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Linking Organic Aerosol Volatility and Cloud Condensation ...

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Kate M. Cerully 1 , James R. Hite, Jr. 2 , Molly McLaughin 1,* , and Athanasios Nenes 1,2 1 Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA 2 Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 3 Currently at Coal River Mountain Watch, Naoma, WV Linking Organic Aerosol Volatility and Cloud Condensation Nuclei Activity Air & Waste Management Association Brown Bag Luncheon November 30, 2012
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Kate M. Cerully1, James R. Hite, Jr.2, Molly McLaughin1,*, and Athanasios Nenes1,2

1Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA

2Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA

3Currently at Coal River Mountain Watch, Naoma, WV

Linking Organic Aerosol Volatility and

Cloud Condensation Nuclei Activity

Air & Waste Management Association Brown Bag Luncheon

November 30, 2012

Motivation for Researching Aerosol

Direct Effect

Aerosol particles reflect and

absorb solar and infrared

radiation

Cloud Albedo Effect

Aerosols cool climate

indirectly through the

changes they cause in cloud

properties

Figure: IPCC, 2007

2

Organic Aerosol Volatility

3

Solar Radiation

Organic Aerosol (OA) in µg m-3

0 1 2 3 4

Plots: Robinson et al., 2007

Aerosol-Cloud-Climate Interactions

Clean Environment

CCN

Lower Albedo

(few Cloud Condenstion Nuclei)Polluted Environment

(many Cloud Condensation Nuclei)

Higher Albedo

CCN

4

Organic Aerosol Complexities

5

0.75”

Wire Mesh

Fiberglass Insulation

Thermistor

Heating Tape

Activated Carbon

Heating Section Cooling Section

Measuring Volatility - Thermodenuder

6

30” 30”

Volatilized

Mass Distance

Temperature

Particle Size

Measuring Cloud Condensation Nuclei (CCN)

7

Outlet: Droplets = CCN

Inlet: Aerosols Design

� Cylindrical column

� Temperature gradient along

the wall

� Wall saturated with H2O

Principle

� H2O diffuses faster than

heat in air

� Creates a supersaturation

at the centerline

0

1

2

3

4

5

6

7

8

9

10

-2 -1 0 1 2 3 4 5

Organic Mass Conc (ug m

-3)

Log10 Saturation Concentration* (ug m-3)

Implications and Future Directions

� Use volatility basis set approach*

to provide a picture of organic

aerosol phase partitioning

behavior into unique bins

� Along with CCN properties, these

basis sets will be measured

across the globe to constrain

inputs to global climate models

8

= condensed phase

� Reduce the uncertainty in global climate predictions

� Better understand and define the impacts of personal and industrial

activities on local and global environments

*Donahue et al., 2006

Thank you!

Acknowledgments: NASA, NSF CAREER, Air Products Undergraduate Research Grant, UROP

2010 Materials and Supplies Grant, Rodney Weber, Dave Tanner, and Greg Huey


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