Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning...

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Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric Sciences April 7, 2014

Transcript of Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning...

Page 1: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

Atmospheric Aerosols in Amazonia and land use change: from natural

biogenic to biomass burning conditions

Keith HeidecornGraduate Seminar in Atmospheric Sciences

April 7, 2014

Page 2: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

1. Learn Something New2. Observe the Effect of the Dry & Wet Season on Land Types3. Gain Insight into how Aerosols Effect more than just the Atmosphere

Goals

Page 3: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

Aerosol Optical DepthBlack CarbonSingle Scattering AlbedoNet Ecosystem Exchange (NEE)

Definitions

Page 4: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.
Page 5: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.
Page 6: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.
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TT34 (Central Amazon)

PVH (Southern Amazon)

Page 8: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

Wet Season is from January to JuneDry Season is from July to DecemberWhich Season would you expect more Land

Use Change?

Wet vs. Dry Season

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Deforestation

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Instrumentation

TSI-3080 SMPS TSI CPC MODEL 3010

MODIS SATELLITE

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Mass Concentrations of the Sites

Why?

Page 12: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

Black Carbon

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Median Aerosol Number Size Distributions

DOES SIZE MATTER?

YES

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Submicron Non Refractory Aerosol Composition

PVH SITE TT34 SITEWHY DIFFERENT?

Page 15: Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric.

Median Scattering & Absorption Coefficients

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550 nm

637 nm

637 nm

WET DRY

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Aerosol Optical Depths (AOD)

ARE THE PEAKS DURING THE DRY OR WET SEASON?DR

Y

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Monthly Ozone

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Daily Ozone

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Carbon Monoxide

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Net Ecosystem Exchange (NEE)

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https://www.youtube.com/watch?v=mLNTJYXl9Fg

Drought of 2010

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Complexity of the ProblemLand Use Change has Altered Multiple

Systems Insights from an Interdisciplinary Approach

What Have We Learned

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Why Should We Care?

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“It is difficult to get a man to understand something, when his salary depends upon his not understanding it!” –Upton Sinclair

Questions?

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Aerosol Size Distributions

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TT34

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PVH

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Artaxo, P., L. V. Rizzo, J. F. Brito, H. M. J. Barbosa, A. Arana, E. T. Sena, G. G. Cirino, W. Bastos, S. T. Martin, and M. O. Andreae, 2013, Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions: Faraday Discussions, v. 165, p. 203-235.

“Africa.” Map. Google Earth. Google, 05 April 2014. Web. 05 April 2014. Chambers, Jeffrey. "Jeffrey Chambers' Lab Page." Jeffrey Chambers' Lab Page. N.p.,

n.d. Web. 04 Apr. 2014. "The Water Cycle : Feature Articles." The Water Cycle : Feature Articles. NASA Earth

Observatory, n.d. Web. 05 Apr. 2014. "United Kingdom Chemistry and Aerosols (UKCA) Model." Met Office. N.p., n.d. Web.

06 Apr. 2014.

References