The Arctic Low-Level Mixed-Phase Haze Regime and its Microphysical Differences to Mixed-Phase Clouds
Manuel Moser (Deutsches Zentrum für Luft- und Raumfahrt (DLR))
Christiane Voigt (Deutsches Zentrum für Luft- und Raumfahrt (DLR), University of Mainz)
Oliver Eppers (Max Planck Institute of Chemistry)
Johannes Lucke (Deutsches Zentrum für Luft- und Raumfahrt (DLR), Rail Tec Arsenal, TU Delft - Aerospace Engineering)
Elena De La Torre Castro (Deutsches Zentrum für Luft- und Raumfahrt (DLR))
Hans Christian Clemen (Max Planck Institute of Chemistry)
Johannes Schneider (Max Planck Institute of Chemistry)
André Ehrlich (University of Leipzig)
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Abstract
A comprehensive in-situ dataset of low-level Arctic clouds was collected in the Fram Strait during the HALO-(AC)3 campaign in spring 2022 using the research aircraft Polar 6. The clouds observed at altitudes below 1000 m were frequently in a mixed-phase state. We demonstrate that despite comparable optical properties, classic mixed-phase clouds (MPC) and mixed-phase haze (MPH) can be distinguished on the basis of their microphysical properties, with MPH observed about 8 times more frequently than MPC. While the thermodynamic phases of the particles within the MPH are similar to those in the MPC, the supercooled droplets observed in MPC are replaced by large (> 3 µm) wet aerosol particles in MPH. Furthermore, the particle number concentration measured in MPH is reduced by approximately 3 orders of magnitude compared to MPC. MPH is observed in subsaturated air with respect to water, suggesting that the small liquid particles are haze droplets and are in equilibrium below the activation threshold to form cloud droplets. Chemical analysis suggested that the haze particles contained significant amounts of sea salt. Additional in-situ measurements with an optical particle counter indicated that their number concentration was 2 times larger over the sea ice compared to the open ocean. Furthermore, measurements of the vertical distribution of the thermodynamic phases in low-level Arctic clouds revealed a characteristic structure, with a liquid regime frequently occurring at the top of the atmospheric boundary layer, followed by MPCs, and an MPH layer below. The findings from this study enhance our understanding of the microphysical composition of clouds in mixed-phase conditions.
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