Recommendations for Interpretation of "Black Carbon" Measurements John A. Ogren Chairman, WMO/GAW Scientific Advisory Group for Aerosols National Oceanic.

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Recommendations for Interpretation of "Black Carbon" Measurements John A. Ogren Chairman, WMO/GAW Scientific Advisory Group for Aerosols National Oceanic and Atmospheric Administration Earth System Research Laboratory Global Monitoring Division Boulder, Colorado, USA

GAW SAG-Aerosol Members John Ogren (Chairman), Urs Baltensperger, Angela Benedetti, Markus Fiebig, Thomas Holzer-Popp, Stefan Kinne, Paolo Laj, Shao-Meng Li, Gelsomina Pappalardo, Andreas Petzold, Nobuo Sugimoto, Christoph Wehrli, Alfred Wiedensohler, Xiao-Ye Zhang Manuscript under discussion at discuss.net/13/9485/2013/acpd html J. Ogren Global Monitoring Annual Conference2

What are the Issues? Black carbon (BC) has important effects on climate and health Recently identified as #2 most important climate forcing agent (+1.1 W m -2, 90% bounds to +2.1 W m -2, Bond et al., 2013). Associated with asthma and other respiratory problems, heart attacks and lung cancer. BC is poorly defined in the scientific literature Carbonaceous matter does not appear in atmospheric aerosols as a pure substance. Measurements may refer to the same quantity with different names, or to different quantities with the same name. BC measurements depend on the method used Current methods respond to different properties of BC. Correlations between methods are frequently high, but relationships vary among sites, seasons and aerosol types. J. Ogren Global Monitoring Annual Conference3

Delhaye, 2009 Ogren & Charlson 1983 What is Black Carbon? Nanometer scale  Meter scale Soto, 2008 J. Ogren Global Monitoring Annual Conference4

What is Black Carbon? Defined by five essential characteristics –Composition –Morphology –Volatility –Solubility –Light absorption J. Ogren Global Monitoring Annual Conference5

PropertyCharacteristicsConsequences Composition graphitic-like structure containing a high fraction of sp 2 -bonded carbon atoms low chemical reactivity in the atmosphere; slow removal by chemical processes; strong optical absorption Morphology aggregates consisting of small carbon spherules, each typically nm diameter high specific surface area; high capacity for sorption of other species Volatilityrefractory material with a volatilization temperature near 4000K; gasification is possible only by oxidation at T > 340°C high stability in the atmo- sphere; longer atmospheric residence time J. Ogren Global Monitoring Annual Conference6

PropertyCharacteristicsConsequences Solubility insoluble in water, in organic solvents including methanol and acetone, and in the other components of the atmospheric aerosol Slow removal by clouds and precipitation, unless coated with water-soluble compounds; longer atmospheric residence time Light absorptionuniformly absorbing in the spectral range of visible light; characterized by a significant, non-zero and wavelength- independent imaginary part of the refractive index over VIS and NIR spectral regions Reduction of the albedo of clouds, snow, and ice; atmospheric heating; surface cooling – all of which lead to effects on solar radiation and climate J. Ogren Global Monitoring Annual Conference7

“BC” Measurement Methods Evolved Carbon  CO 2 evolved from thermal or thermo- optical methods: IMPROVE / EUSAAR  BC properties: composition, volatility Light Absorption  Filter-based: Aethalometer, PSAP, MAAP, COSMOS  In situ: photo-acoustic, ext. minus scat.  BC properties: light absorption Laser Incandescence  Laser heating of particles, e.g., SP2, LII  BC Properties: volatility, composition J. Ogren Global Monitoring Annual Conference8

Aerosol Mass Spectrometry  Vaporization and detection of carbon ion clusters in mass spectra: ATOFMS, SP-AMS  BC properties: composition Raman Spectrometry  Detection of graphite-like ordered and disordered carbon  BC properties: composition Electron microscopy  Detection of particle microstructure and morphology, e.g. TEM  BC properties: morphology Onasch et al., AS&T 2012 Ivleva et al., AS&T 2007 Delhaye, 2009 “BC” Measurement Methods J. Ogren Global Monitoring Annual Conference9

Recommended Terminology No current method combines all five essential characteristics of BC Consequently, no current method can justifiably claim to provide a quantitative measurement of BC Recommendations –Use “BC” as a qualitative term referring to any of the quantitative methods –Use terms associated with the measurement methods when reporting quantitative results J. Ogren Global Monitoring Annual Conference10

Equivalent black carbon (EBC) should be used instead of black carbon for data derived from optical absorption methods. It is recommended to report the optical measurements primarily as light absorption coefficient, and secondarily as EBC, together with a suitable mass absorption coefficient for the conversion of light absorption coefficient into mass concentration. Refractory black carbon (rBC) should be used instead of black carbon for measurements derived from incandescence methods. Elemental carbon (EC) should be used instead of black carbon for data derived from methods that are specific to the carbon content of carbonaceous matter (evolved carbon, aerosol mass spectrometry, Raman spectroscopy). Recommended Terminology J. Ogren Global Monitoring Annual Conference11

Recommended Terminology Equivalent black carbon (EBC) –Data derived from optical absorption methods. –Report the optical measurements primarily as light absorption coefficient, and secondarily as EBC, along with the mass absorption efficiency used to convert absorption to EBC. Refractory black carbon (rBC) –Data derived from incandescence methods. Elemental carbon (EC) –Data derived from methods that are specific to the carbon content of carbonaceous matter (evolved carbon, aerosol mass spectrometry, Raman spectroscopy). J. Ogren Global Monitoring Annual Conference12

Blind Men and the Elephant J. Ogren Global Monitoring Annual Conference13

Interpreting “BC” Measurements J. Ogren Global Monitoring Annual Conference14