EGU21-12251
https://doi.org/10.5194/egusphere-egu21-12251
EGU General Assembly 2021
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Survey of microphysical properties of marine boundary-layer clouds in the Western North Atlantic 

Simon Kirschler1,2, Christiane Voigt1,2, Andrew S. Ackerman3, Bruce Anderson4, Gao Chen4, Andrea F. Corral5, Ewan Crosbie4, Hossein Dadashazar5, Richard A. Ferrare4, Ann Fridlind3, Johnathan W. Hair4, Xiangyu Li6, Richard Moore4, Dominik Schollmayer1,2, Michael A. Shook4, K. Lee Thornhill4, Florian Tornow3, Halong Wang6, Luke D. Ziemba4, and Armin Sorooshian5
Simon Kirschler et al.
  • 1Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
  • 2Institut für Physik der Atmosphäre, Johannes Gutenberg-Universität, Mainz, Germany
  • 3NASA Goddard Institute for Space Studies, New York, NY, USA
  • 4NASA Langley Research Center, Hampton, VA, USA
  • 5Department of Chemical and Environmental Engeneering, University of Arizona, Tucson, Arizona, USA
  • 6Pacific Northwest National Labratory, Richland, WA, USA

Oceanic low level clouds strongly affect the atmospheric radiation budget. Uncertainties in their microphysical properties and cover currently limit the accuracy of climate predictions. Further, studies quantifying the relative importance of aerosol and dynamics on cloud properties in specific meteorological regimes are poorly constrained by observations in the Western North Atlantic boundary layer.

Low level clouds were measured during the Aerosol Cloud meTereology Interactions oVer the western ATlantic Experiment (ACTIVATE) campaign in winter and summer 2020. The two NASA LaRC research aircraft HU-25 Falcon and UC-12 B-200 King Air conducted 35 simultaneous flights to investigate aerosol-cloud interactions of maritime clouds and their impact on radiation. Number concentration, liquid water content, ice water content, and particle size distribution in the size range of 3 µm to 1460 µm in diameter were measured with the fast forward scattering cloud probe (FCDP) and 2-dimensional optical array imaging probe (2D-S) onboard the Falcon. Here, we present an overview of late winter (February-March) and late summer (August-September) oceanic cloud properties in the region 65°W to 80°W and 30°N to 40°N. We compare cloud properties in these two seasons and investigate their dependence on meteorological parameters and aerosol abundance. In a case study, we present cloud observations in a cold air outbreak event on 1 March 2020 with a specific focus on mixed-phase clouds.

How to cite: Kirschler, S., Voigt, C., Ackerman, A. S., Anderson, B., Chen, G., Corral, A. F., Crosbie, E., Dadashazar, H., Ferrare, R. A., Fridlind, A., Hair, J. W., Li, X., Moore, R., Schollmayer, D., Shook, M. A., Thornhill, K. L., Tornow, F., Wang, H., Ziemba, L. D., and Sorooshian, A.: Survey of microphysical properties of marine boundary-layer clouds in the Western North Atlantic , EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-12251, https://doi.org/10.5194/egusphere-egu21-12251, 2021.

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