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Organic Aerosol: A riddle, wrapped in a mystery, inside an enigma *. Colette L. Heald - PowerPoint PPT Presentation
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Organic Aerosol: A riddle, wrapped in a mystery, inside an enigma*
University of LeedsJune 2, 2010
Colette L. Heald
Acknowledgements: Dave Ridley, Kateryna Lapina (CSU), 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)
* I’m sure Winston Churchill would have agreed with me
AEROSOL: CONNECTION TO BIG RESEARCH TOPICS IN ENVIRONMENTAL SCIENCE…A MOTIVATION TO GET IT RIGHT!
AIR QUALITY / HEALTH
Clear DayVISIBILITY BIOSPHERE-ATMOSPHERE
CLIMATE
+ oxidants
Terpenes(gas-phase)PBAP
Hydrocarbons(gas-phase & particulate)
ORGANIC AEROSOL IN PARTICULAR…
Primary Organic Aerosol: emittedSecondary Organic Aerosol: formed
NATURAL ANTHROPOGENIC
MOTIVATION #1: ORGANIC AEROSOL MAKES UP AN IMPORTANT FRACTION OF OBSERVED AEROSOL
Globally makes up 25-75% of total fine aerosol at the surface (ignoring soot here)
[Zhang et al., 2007]SulfateOrganics
MOTIVATION #2: ORGANIC AEROSOL MAY BECOME EVEN MORE IMPORTANT IN THE FUTURE!
Present-Day Burden: 1.5-2.1 Tg1
Projection:↓ by > 50% by 2100?
SULFATE
OA
1 [Koch et al., 1999; Barth et al., 2000; Takemura et al., 2000]
Present-Day Burden: ? (models ~1.6 Tg)Projection: ? [Heald et al., 2008]
OA
Bur
den
Andreae et al. [2005] suggest ↓ sulfate will accelerate greenhouse gas warming, but organics could compensate…
?
MOTIVATION #3: DEFINING THE “NATURAL” BACKGROUND
Estimating the “natural” background is CRITICAL for the indirect effect – how much have CCN values increased??
July 97 [Spracklen et al., 2005] Pre-industrial values?
More broadly, (1) How much is anthropogenic (controllable) (2) Can we predict how the natural fraction will respond to climate change?
CHALLENGES IN MODELING THE RIGHT LEVELS OF OA
SOA measured/modeled = 4-100!
[Volkamer et al., 2006]
Models do get it right sometimes (even more puzzling?) but is it for the right reason?
ITCT-2K4
IMPEXAMAZE-08
AMMA
Egbert
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
FOCUS ON TODAY:
(1) Trying to simplify our description of organic aerosol composition
(2) Look at whether measurements of AOD from space can shed any light on the budget of OA
H:C
O:C
HOW ATMOSPHERIC AGING CAN CHANGE OA COMPOSITION
OXIDATION:
Functionalization Fragmentation (break C-C bonds)
OH
Volatility Generally O:C
Volatility Composition may change(depends on where bond breaks and what caps end)
VOLATILIZATION/CONDENSATION: More oxygenated material pulled into aerosol.
PHYSICAL MIXING: Mean composition reflecting constituent air masses
Organic Aerosol Composition is DYNAMIC – what a headache for modeling!
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…
THE VAN KREVELEN DIAGRAMDeveloped by Van Krevelen in 1950’s to describe oil formation
Simple way to visualize changing composition
HOW DOES FUNCTIONALIZATION CHANGE AEROSOL COMPOSITION?
If replace aliphatic carbon (-CH2-) with functional group, composition changes as follows:
Example: Replace -CH2- with a carbonyl group -C(=O)- Add 1O, lose 2H, slope = -2
LAB & FIELD ORGANIC AEROSOL LINE UP IN A VAN KREVELEN DIAGRAM!
Surprisingly, despite complexity, aerosol composition changes during aging looks like carboxylation!
[Heald et al., 2010]
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?
WHAT DOES THIS TELL US ABOUT PROCESSES AND/OR COMPOSITION?
Lipids
Monocarboxylic Acids
Dicarboxylic Acids
Proteins
Lignin
SOA
Cellulose
Tannins
Condensed Hydrocarbons
ObservedOA
Isoprene Tetrols
→Glyoxal
Oligomers
Suggests that oligomerization is not the dominant aging process.Suggests that glyoxal oligomers and isoprene tetrols do not make up major
fraction of mass.
