Measurements and Modeling of Black-Carbon Aerosols in the Arctic.

We have made the first continuous measurements of black carbon in Barrow, Alaska at the ARM aerosol- observing site at the NOAA Barrow Observatory using a Single-Particle Soot Photometer (SP2). These data demonstrate that BC particles are extremely small, and a majority of the particles (by number d...

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Bibliographic Details
Main Authors: Bambha, Ray, LaFranchi, Brian, Schrader, Paul E., Lucero, Daniel A., Ivey, Mark D., Michelsen, Hope A.
Language:unknown
Published: 2019
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1562413
https://www.osti.gov/biblio/1562413
https://doi.org/10.2172/1562413
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Summary:We have made the first continuous measurements of black carbon in Barrow, Alaska at the ARM aerosol- observing site at the NOAA Barrow Observatory using a Single-Particle Soot Photometer (SP2). These data demonstrate that BC particles are extremely small, and a majority of the particles (by number density) are smaller than 0.5 fg, the lower limit of reliability of the SP2. We developed the first numerical model capable of quantitatively reproducing the laser-induced incandescence (LII) and scattering signals produced by the SP2, the industry-standard BC instrument. Our model reproduces the SP2 signal temporally and spectrally and demonstrates that the current SP2 optical design allows substantial contamination of LII on the scattering signal. We ran CAM5-SE in nudged mode, i.e., by constraining the transport used in the model with meteorological data. The results demonstrate the problem observed previously of under-predicting BC at high latitudes. The cause of the discrepancy is currently unknown, but we suspect that it is associated with scavenging and rainout mechanisms.