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Aerosols and climateRob Wood, Atmospheric Sciences
What are aerosols?What are aerosols?
• Solid or liquid particles suspended in air
• Sizes range from a few nm to a few thousand nm⇒ Huge range of masses
Where do aerosols come from?
Estimate of Present-Day Global Emission of Major Aerosol Types (in Tg/year)
Present flux
Source Low High Best
Present flux
Source Low High Best
j yp ( g y )
NaturalPrimary
Soil dust (mineral aerosol)
1,000 3,000 1,500
AnthropogenicPrimary
Industrial dust etc. 40 130 100
Bl k b ( t d 10 30 20aerosol)
Sea salt 1,000 10,000 1,300
Volcanic dust 4 10,000 33
Black carbon (soot and charcoal)
10 30 20
Secondary
Sulphates from SO 120 180 140Biological debris 26 80 50
Secondary
Sulphates from SO2 120 180 140Biomass burning (w/o black carbon)
50 140 80
Nitrates from NOx 20 50 36Sulfates from biogenic gases
60 110 90
Sulfates from volcanic SO2
4 45 12
x 20 50 36Organics from anthropogenic NMHC*
5 25 10
Organic matter from biogenic NMHC*
10 200 55
Nitrates from NOx 10 40 22
1 10 100 103 104 105 106 [nm]
Aerosols and light scattering• Scattering of solar radiation per unit mass is maximum
when particle size is close to solar wavelengths (λ ~ 400-800 nm))
• Particles in the size range 200-2000 nm are most efficient scatterers
• Particle surface area more important than massParticle surface area more important than mass
er m
ass
ffici
ency
pat
terin
g ef
10 100 1000 10000
Particle diameter [nm]
Sca
Surface area and massSurface area and mass
• M = (4π/3) ρ r3M (4π/3) ρ r• A = 4π r2
• A/M ∝ 1/r per m
ass
A/M ∝ 1/r
• when r « λ scattering effic
ienc
y p
when r « λ scattering efficiency increases with r4
catte
ring
e
⇒ r<100 nm particles don’t matter
10 100 1000 10000
Particle diameter [nm]
Sc
[ ]
Aerosols and light scattering
• If aerosol particle is soluble then size willIf aerosol particle is soluble then size will depend upon water uptake
• Water uptake depends upon relative humidity p p p y(RH)
• For given number of particles, scattering will g p , gincrease with RH
• But with no particles there is no scattering despite what the RH is
Size as a function of RH
Chemical composition affects thgrowth
r/rdr
y 3 marine airmass
acto
r rw
th fa 2
grow
1 polluted airmass
RH1 p
What determines scattering?What determines scattering?
• For particles of size > 200 nm, surface area p ,determines scattering from one particle
• Multiply this by the number concentration of i l ll i i lparticles to get overall scattering per unit volume
of air• A ∝ N r2 M ∝ N r3• Atot ∝ N r2, Mtot ∝ N r3
⇒ Atot ∝ N1/3 M2/3
• Need to know both total aerosol mass and the number concentration
Importance of sulfate
• Sulfate aerosols dominate the scattering over continental regionscontinental regions
• Anthropogenic sources comparable to natural sourcessources
• Regionally, this scattering can seriously degrade visibilityvisibility
• Globally, this scattering reduces solar radiation entering the climate system by ≈2 W m-2entering the climate system by ≈2 W m
• Studies suggest that about 0.3-0.8 W m-2 of this scattering are from anthropogenic aerosols, g p g ,mostly sulfate (“direct” effect of aerosols)
Beijing after rain Beijing during dry period
Solar radiation reaching the surfaceSolar radiation reaching the surface
Global Sulfur BudgetRates in Tg S yr-1
SO2
SO42-
τ 3 9dOH
cloud42
2
τ = 1.3d
OHNO3
τ = 3.9dOH
8184H2SO4(g)
(CH3)2S(DMS) 1 0d
OHNO3
10 64 dep27 dry
dep6 dry
τ = 1.0d
22
27 dry20 wet
y44 wet
Phytoplankton Volcanoes Combustion/Smelters
Global Sulfur Emission PatternsGlobal Sulfur Emission Patterns
Chin et al. [2000]
SO2 sources by type
Direct effect of laerosols upon
solar radiation
• Aerosols scatter solar radiationradiation
• More particles ⇒ more scatteringg
• Some scattered radiation returns to spacespace
• Reduction in amount entering climate systemg y
• ⇒ Cooling effect
Aerosol optical depth (measure of scattering)scattering)
How well do we
understand hhuman
influence?
• Direct radiative forcing (effect of g (anthropogenic emissions on aerosolaerosol scattering) from different models
Trends in U.S. NOx AND SO2 EmissionsEmissions
Aerosol-cloud-climate interactions
More aerosol-Climate effects
Cloud droplets form on aerosol particlesCloud droplets form on aerosol particles
• For soluble aerosols, particle size increases with RHp
• When a parcel of air rises, it cools and the RH increases
• When RH>1 the soluble aerosols can “activate” (grow• When RH>1, the soluble aerosols can activate (grow unstably into much larger cloud droplets)
• The RH at which an aerosol activates is stronglyThe RH at which an aerosol activates is strongly dependent upon its size
• Larger aerosols activate first and can consume vapor, g ppreventing the smaller ones from activating
• The number of cloud droplets is strongly controlled by th b f l bl lthe number of soluble aerosols
What determines N in warm clouds?et
[c
m-3
] d
ropl
ratio
n [
Clo
udnc
entr
Cco
n
Aerosol concentration (r>0.1 micron) [cm-3]
Link between number of cloud droplets d l d lb dand cloud albedo
• Similar arguments as for light scattering due to aerosols
• For given amount of liquid water, increased N gives smaller average size of dropletsS f• Smaller droplets have larger surface area
• More reflective cloud, more albedo
• Most well-understood
l l daerosol-cloud-climate effects (indirect(effects)
Global Sulfur Emission PatternsGlobal Sulfur Emission Patterns
Chin et al. [2000]
MODIS, data courtesy of NASA
IPCC, 2007
Putting it all together