organic aerosol: from oxidation to optical depth igac conference, halifax, canada july 14, 2010...
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Organic Aerosol: From Oxidation to Optical Depth
IGAC Conference, Halifax, CanadaJuly 14, 2010
Colette L. Heald
Acknowledgements: Jesse Kroll (MIT), Jose Jimenez, Ken Docherty, Delphine Farmer, Pete DeCarlo, Allison Aiken (CU-Boulder, currently or former), Qi Chen &
Scot Martin (Harvard), Paulo Artaxo (University of Sao Paulo)David Ridley (CSU), Easan Drury (NREL)
ORGANIC AEROSOL MAKES UP AN IMPORTANT FRACTION OF OBSERVED AEROSOL, YET MODELS STRUGGLE TO
REPRODUCE THESE CONCENTRATIONS
Globally makes up 25-75% of total fine aerosol at the surface (ignoring soot here)
[Zhang et al., 2007]SulfateOrganics
WHY DON’T MODELS GET IT RIGHT….
Terpenes(gas-phase)PBAP
Hydrocarbons(gas-phase & particulate)
Uncertain Formation (Missing sources? Poorly understood processes?)
Continuing Oxidation/Partitioning in the Atmosphere
10,000’s of (unidentified?) compounds with variable properties
A SIMPLIFIED DESCRIPTION OF ORGANIC AEROSOL COMPOSITION
[Goldstein et al., 2008]
Typically < 20% of OA mass can be identified [Williams et al., 2007].
Even if we could identify these species, global models couldn’t handle this complexity!
2D chromatogram of OA
Hydrogen
Carbon
OxygenOther
(N, S, etc)
Alternate: Look at bulk elemental composition of aerosol
Need a framework to compare composition & track changes…
A FRAMEWORK FOR LOOKING AT CHANGES IN COMPOSITION: THE VAN KREVELEN DIAGRAM
Example: Replace -CH2- with a carbonyl group -C(=O)- Add 1O, lose 2H, slope = -2
Developed by Van Krevelen in 1950’s to describe oil formation
Can be used to describe dynamic oxidation processes in the atmosphere: functionalization
of an aliphatic carbon (-CH2-) shown here
LAB & FIELD ORGANIC AEROSOL LINE UP IN A VAN KREVELEN DIAGRAM!
Surprisingly, despite complexity, MEAN aerosol composition changes during aging look like carboxylation!
All measurements taken with the high resolution Aerosol Mass Spectrometer
(HR-AMS)
EXAMPLES FROM THREE FIELD CAMPAIGNS…
Riverside, California: dominated by urban sources
Amazon basin: clean, low loadings, more oxygenated
Mexico city (aircraft): regional sampling (clean & polluted)
Photochemical clock shows moves “down” the line with aging.
Some leveling off with long ages?
IMPLICATIONS
2. From a lab perspective: why does bulk OA “collapse” to this composition? What are the details of fragmentation & functionalization reactions in the atmosphere that result in net carboxylation?
1. From a modeling perspective: hope for a simple parameterization!
Need to understand aging timescale better (how fast do we move down the -1 slope?)
…
H:C
O:C
[Heald, Kroll et al., 2010]
A LARGE MISSING SOURCE OF ORGANIC AEROSOL?Goldstein and Galbally [2007] suggest that SOA source may be anywhere from 140-910 TgC/yr.
Can total aerosol optical depth (AOD) measurements shed any light on the total budget of OA?
For comparison, current model (GEOS-Chem) estimates total ~50 TgC/yr(~2/3 POA, 1/3 SOA), equivalent burden ~0.81 TgC
TgC yr-1
SATELLITE OBSERVATIONS: ADVANTAGES & CHALLENGES
ADVANTAGE: Global view of total atmospheric columnCHALLENGE: AOD is an integrated measure of ALL aerosols – uncertainty on any single
derived particle type will be high.
Strategy: focus on continental AOD, use MISR as a global constraint
Example of MISR/AERONET (MAM 2008)
IF ONLY AEROSOL IN THE ATMOSPHERE WAS OA, WHAT LOADING IS IMPLIED BY SATELLITE AOD?
Calculate the “hypothetical” AOD implied by a constant 1 g/m3 profile over the land, and see how we need to scale this locally to make up ENTIRE AOD reported by MISR.
Inverted OA loading is 3.7 TgC over land.Assume a 6 days lifetime = 230 TgC/yr
extrapolate to include outflow ~460 TgC/yr. (middle of Goldstein & Galbally range)
Inverted total MISR AOD: Equivalent uniform OA profile
topz
0
AOD= α RH z M z dz
A MORE REALISTIC POSSIBILITY:REMOVE CONTRIBUTIONS FROM DUST, BC, INORGANICS
(assuming all the negative bias in the model is ONLY OA)
Estimate that ~230 TgC/yr source is required to close the
MISR-GEOS-Chem discrepancy.
IF we remove N. Africa & the Middle East (dust) from this,
total is reduced to ~180 TgC/yr
If then account for more “reasonable” vertical profile,
reduce to ~160 TgC/yr
DJF JJA
MISR
GEOS-Chem*
MISR-GEOS-Chem*
*excluding OA
910
460
230
47
180
If all AOD inverted for OA
Existing GEOS-Chem sources
If attribute all MISR “excess” AOD to OAIf remove N. Africa & Middle East
140 Best estimate (“likely” vertical distribution)160
Range estimated
by: Goldstein
and Galbally [2007]
All units in TgC/yr
HAVE WE REDUCED THE UNCERTAINTY ON THE OA BUDGET?
[Heald et al., in prep]
Suggests a MAXIMUM global source of ~160 TgC/yr of OA to the atmosphere.
This is more than THREE TIMES what is currently included in global models….
BUT at the low end of Goldstein & Gallbally [2007] range.
* Detailed uncertainty analysis suggests budget derived from AOD has ~80% uncertainty