
  • Gas Chromatography results that show presence of
    a product of isoprene photo-oxidation
  • Similar 5 carbon skeleton as that of isoprene

10
SOA from Isoprene
  • Proposed formation of the 2-methyltetrols from
    isoprene by reaction with OHO2 followed by
    self-and cross-reactions with radicals
  • Intermediate 1,2, diols have been previously
    reported under low NOx conditions Ruppert, 2000

11
Significance of (1) and (2)
  • SOAs have low yield from Isoprene photooxidation
  • However, large emissions of Isoprene, suggest
    significant annual formation of SOAs
  • Estimated 2 Tg per year of (1) and (2) in Amazon
    Basin
  • IPCC estimates 8 to 40 Tg of biogenic SOA
    annually
  • Low Vapor Pressure and High Hygroscopicity

12
SOAs via Sulfuric Acid Catalysts
  • Urban and Rural Areas contain sufficient amounts
    of background acidic catalysts
  • Also significant emissions of Isoprene in these
    regions
  • Limbeck explained that proposed pathway
    contribute to the explanation of HULIS substances
    on continental Europe

13
  • Reaction Yield increases with catalyst
  • Influence of ozone as competing oxidant
  • Effect of Relative air Humidity

14
Short Recap
  • SOAs from Isoprene Exist
  • Photooxidative products have low vapor pressures
  • Humic-like substances generated from acidic
    catalysts
  • All SOAs from Isoprene can be considered to be
    highly hydroscopic

15
Cloud Formation
  • Kohler Equation
  • Kelvin Effects
  • Strong functions of Surface Tension
  • Humic-like aerosols decrease s

16
Decreasing Surface Tension
17
Kohler Curves
18
Consequences of Surfactants
  • Great Cloud Droplet Number
  • 30 decrease in s yields a 20 increase in
    droplet number
  • Smaller cloud droplet Radii
  • Average 6 decrease in droplet size
  • Significant Change in Cloud Properties (hence
    Albedo)

19
Droplet Number and Albedo
20
Albedo and Cloud Optical Thickness
21
Susceptiblity
  • defined as the sensitivity of cloud albedo in
    comparison to cloud droplet number concentration
  • ten percent increase in droplet number
    concentration, leads to an increase of 0.75 in
    albedo

22
Albedo and Cloud Optical Thickness
23
Hydrological Cycle
Cloud Albedo
Cloud Formation
SOA Formation
Isoprene Emissions
Precipitation/ Water Stress
Surface Temperature
24
Conclusions
  • SOAs from Isoprene do exist
  • Humic-like SOAs decrease surface tensions of
    pure water by 30 increase the droplet number
    concentration by 20
  • 20 increase in droplet number, correlates to a
    change in top of atmospheric cloud albedo of
    nearly 1
  • a global mean forcing of almost -1 Wm-2 due to
    SOAs from Isoprene