*regions overlaid from Wozniak et al., 2008
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
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)
FOCUS ON TODAY:
(1) Trying to simplify our description of organic aerosol composition
(2) Look at whether measurements of AOD from space can shed any light on the budget of OA
H:C
O:C
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
SOME CHALLENGES…1. AOD is an integrated measure of ALL aerosols.2. Satellite AOD observations don’t always agree, AERONET coverage sparse
MODIS
MISR
Strategy: focus on continental AOD, use MISR as a global constraint
Example of MODIS/MISR/AERONET (MAM 2008)
DO OBSERVATIONS SUPPORT MISSING SOURCE(S) OF OA?DJF JJA
Model does underestimate observed AOD in most regions/seasons.
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.
OA loading is 3.7 TgC (~230 TgC/yr) over land extrapolate to include outflow ~460 TgC/yr. (middle of Goldstein & Galbally range)
Inverted total MISR AOD: Equivalent uniform OA profile
maxz
0
(RH)[OA]dz
A MORE REALISTIC POSSIBILITY:ATTRIBUTE ALL OF MODEL UNDERESTIMATE TO OA
(assuming all the negative bias is ONLY OA)
Estimate that ~95 TgC/yr over land required to close the MISR-GEOS-Chem discrepancy. extrapolate to global ~200 TgC/yr (approximately 4 times current model OA source)
IF we remove N. Africa & the Middle East (dust) from this, total is reduced to ~160 TgC/yrLikely still too high…
DJF
JJA
Possibly dust?
Biofuels? Agriculture
UNCERTAINTIES ATTRIBUTED TO VERTICAL DISTRIBUTION
1 2
Uniform vertical profile perhaps not very realistic…
If the same mass is distributed with exponential drop off (atmospheric scale height assumed) , the AOD increases by 15%.
OA burden implied by AOD would be 15% lower (140 TgC/yr) if distributed exponentially.Surface concentrations would be ~ twice as high.
OA [g/m3]
SEASONALITY OF “INVERTED” OA BURDEN
Seasonality of “inverted” OA peaks in local spring/summer Coincident to peak in BVOC & oxidants…
COMPARISON AT AERONET SITES
Adding “extra AOD” observed by MISR does improve model ability to
capture both magnitude and variability of AERONET AOD
DJF MAM
JJA SON
GEOS-Chem simulationGEOS-Chem + “extra” AOD
DO THE SURFACE OBSERVATIONS OF OA SUPPORT A SIMILAR CONCLUSION?
Monthly mean GEOS-Chem simulation (for 2003) sampled at sites from Zhang et al, [2007] (AMS observations from 2000-2006 not exactly matched)
Jungfraujoch Tokyo (winter)
Duke Forest
ACE-Asia
Vancouver
Fukue (May)
RiversideTaunus
Beijing (32 g/m3)
Mexico (22 g/m3)
Model does generally underestimate surface OA. “Inverted” surface OA will depend on vertical distribution (use here constant profile). Adding inverted OA marginally improves ability to capture AMS magnitude and variability. The data set is limited geographically.
//
Surface OA Surface OA (including inverted)
(removing Beijing & Mexico)
Jungfraujoch
Storm Peak
Duke Forest
SENSITIVITY OF ORGANIC AEROSOL OPTICSAssumed optical properties based on GADS database and log-normal size distribution recently evaluated by Drury et al. [2010]
Uncertainty in simulated AOD due to optical properties a factor of 0.5-1.5
HAVE WE REDUCED THE UNCERTAINTY ON THE OA BUDGET?
[Heald et al., in prep]
910 TgC/yr
460 TgC/yr
200 TgC/yr
50 TgC/yr
160 TgC/yr
Goldstein and Galbally [2007]
If all AOD inverted for OA
Existing GEOS-Chem sources
If attribute all MISR “excess” AOD to OAIf remove Africa & Middle East
Observations support a continental OA source of 140 TgC/yr (or less).
Range estimated from uncertainty in optical properties
140 TgC/yr Account for “likely” vertical distribution140 TgC/yr
WHAT ABOUT MARINE SOURCES OF OA?
Kateryna Lapina
Oceanic AOD is underestimated in the model – patterns seem to match the marine OA estimated by Spracklen et al. [2008], but scaling up source by a factor of 10 required.
Spracklen et al, annual mean marine OA emissions
Spracklen et al., [2008] estimate source of 4 TgC/yr, Roelofs et al., [2008] estimate 75 TgC/yr, Gantt et al. [2009] estimate 22.3 TgC/yr , Vignati et al. [2010] estimate 4.1 TgC/yr
What about in terms of AOD?
910 TgC/yr Goldstein and Galbally [2007]
Suggests a MAXIMUM global source of ~180 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.
140 TgC/yr
180 TgC/yr
HAVE WE REDUCED THE UNCERTAINTY ON THE OA BUDGET?
CONTINENTAL
MARINE