E03: Process-level assessments of Arctic mixed-phase clouds
PIs: Vera Schemann, Sabrina Schnitt (former PIs: Stefan Kneifel, Roel Neggers, Yaping Shao, Ulrich Löhnert)
The occurrence, persistence, and dissolution of Arctic mixed-phase clouds (MPC) are important factors to describe relevant processes for Arctic amplification and to understand the evolution of the Arctic system under global warming. During phase II, the observational capabilities at the Arctic research station AWIPEV in Ny-Ålesund (NYA) were extended by installing a new polarimetric Ka-band radar. The dual-frequency Ka-W-band radar measurements revealed new insights into ice microphysical and precipitation formation processes. Alongside, a unique semi-operational ICON simulation testbed was established for NYA. So far, approximately 2.5 years of cloud- resolving simulations have been performed by starting a simulation with 600m resolution every day based on operational weather forecast forcing. The corresponding statistical analysis showed a good agreement with observations, but revealed also model uncertainties and open questions. In phase III, we will combine simulations with measurements from ground-based, and previous as well as upcoming campaigns to investigate how MPC properties are influenced by large-scale forcing and surroundings as well as by the micro-scale. One focus will be on the differences caused by surface properties – like open ocean and sea-ice – and the island effect around Svalbard. We suspect the model performance to depend on the synoptic situation, which can be characterized by circulation weather types. Another open question is the sensitivity of MPC on local circumstances and especially on known uncertainties in number of Cloud Condensation Nuclei (CCN) and Ice Nucleating Particles (INP). To understand these dependencies, we will benchmark the model by CCN and INP measurements from phase I and II. The analysis on the micro-scale will be complemented by investigating the uncertainties connected to the moisture availability and in-cloud water phase distribution for formation and persistence of MPC. In order to evaluate the model, triple-frequency radar observations in combination with the Differential Absorption Radar technique are envisioned to gain a unique characterization of MPC and corresponding hydrometeor distributions.
Hypothesis:
The representation of Arctic mixed-phase clouds at Ny-Ålesund is on the smallscale strongly dependent on local effects, but on the large-scale representative for a larger area.
Central research question which directly follow from our hypothesis are:
- How comparable are modeled and observed MPC properties at NYA to the surroundings including other surface types?
- How strongly does the model performance depend on the circulation weather type? And why?
- How important are the modeled representation of CCN/INP, water phase transitions and moisture supply for the persistence and dissolution of low-level MPC?
Arctic MPC and their contribution to atmospheric feedback processes are one important phenomenon responsible for Arctic amplification. Nevertheless, the strength of this contribution, its representation in current climate projections, and the sensitivity on necessary simplifications and assumptions is still under debate, which requires further observational evidence for model evaluation. The process understanding created within this project will support the interpretation of the contribution of Arctic MPC to Arctic amplification (SQ1). Especially the evolution of Arctic MPC in continued warming trends and the related changes in water phase transition and precipitation formation will strongly influence the future of the Arctic climate system (SQ3).
Achievements phase II
- Continuous multi-frequency and polarimetric radar measurements at NYA to advance understanding and modeling of precipitation-forming microphysical processes
- Semi-operational ICON-LEM simulations (600 m) every day, covering more than 2.5 years
- Statistical assessment of simulations and observations showed lack of liquid water in simulated clouds and a need for detailed analysis of water phase transitions
Achievements phase I
E03 has characterised persisting low-level, mixed-phase clouds in an Arctic environment, including complex orography and high synoptic variability (Ny-Ålesund) by means of a novel, combined radar/radiometer system (Küchler et al., 2017). Idealised, ultra-highly resolved (up to 3 m) LES of mixed-phase clouds over sea ice and respective sensitivity studies concerning model resolution and surface patterns were performed. An innovative, nested ICON-LEM modelling framework for the simulation of Arctic mixed-phase clouds over a complex terrain on the 100 m-scale combined with a consistent radar forward operator was developed. It was shown that large-scale subsidence acts as a remote control on ABL deepening with the potential to cloud base collapse and driving into a cloud-free state.
