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Ultrafine Particles and Climate Change

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Title: Ultrafine Particles and Climate Change


1
Ultrafine Particles and Climate Change
  • Peter J. Adams

HDGC Seminar November 5, 2003
2
Overview
  • Introduction
  • climate effects of aerosols
  • aerosol size distribution, mass / number
    concentrations
  • Ultrafine particles and clouds

3
Overview
  • 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

4
Theme
  • Regulations based on mass concentrations (PM10
    and PM2.5)
  • less attention to modeling number concentrations
    (i.e. ultrafines)

5
Theme
  • 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

6
Theme
  • 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)

7
Earths Energy Budget
Anthropogenic GHGs 2.5 W m-2
8
Aerosols and Climate Direct Effect
Direct Effect Scattering and absorption
by particles
photo SeaWifs website
9
Aerosols and Climate Direct Effect
Direct Effect Scattering and absorption
by particles
Roughly proportional to aerosol mass
concentration
photo SeaWifs website
10
Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
activation / nucleation
11
Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
Clean Air
Polluted Air
12
Indirect Effect on Climate
Aerosol Particles
Cloud Droplets
First indirect effect albedo Second indirect
effect lifetime
Clean Air
Brighter, more persistent clouds
Polluted Air
13
Aerosols and Climate Indirect Effect
AVHRR observation of indirect effect
Red visible Green 3.7 mm solar IR Blue
infrared
14
Aerosols 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
15
Aerosol Activation
  • Activation formation of cloud droplet
  • involves a competition between solute
  • and surface tension effects

Number
  • Diameter

16
Aerosol Activation
  • Activation formation of cloud droplet
  • involves a competition between solute
  • and surface tension effects

Depends on number concentration above critical
diameter
Number
  • Diameter

17
Source IPCC Third Assessment Report
18
Typical Number Distribution
19
Typical Mass Distribution
20
Previous 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
21
Previous 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
22
Aerosol Microphysics
Nucleation Emissions
Coagulation Condensation
Deposition
Number
  • Diameter

23
Two-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
24
Two-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
25
Aerosol Microphysics
  • 30,000 grid cells
  • 1 year
  • Adaptive time steps

General Dynamic Equation
  • Coagulation

Condensation
26
Model 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

27
Size Distributions
28
Size Distributions
29
Van Dingenen et al., 1995 JGOFS cruise Sep/Oct,
1992
30
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31
CCN (cm-3) 0.2 Supersaturation
32
Uncertainties
  • 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

33
Sensitivity 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

34
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35
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36
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37
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38
Vertical Profiles
39
CCN Vertical Profiles
40
CCN Vertical Profiles
41
Ultrafine Particles and CCN
Number
  • Diameter

42
Ultrafine Particles and CCN
Condensation to accumulation mode does
not produce new CCN
Condensation
Number
Growth
  • Diameter

43
Ultrafine Particles and CCN
Additional ultrafine particles result in
enhanced CCN formation
Condensation to accumulation mode does
not produce new CCN
Condensation
Number
Growth
  • Diameter

44
Impact of Particulate Emissions
SO2 emissions SO2/SO42- emissions
45
Summary 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?
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