MOSAiC studies of long-lasting mixed-phase cloud events and analysis of the liquid-phase properties of Arctic clouds

Journal Article · Mon Oct 20 00:00:00 EDT 2025 · Atmospheric Chemistry and Physics (Online)

DOI:https://doi.org/10.5194/acp-25-12955-2025· OSTI ID:2999984

Jimenez, Cristofer ^[1]; Ansmann, Albert ^[1]; Ohneiser, Kevin ^[1]; Griesche, Hannes ^[1]; Engelmann, Ronny ^[1]; Radenz, Martin ^[1]; Hofer, Julian ^[1]; Althausen, Dietrich ^[1]; Knopf, Daniel A. ^[2]; Dahlke, Sandro ^[3]; Bühl, Johannes ^[4]; Baars, Holger ^[1]; Seifert, Patric ^[1]; Wandinger, Ulla ^[1]

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1. Leibniz Inst. for Tropospheric Research (ITR), Leipzig (Germany)
2. Stony Brook Univ., NY (United States)
3. Alfred Wegener Inst. for Polar and Marine Research, Potsdam (Germany)
4. Leibniz Inst. for Tropospheric Research (ITR), Leipzig (Germany); Harz Univ. of Applied Sciences (Germany)

Vertically resolved observations of the temporal evolution of mixed-phase clouds (MPCs) were performed over the central Arctic during the MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) expedition, which lasted from October 2019 to September 2020. The research icebreaker Polarstern, drifting with the pack ice for more than 7 months, mostly at latitudes > 85° N, served as a platform for state-of-the-art remote sensing of aerosols and clouds. The use of the recently introduced dual field-of-view (FOV) polarization lidar technique in combination with the well-established lidar-radar retrieval technique provided, for the first time, a robust instrumental basis to monitor the evolution of the liquid and the ice phase of MPCs and the interplay between the two phases. Two long-lasting Arctic MPC events observed close to the North Pole in mid-winter (December 2019) and late summer (September 2020) are discussed to provide new insight into Arctic MPC evolution processes. In the second part of the article, cloud statistics, covering all seasons of a year, are presented. The focus is on the optical and microphysical properties of the liquid phase. These results are solely derived from the dual-FOV lidar observations. The key findings of the study can be summarized as follows: persistent activation of aerosol particles to form water droplets is of great importance for the longevity of MPCs. The observations confirm that ice formation occurs predominantly via immersion freezing. The field studies suggest that the free tropospheric reservoirs of cloud condensation nuclei (CCN) and of ice-nucleating particles (INPs) were always well filled, i.e., the clouds did not exhaust their supply of activatable and activated particles. The observation of long-lasting MPC events, low ice production rates, and a sufficiently large INP reservoir leads to the recommendation to use a time-dependent immersion freezing parameterization in MPC modeling efforts.

• Research Organization: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Atmospheric Radiation Measurement (ARM) Archive
• Sponsoring Organization: USDOE Office of Science (SC), Biological and Environmental Research (BER)
• Contributing Organization: Pacific Northwest National Laboratory (PNNL); Argonne National Laboratory (ANL); Brookhaven National Laboratory (BNL)
• Grant/Contract Number: SC0021034
• OSTI ID: 2999984
• Journal Information: Atmospheric Chemistry and Physics (Online), Journal Name: Atmospheric Chemistry and Physics (Online) Journal Issue: 20 Vol. 25; ISSN 1680-7324
• Publisher: Copernicus Publications, EGU
• Country of Publication: United States
• Language: English