Title: Ultrafine Particles and Climate Change
1Ultrafine Particles and Climate Change
HDGC Seminar November 5, 2003
2Overview
- Introduction
- climate effects of aerosols
- aerosol size distribution, mass / number
concentrations - Ultrafine particles and clouds
3Overview
- Introduction
- climate effects of aerosols
- aerosol size distribution, mass / number
concentrations - Ultrafine particles and clouds
- Theme
- Aerosol (particulate matter) models developed for
PM regulations / visibility are inadequate for
newer issues
4Theme
- Regulations based on mass concentrations (PM10
and PM2.5) - less attention to modeling number concentrations
(i.e. ultrafines)
5Theme
- Regulations based on mass concentrations (PM10
and PM2.5) - less attention to modeling number concentrations
(i.e. ultrafines) - Ultrafines cause concern
- health effects
- climate change
6Theme
- Regulations based on mass concentrations (PM10
and PM2.5) - less attention to modeling number concentrations
(i.e. ultrafines) - Ultrafines cause concern
- health effects
- climate change
- Sources of ultrafines poorly understood
- direct (primary) emission by combustion
- atmospheric formation from supersaturated gases
(nucleation)
7Earths Energy Budget
Anthropogenic GHGs 2.5 W m-2
8Aerosols and Climate Direct Effect
Direct Effect Scattering and absorption
by particles
photo SeaWifs website
9Aerosols and Climate Direct Effect
Direct Effect Scattering and absorption
by particles
Roughly proportional to aerosol mass
concentration
photo SeaWifs website
10Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
activation / nucleation
11Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
Clean Air
Polluted Air
12Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
First indirect effect albedo Second indirect
effect lifetime
Clean Air
Brighter, more persistent clouds
Polluted Air
13Aerosols and Climate Indirect Effect
AVHRR observation of indirect effect
Red visible Green 3.7 mm solar IR Blue
infrared
14Aerosols and Climate Indirect Effect
AVHRR observation of indirect effect
Power plant
Lead smelter
Port
Oil refineries
Red visible Green 3.7 mm solar IR Blue
infrared
15Aerosol Activation
- Activation formation of cloud droplet
- involves a competition between solute
- and surface tension effects
Number
16Aerosol Activation
- Activation formation of cloud droplet
- involves a competition between solute
- and surface tension effects
Depends on number concentration above critical
diameter
Number
17Source IPCC Third Assessment Report
18Typical Number Distribution
19Typical Mass Distribution
20Previous Work
Ultrafine
Cloud Droplets (cm-3)
CCN
Boucher Lohmann, 1995
Sulfate Mass (mg m-3)
- Mechanistic number of cloud drops depends on
number of particles large enough to activate
Empirical number of cloud drops correlated with
sulfate mass based on observations
21Previous Work
- I Martin et al. 1994
- -0.68 W/m2
- II Martin et al. with background CCN
- -0.40 W/m2
- III Jones et al. 1994
- -0.80 W/m2
- IV Boucher and Lohmann 1995
- -1.78 W/m2
Cloud Droplets (cm-3)
Sulfate Mass (mg m-3)
It is argued that a less empirical and more
physically based approach is required
Kiehl et al. 2000
22Aerosol Microphysics
Nucleation Emissions
Coagulation Condensation
Deposition
Number
23Two-Moment Sectional Algorithm
- This work two moments of the size
- distribution (mass and number)
- are tracked for each size bin.
- Air quality regulatory model
- tracks mass in each size bin
Tzivion et al., JAS 44, 3139 3149, 1987 Adams
et al., JGR 10.1029/2001JD001010, 2002
24Two-Moment Sectional Algorithm
- This work two moments of the size
- distribution (mass and number)
- are tracked for each size bin.
- Air quality regulatory model
- tracks mass in each size bin
- Two-moment method conserves
both mass and number precisely - Prevents numerical diffusion present in
single-moment methods - Excellent size resolution 30 sections from .01
mm to 10 mm
Tzivion et al., JAS 44, 3139 3149, 1987 Adams
et al., JGR 10.1029/2001JD001010, 2002
25Aerosol Microphysics
- 30,000 grid cells
- 1 year
- Adaptive time steps
General Dynamic Equation
Condensation
26Model Structure
- Aerosol composition
- Current Sulfate / Sea-salt
- Development Organic / Elemental carbon
- Future Mineral dust
- Processes
- Emissions
- Chemistry
- Microphysics
- Cloud processing
- Size-resolved dry / wet deposition
27Size Distributions
28Size Distributions
29Van Dingenen et al., 1995 JGOFS cruise Sep/Oct,
1992
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31CCN (cm-3) 0.2 Supersaturation
32Uncertainties
- Particulate Emissions
- Most sulfate aerosol mass results from gas-phase
SO2 emissions - Particulate sulfate lt5 of anthropogenic sulfur
emissions - Nucleation of new aerosol particles
- Important uncertainties in mechanism and rate
- Both processes contribute significant numbers of
small particles - insignificant contribution to sulfate mass
- important contribution to aerosol number
concentrations and size distributions
33Sensitivity Scenarios
- Base Case
- 1985 sulfur emissions
- all emissions as gas-phase SO2
- nucleation based on critical concentration from
binary (H2SO4-H2O) theory - Primary Emissions
- 3 of sulfur emissions as sulfate
- Enhanced Nucleation
- critical H2SO4 concentration factor of 10 lower
- Pre-industrial
- no anthropogenic emissions
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38Vertical Profiles
39CCN Vertical Profiles
40CCN Vertical Profiles
41Ultrafine Particles and CCN
Number
42Ultrafine Particles and CCN
Condensation to accumulation mode does
not produce new CCN
Condensation
Number
Growth
43Ultrafine Particles and CCN
Additional ultrafine particles result in
enhanced CCN formation
Condensation to accumulation mode does
not produce new CCN
Condensation
Number
Growth
44Impact of Particulate Emissions
SO2 emissions SO2/SO42- emissions
45Summary and Conclusions
- A regulatory model (mass concentrations) omits
important physics - Ultrafine particles have a significant impact on
clouds via CCN number concentrations - Require better knowledge of sources of ultrafines
- nucleation
- primary emissions from combustion
- Future changes in ultrafine emissions?