Title: Amazon has low levels of anthropogenic emissions ..
1The Impact of Secondary Organic Aerosol
Derivatives of Isoprene on Cloud Formation and
Albedo
- Akua Asa-Awuku
- EAS6410 Term Paper Presentation
2Summary
- Motivation
- Biogenic Emissions
- Sources of Isoprene
- Sources of SOA from Isoprene
- The impact of SOAs on Cloud Formation
- Cloud Formation and Albedo
- Hydrological Implications
3The 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
4Major Sources of NMHC
Tg C yr-1
5What is Isoprene
- Olefinic
- Highly reactive Double Bonds
- Volatile Organic Compound (VOC)
- Non-Methane Hydrogen Carbon (NHMC)
6Products of Isoprene Photooxidation
7Derivatives 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
8Data 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
9SOA from Isoprene
- Gas Chromatography results that show presence of
a product of isoprene photo-oxidation - Similar 5 carbon skeleton as that of isoprene
10SOA 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
11Significance 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
12SOAs 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
14Short 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
15Cloud Formation
- Kohler Equation
- Kelvin Effects
- Strong functions of Surface Tension
- Humic-like aerosols decrease s
16Decreasing Surface Tension
17Kohler Curves
18Consequences 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)
19Droplet Number and Albedo
20Albedo and Cloud Optical Thickness
21Susceptiblity
- 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
22Albedo and Cloud Optical Thickness
23Hydrological Cycle
Cloud Albedo
Cloud Formation
SOA Formation
Isoprene Emissions
Precipitation/ Water Stress
Surface Temperature
24Conclusions
- 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
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