Airborne investigation of black carbon interaction with low-level, persistent, mixed-phase clouds in the Arctic summer ...

Aerosol–cloud interaction is considered one of the largest sources of uncertainty in radiative forcing estimations. To better understand the role of black carbon (BC) aerosol as a cloud nucleus and the impact of clouds on its vertical distribution in the Arctic, we report airborne in situ measuremen...

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Bibliographic Details
Main Authors: Zanatta, Marco, Mertes, Stephan, Jourdan, Olivier, Dupuy, Regis, Järvinen, Emma, Schnaiter, Martin, Eppers, Oliver, Schneider, Johannes, Jurányi, Zsófia, Herber, Andreas
Format: Text
Language:English
Published: European Geosciences Union (EGU) 2023
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Online Access:https://dx.doi.org/10.5445/ir/1000162188
https://publikationen.bibliothek.kit.edu/1000162188
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Summary:Aerosol–cloud interaction is considered one of the largest sources of uncertainty in radiative forcing estimations. To better understand the role of black carbon (BC) aerosol as a cloud nucleus and the impact of clouds on its vertical distribution in the Arctic, we report airborne in situ measurements of BC particles in the European Arctic near Svalbard during the “Arctic CLoud Observations Using airborne measurements during polar Day” (ACLOUD) campaign held in the summer of 2017. BC was measured with a single-particle soot photometer aboard the Polar 6 research aircraft from the lowest atmospheric layer up to approximately 3500 m a.s.l (metres above sea level). During in-cloud flight transects, BC particles contained in liquid droplets (BC residuals) were sampled through a counterflow virtual impactor (CVI) inlet. Four flights, conducted in the presence of low-level, surface-coupled, inside-inversion, and mixed-phase clouds over sea ice, were selected to address the variability in BC above, below, and ...