25
References
  • Barth, Mary et. al., Future Scientific
    Directions Coupling between land ecosystems and
    the atmospheric hydrologic cycle through biogenic
    aerosol pathways., Bulletin of the American
    Meteorological Society, (submitted)
  • Brasseur, G., J. Orlando and G. Tyndall,
    Atmospheric Chemistry and Global Change, Oxford
    Univ. Press, New York, NY,1999
  • Claeys M, Graham B, Vas G, Wang W Vermeylen R,
    Pashaynshka V, Cafmeyer J, Guyon P, Andrae MO,
    Artaxo P, Maehunt W., Formation of Secondary
    Organic Aerosols through photooxidation of
    Isoprene, Science, 202 (5661)1173-1176 Feb. 20.
    2004
  • Helmig, Detlev .,Ben Balsley, Kenneth Davis,
    Laura R. Kcuck. Mike Jensen, John Bognar, Tyrrel
    Smith Jr., Rosaura Vasquez Arrieta, Roldolfo
    Rodriguez, and John W. Berks., Vertical profiling
    and determination of landscape fluxes of biogenic
    non methange hydrocarbons with the planetary
    boundary layer in the Peruvian Amazon, J.
    Geophys. Res.103 (D19) 25519-25532, 1998
  • Durieux, L., L.A.T. Machado, H. Laurent, The
    impact of deforestation on cloud cover over the
    Amazon arc of deforestation, Remote Sensing of
    Environ., 86, 132-140, 2003.
  • Facchini, M.., M. Mircea, S. Fuzzi, and R. J.
    Charlson, Cloud albedo enhancement by
    surface-active organic solutes in growing
    droplets, Nature, 401, 257-259. 1999
  • Fall, R. and M.C. Wildermuth. Isoprene synthase
    From biochemical mechanism to emission algorithm,
    J. Geophys. Res.103 (D19) 25599-25609, 1998.
  • Griffin, R.J., D.R. Cocker III, J.H. Seinfeld and
    D. Dabdub. Estimate of global atmospheric organic
    aerosol from oxidation of biogenic hydrocarbons,
    Geophys. Res. Lett., 26 (17), 2721-2724, 1999.
  • Guenther, A., C.N. Hewitt, D. Erickson, R. Fall,
    C. Geron, T. Graedel, P. Harley, L. Klinger, M.
    Lerdau, W.A. Mckay, T. Pierce, B. Scholes, R.
    Steinbrecher, R. Tallamraju, J. Taylor and P.
    Zimmerman, A global model of natural volatile
    organic compound emissions, J.Geophys. Res. 100,
    8873-8892,1995.
  • Guenther, A., S. Archer, J. Greenberg, P. Harley,
    D. Helmig, L. Klinger, L. Vierling, M.
    Wildermuth, Biogenic hydrocarbon emissions and
    landcover/climate change in a subtropical
    savanna, Phys. Chem. Earth (B), 24, 659-667,
    1999.
  • Jang, M., and R. Kamens, Atmospheric secondary
    aerosol formation by heterogeneous reaction of
    aldehydes in the presence of a sulfuric acid
    aerosol catalyst, Environ. Sci. Technol., 35,
    4758-4766, 2001.
  • Klinger, L.F., J. Greenberg, A. Guenther, G.
    Tyndall, P. Zimmerman, M. MBangui, J.M.
    Moutsambot, and D. Kenfck, Patterns in volatile
    organic compound emissions along a savanna
    rainforesst gradient in central Africa, J.
    Geophys. Res., 103, 1443-1454, 1998.
  • Limbeck, A., M. Kulmala, and H. Puxbuam,
    Secondary organic aerosol formation in the
    atmosphere via heterogeneous reaction of gaseous
    isoprene on acidic particles, Geophys. Res.
    Lett., 30 (19), 1996, 2003. doi
    10.1029/2003GL017738
  • Otter, L.B., Guenther, A., Greenber, J.,
    Seasonal and spatial vatirations in biogeneic
    hydrocarbon emissions from southern African
    savannas and woodlands, Atmospheric Enirmonmet,
    36, 4265-4275, 2002.
  • Pétron, G., P. Harley, J. Greenberg, A. Guenther,
    Seasonal temperature variations influence
    isoprene emission, Geophys. Res. Lett., 28,
    1707-1710, 2000.
  • Pirjola Liisa, Effects of the increased UV
    radiation and biogenic VOC emissions on Ultra
    fine sulphate aerosol Formation, J.Aerosol Sci.,
    30, 3, 355-367, 1999.
  • Roberts, G. C., M. O. Andreae, J. Zhou, P.
    Artaxo, Cloud condensation nuclei in the Amazon
    Basin Marine conditions over a continent?,
    Geophys. Res. Lett., 28, 2807-2810, 2001.
  • Seinfeld, J., and N. Pandis, Atmospheric
    Chemistry and Physics From air pollution to
    climate change, John Wiley Sons, Inc., New
    York, NY 1998.
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