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[object Object],[object Object],Intercontinental Aerosol Transport: Quantitative Tools an Results ?? July
Global Aerosol Pattern – NASA MISR Team ,[object Object],[object Object],[object Object]
Regional Haze Rule: Glide Path Toward ‘Natural Condition’ Natural haze  is due to natural windblown dust, biomass smoke and other natural processes  Man-made  haze is due industrial activities  AND man-perturbed smoke and dust emissions (A fraction of the man-perturbed smoke and dust is assigned to natural by policy decisions)
Origin of Fine Dust Events over the US Gobi dust in spring Sahara in summer US-scale fine dust events are mainly from intercontinental transport Fine Dust Events, 1992-2003 ug/m3
Observational Tools Establishing Aerosol Origin ( Egen, 1835) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Direct Evidence Spatial Pattern Wind Pattern Composition Temporal Pattern Trajectory
 
 
 
Sahara and Local Dust Apportionment: Annual and July • The maximum annual Sahara dust  contribution is about 1   g.m 3 • In Florida, the local and Sahara dust  contributions are about equal but at Big  Bend, the Sahara contribution is < 25%.  The Sahara and Local dust was apportioned based on their respect ive Al/Si ratios.  • In July the Sahara dust contributions are 4 - 8   g.m 3 • Throughout the Southeast, the Sahara dust  exceeds the local source contributions by  w wide margin (factor of 2 - 4) Annual July
Temporal Scales of Aerosol Events ,[object Object],[object Object],[object Object],[object Object],[object Object]
Dust ,[object Object],[object Object],[object Object],[object Object],US West East
Example high fine dust days ( See console for complete list ) Asian Dust April 16, 2001 Sahara Dust July 5, 2001 Southwestern Dust Oct. 16, 2001
Dust ,[object Object],[object Object],[object Object],[object Object],US West Western US - Dust Western US - Sulfate ,[object Object],[object Object],[object Object],Sulfate
Seasonal Pattern of Dust Baseline and Events ,[object Object],[object Object],[object Object]
Temporal Signal Decomposition and Event Detection ,[object Object],[object Object],EUS Daily Average 50%-ile, 30 day 50%-ile smoothing Deviation from %-ile Event : Deviation > x*percentile Average Median ,[object Object]
TOMS and VIEWS, July ,[object Object]
Sahara Dust Impact Events AIRS PM10 Concentration
Seasonal Average Fine Soil  (VIEWS database, 1992-2002) ,[object Object],[object Object],[object Object]
Combined Aerosol-Trajectory Tool (CATT) ,[object Object],[object Object]
Eastern US PM25 Event Composition ,[object Object],[object Object],[object Object]
Summary of Quantification Techniques ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Analyst Consoles : Near-Real-Time Data   Example:  NE Sulfate Episode: 8/27/04 17:00UTC Sulfate in the Northeast Sahara Dust in the Gulf Fires in the Southeast Time Series Console: Southeast
Aerosol Event Catalog :  Distributed Web pages ,[object Object],[object Object],[object Object],[object Object],[object Object],Browser Links to Distributed Analyst/Data Web page
Start with Kitty:   http:// webapps . datafed .net/ dvoy _services/ datafed . aspx ?view=Kitty Kitty DataFed.net  Large Collection of Projects, Data, Tools. Where’s CATT “Start”?
Aerosol Event Catalog: Web pages ,[object Object],[object Object]

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2006-03-08 Intercontinental Aerosol Transport: Quantitative Tools an Results

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  • 3. Regional Haze Rule: Glide Path Toward ‘Natural Condition’ Natural haze is due to natural windblown dust, biomass smoke and other natural processes Man-made haze is due industrial activities AND man-perturbed smoke and dust emissions (A fraction of the man-perturbed smoke and dust is assigned to natural by policy decisions)
  • 4. Origin of Fine Dust Events over the US Gobi dust in spring Sahara in summer US-scale fine dust events are mainly from intercontinental transport Fine Dust Events, 1992-2003 ug/m3
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  • 9. Sahara and Local Dust Apportionment: Annual and July • The maximum annual Sahara dust contribution is about 1  g.m 3 • In Florida, the local and Sahara dust contributions are about equal but at Big Bend, the Sahara contribution is < 25%. The Sahara and Local dust was apportioned based on their respect ive Al/Si ratios. • In July the Sahara dust contributions are 4 - 8  g.m 3 • Throughout the Southeast, the Sahara dust exceeds the local source contributions by w wide margin (factor of 2 - 4) Annual July
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  • 12. Example high fine dust days ( See console for complete list ) Asian Dust April 16, 2001 Sahara Dust July 5, 2001 Southwestern Dust Oct. 16, 2001
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  • 17. Sahara Dust Impact Events AIRS PM10 Concentration
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  • 22. Analyst Consoles : Near-Real-Time Data Example: NE Sulfate Episode: 8/27/04 17:00UTC Sulfate in the Northeast Sahara Dust in the Gulf Fires in the Southeast Time Series Console: Southeast
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  • 24. Start with Kitty: http:// webapps . datafed .net/ dvoy _services/ datafed . aspx ?view=Kitty Kitty DataFed.net Large Collection of Projects, Data, Tools. Where’s CATT “Start”?
  • 25.