timothy logan university of north dakota department of atmospheric science

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Timothy Logan Timothy Logan University of North Dakota University of North Dakota Department of Atmospheric Science Department of Atmospheric Science

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Page 1: Timothy Logan University of North Dakota Department of Atmospheric Science

Timothy LoganTimothy Logan

University of North DakotaUniversity of North Dakota

Department of Atmospheric ScienceDepartment of Atmospheric Science

Page 2: Timothy Logan University of North Dakota Department of Atmospheric Science

Outline Aerosol Characteristics

Formation and Behavior Aerosol Detection and Transport

Asian aerosol eventsPast research findings

Aerosol ClassificationCurrent researchSeasonal variability

Research ApplicationsPrimary tools and methodsMain goals and applications

Page 3: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Characteristics

http://www.sciencenews.org/view/feature/id/65734/title/The_final_climate_frontiers NASA Terra Image 20 Mar 2011

Anthropogenic Aerosols Natural Aerosols

Page 4: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Detection Size and composition of aerosols

Attenuation of EM radiation illustrates the nature of aerosols○ Aerosol optical depth (AOD)

Aerosol attenuation (extinction) is the sum of the aerosol scattering and absorption of light○ Extinction part – correlated with size○ Absorption part – correlated with composition

Recent studies looking into thisMain focus of current research

Page 5: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Detection

My past researchUsed dependence of extinction AOD over a

wavelength interval (Angstrom exponent or )○ Distinguishes between small and large aerosols

Fine mode vs. coarse mode aerosols

○ Does not distinguish aerosol compositionSome pollution aerosols can disguise themselves as large size

natural aerosols

Detected Asian aerosol events capable of transporting large amounts of dust and pollution via the Pacific Ocean to North America○ Primarily used aerosol size as a proxy

Page 6: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Transport

AOD > 0.2

AOD > 0.4

AOD > 0.6

Aerosol Transport TrendAerosol Optical Depth

Frequency of Occurrence

Major Aerosol Regions

MODIS AOD Retrievals

Page 7: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Classification

Current research uses second derivative of the absorption part of AOD Spectral curvature or absslope of absDevelop a classification scheme that reduces

ambiguities in Asian aerosol compositionPreliminary results show a clustering of

different types of aerosols○ Sulfate, biomass, mineral dust, black carbon○ Can also see a seasonal variability and rate of

change of Asian aerosol composition

Page 8: Timothy Logan University of North Dakota Department of Atmospheric Science

Desert Regions

Clean Region

Urban Region

2008 AERONET Derived Aerosol Seasonal Variability

Discussion (Absorption)• Most mean abs values for the two seasons fall between 1 and 2 (red lines)

• Mean abs (blue line) explains seasonal variance

• Summer – mean abs is slightly negative

• Sulfate and/or other scattering aerosols

• Winter – mean abs is much higher

• Indicating strong absorption• Result of coal and wood combustion for heat

Xianghe, China 39N 117E

Page 9: Timothy Logan University of North Dakota Department of Atmospheric Science

Research Applications

My research both past and present relies heavily on in situ AERONET, aircraft, space based, and re-analysis observations.NASA sponsored/maintained platforms

Main goal of research is to classify aerosols and the variability of their compositions as they transport far away from their source regions Determine their effects on climate change and

human health

Page 10: Timothy Logan University of North Dakota Department of Atmospheric Science

Thank You

Page 11: Timothy Logan University of North Dakota Department of Atmospheric Science

Extra Slides

Page 12: Timothy Logan University of North Dakota Department of Atmospheric Science

Aerosol Characteristics

Aerosol formationClassified as either man-made (anthropogenic) or

natural

Aerosol behaviorIn terms of climate change – direct vs. indirect effect

○ Influence solar radiation vs. cloud physical propertiesEffects are influenced by physical and chemical

properties of aerosols○ Radiative properties, size and chemical structure

Page 13: Timothy Logan University of North Dakota Department of Atmospheric Science