aerosol-cloud-surface flux interactions in warm cumulus clouds over land
DESCRIPTION
Aerosol-cloud-surface flux Interactions in warm cumulus clouds over land. Hongli Jiang 1 Graham Feingold 2 1 CIRA/NOAA/ESRL, Boulder, CO 2 NOAA/E SR L, Boulder, CO RICO workshop, Sept. 21, 2006. The “First Aerosol Indirect Effect”. - PowerPoint PPT PresentationTRANSCRIPT
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Aerosol-cloud-surface flux Interactions in warm cumulus clouds over land
Hongli Jiang1
Graham Feingold2
1 CIRA/NOAA/ESRL, Boulder, CO2 NOAA/ESRL, Boulder, CO
RICO workshop, Sept. 21, 2006
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The “First Aerosol Indirect Effect”
• More aerosol more drops while LWC remains constant (Twomey 1974)
The “Second Aerosol Indirect Effect”
• More aerosol more drops suppressed coalescence less rain larger LWP longer lifetime (Warner ’68, Albrecht 1989)
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Prior Work
• Local effects on clouds
– Ackerman et al. (2000)
– Johnson et al. (2004)
– Koren et al. (2004)
– Feingold et al. (2005)
Clo
ud
Fra
ctio
n
Smoke Optical Depth
Menon et al. 2002
Regional Effects:Disruption in precipitation patterns in China: Drought in north; floods in south
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2. Examine the semi-direct effect - Evaluate the importance of coupling aerosol radiative properties to microphysics, dynamics, surface soil and vegetation model
Objectives:
1. Study the second aerosol indirect effect on warm cumulus clouds over land
- Aerosol induced changes in LWP, cloud fraction, precipitation, etc….
3. Consider counteracting effects of the 2nd aerosol indirect effect and the semi-direct effect
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Incoming solar radiation
Surface sensible and latent heat fluxes
S1 Simulations: Aerosol-Cloud Interactions + Land Surface Model
balance
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Incoming solar radiation
Incoming solar radiationdiminished by aerosol
Surface sensible and latentheat fluxes reduced
Aerosolscattering &absorption
balance
S2 Simulations: Aerosol-Cloud Interactions + Aerosol Radiation +Land Surface Model
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Table 1. Description of Experiments
EXP Na , cm-3 a Aerosol Heating
S1-100 100 0.04 No
S1-500 500 0.20 No
S1-1000 1000 0.40 No
S1-2000 2000 0.80 No
S2-100 100 Yes
S2-500 500 Yes
S2-1000 1000 Yes
S2-2000 2000 Yes
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Simulation of case from Amazon SMOCC experiment
Smoke:• ωo ~ 0.9 (dry)• Optical properties calculated in 8 λ bands (SW and LW)• Effects of uptake of water vapor on size and composition • Various values of concentration Na, but constant with height
• Large Eddy Model (LES ~ x ~100m) – Resolves aerosol and drop sizes + dissolved aerosol– Resolves large eddy dynamics (rams@noaa)– Radiation model (Harrington et al., 2000)– Radiatively-active aerosol – absorbing aerosol heats atmosphere locally– Soil and vegetation model (Walko et al., 2000)
• Domain size: x=y=6.4 km; z= 5.0 km • Grid size: x=y=100 m; z=50 m• t = 2 sec
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Expected: More aerosol more drops less rain
Rain rate
Nd
Unexpected: No clear separation in LWP, cloud fraction, and cloud depth as Na increases.
Na=100
LWP
CF
Zdepth
Zbase
S1: No Aerosol Heating
100/cc
500/cc
2000/cc
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• Dynamic variability is much larger than aerosol effects on LWP, CF, cloud depth
• When raindrops are excluded in the LWP calculation, second aerosol indirect effect is simulated
S1: No Aerosol Heating: 5-h averages vs Na
Standard deviation
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rain rate
w’w’
S2: With Aerosol-Radiative Coupling
LWP
CF
Zdepth
Zbase
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S2: With Aerosol-Radiative Coupling: 5-h average vs Na
LWP
CF
Nd,int
Zdepth
τ
Tsfc
Rnet
Fsen+lat
Non-monotonic behavior
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(S2(2000)-S2(100))/S2(100), %
S2: With Aerosol-Radiative Coupling
CF
Nd,int
Zdepth
Tsfc
Rnet
Fsen+lat
LWP τ
CF
Tsfc
Nd,int Rnet
Zdepth
Fsen+lat
LWP 64%
CF 58%
Zdepth 62%
Tsfc -1.31oC
Rnet 31%
Rsw 26%
LWP
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SummaryS1 simulations (2nd indirect effect only):
• Increase in Na leads to increase in Nd, cloud optical depth decrease in reff, reduction in surface precip
• Aerosol effects on LWP, cloud fraction are small and well within the dynamical variability at a given Na
S2 simulations (2nd indirect + semi-direct effects):• The aerosol blocks up to 26 % of incoming solar
radiation from reaching the surface;• Reduced surface radiative fluxes reduction in surface
heat fluxes strong decrease in LWP, cloud fraction, cloud depth, and weaker convection;
• Possible non-monotonic response of cloud properties to increases in aerosol
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Final Comments
• Current work focused on determining the effects of poor representation of mixing in LES
– Damkohler No. = eddy/evap
(homogeneous/inhomogeneous)
– Evaporation limiters: (C. Jeffery, J. Reisner, JAS 2006)
– W. Grabowski (J. Climate 2006)
– S. Krueger: EMPM
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Aerosol Conc., cm-3
Cloud Fraction
LWP (domain ave.)
LWP (cloud ave.)
BOMEX
10 100 1000
LWP (cloud ave.)
Aerosol Conc., cm-3
500 1000 2000
SMOCC
Excluding drizzle
Note large std deviations!
Xue and Feingold 2006 Jiang and Feingold 2006