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Scavenging of black carbon by ice crystals over the northern Pacific

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Field Value
Title Scavenging of black carbon by ice crystals over the northern Pacific
Names Baumgardner, D. (creator)
Subramanian, R. (creator)
Twohy, Cynthia (creator)
Stith, J. (creator)
Kok, Gregory L. (creator)
Date Issued 2008 (iso8601)
Note copyrighted by American Geophysical Union
Abstract Airborne measurements over the northern Pacific are
evaluated to characterize properties of black carbon (BC) in
cirrus crystal residuals and background aerosols in the upper
troposphere. Although the mass and number concentrations
of BC were 7–25 times lower in crystal residuals than in
particles outside of cloud, twice as many of the residuals
(31%) contained BC compared to 17% of the particles in
cloud-free air. In addition the average mass equivalent
diameter (MED) of BC was 10% larger in crystal residuals
than in particles outside of cloud. These differences in
crystal residuals compared to the background aerosols
suggest that inertial scavenging is a significant mechanism
for removing BC compared to removal by nucleation. The
scavenging efficiency, calculated as the BC mass in
condensed cloud water, ranged from 7–44 ng of carbon per
gram of water, consistent with previous studies in marine
stratus clouds.
Genre Article
Identifier Baumgardner, D, Subramanian, R., Kok, G., Twohy, C. and Stith, J., 2008, Scavenging of black carbon by ice crystals over the northern Pacific: Geophys. Res. Lett, v.35, L22815.

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