Role within (AC)³
Members
Tracy Kiszler
PhD
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Dr. Vera Schemann
Principal Investigator
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Dr. Sabrina Schnitt
Principal Investigator
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Prof. Dr. Roel Neggers
Principal Investigator
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Dr. Giovanni Chellini
PhD (in phase II)
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Former Members
Prof. Dr. Yaping Shao
Principal Investigator
University of Cologne
Insitute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Dr. Ulrich Löhnert
Principal Investigator
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Dr. Stefan Kneifel
Principal Investigator
phone:
e-mail:
Dr. Rosa Gierens
Postdoc (in phase II)
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
phone:
e-mail:
Dr. Robert Rauterkus
PhD (in phase I)
University of Cologne
Institute for Geophysics and Meteorology (IGM)
Pohligstr. 3
50969 Cologne
Publications
2024
Chellini, G., 2024: Precipitation formation in low-level mixed-phase clouds: determining relevant processes and drivers based on cloud radar observations from a high Arctic site, Dissertation, Universität zu Köln, https://kups.ub.uni-koeln.de/72320/
2023
Chellini, G. and Gierens, R. and Ebell, K. and Kiszler, T. and Krobot, P. and Myagkov, A. and Schemann, V. and Kneifel, S., 2023, Low-level mixed-phase clouds at the high Arctic site of Ny-Ålesund: A comprehensive long-term dataset of remote sensing observations, Earth Syst. Sci. Data, 15, 5427–5448, https://doi.org/10.5194/essd-15-5427-2023
Schnitt, S.; Mech, M.; Rose, T. & Crewell, S., 2023: Ground- and ship-based microwave radiometer measurements during the EUREC4A campaign, Earth Syst. Sci. Data, https://doi.org/10.5194/essd-2023-140, [preprint], accepted
Kiszler, T.; Ebell, K. & Schemann, V., 2023: A Performance Baseline for the Representation of Clouds and Humidity in Cloud-Resolving ICON-LEM Simulations in the Arctic, J. Adv. Model. Earth Syst., e2022MS003299, https://doi.org/10.1029/2022MS003299
Wendisch, M.; Brückner, M.; Crewell, S.; Ehrlich, A.; Notholt, J.; Lüpkes, C.; Macke, A.; Burrows, J. P.; Rinke, A.; Quaas, J.; Maturilli, M.; Schemann, V.; Shupe, M. D.; Akansu, E. F.; Barrientos-Velasco, C.; Bärfuss, K.; Blechschmidt, A.-M.; Block, K.; Bougoudis, I.; Bozem, H.; Böckmann, C.; Bracher, A.; Bresson, H.; Bretschneider, L.; Buschmann, M.; Chechin, D. G.; Chylik, J.; Dahlke, S.; Deneke, H.; Dethloff, K.; Donth, T.; Dorn, W.; Dupuy, R.; Ebell, K.; Egerer, U.; Engelmann, R.; Eppers, O.; Gerdes, R.; Gierens, R.; Gorodetskaya, I. V.; Gottschalk, M.; Griesche, H.; Gryanik, V. M.; Handorf, D.; Harm-Altstädter, B.; Hartmann, J.; Hartmann, M.; Heinold, B.; Herber, A.; Herrmann, H.; Heygster, G.; Höschel, I.; Hofmann, Z.; Hölemann, J.; Hünerbein, A.; Jafariserajehlou, S.; Jäkel, E.; Jacobi, C.; Janout, M.; Jansen, F.; Jourdan, O.; Jurányi, Z.; Kalesse-Los, H.; Kanzow, T.; Käthner, R.; Kliesch, L. L.; Klingebiel, M.; Knudsen, E. M.; Kovács, T.; Körtke, W.; Krampe, D.; Kretzschmar, J.; Kreyling, D.; Kulla, B.; Kunkel, D.; Lampert, A.; Lauer, M.; Lelli, L.; von Lerber, A.; Linke, O.; Löhnert, U.; Lonardi, M.; Losa, S. N.; Losch, M.; Maahn, M.; Mech, M.; Mei, L.; Mertes, S.; Metzner, E.; Mewes, D.; Michaelis, J.; Mioche, G.; Moser, M.; Nakoudi, K.; Neggers, R.; Neuber, R.; Nomokonova, T.; Oelker, J.; Papakonstantinou-Presvelou, I.; Pätzold, F.; Pefanis, V.; Pohl, C.; van Pinxteren, M.; Radovan, A.; Rhein, M.; Rex, M.; Richter, A.; Risse, N.; Ritter, C.; Rostosky, P.; Rozanov, V. V.; Donoso, E. R.; Saavedra-Garfias, P.; Salzmann, M.; Schacht, J.; Schäfer, M.; Schneider, J.; Schnierstein, N.; Seifert, P.; Seo, S.; Siebert, H.; Soppa, M. A.; Spreen, G.; Stachlewska, I. S.; Stapf, J.; Stratmann, F.; Tegen, I.; Viceto, C.; Voigt, C.; Vountas, M.; Walbröl, A.; Walter, M.; Wehner, B.; Wex, H.; Willmes, S.; Zanatta, M. & Zeppenfeld, S., 2023: Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC)³ Project, Bull. Am. Meteorol. Soc., American Meteorological Society, 104, E208–E242, https://doi.org/10.1175/bams-d-21-0218.1
2022
Pasquier, J. T., Henneberger, J., Ramelli, F., Lauber, A., David, R. O., Wieder, J., Carlsen, T., Gierens, R., Maturilli, M., and Lohmann, U., 2022: Conditions favorable for secondary ice production in Arctic mixed-phase clouds, Atmos. Chem. Phys., 22, 15579–15601, https://doi.org/10.5194/acp-22-15579-2022.
Chellini, G.; Gierens, R. & Kneifel, S., 2022: Ice Aggregation in Low-Level Mixed-Phase Clouds at a High Arctic Site: Enhanced by Dendritic Growth and Absent Close to the Melting Level, J. Geophys. Res. Atmos., 127, e2022JD036860, https://doi.org/10.1029/2022JD036860
2021
Rauterkus, R., 2021: Large-Eddy Simulations of Arctic Stratocumulus – Process Representation and Surface Heterogeneity, Dissertation, Universität zu Köln, http://kups.ub.uni-koeln.de/id/eprint/53928.
2020
Rauterkus, R., and Ansorge, C., 2020: Cloud-Top Entrainment in Mixed-Phase Stratocumulus and Its Process-Level Representation in Large-Eddy Simulation, J. Atmos. Sci., 77(12), 4109-4127. https://doi.org/10.1175/JAS-D-19-0221.1.
Gierens, R., 2020: Observations of Arctic low-level mixed-phase clouds at Ny-Ålesund: Characterization and insights gained by high-resolution Doppler radar, Universität zu Köln, http://kups.ub.uni-koeln.de/id/eprint/53900.
Gierens, R., S. Kneifel, M.D. Shupe, K. Ebell, M. Maturilli, and U. Löhnert, 2020: Low-level mixed-phase clouds in a complex Arctic environment, Atmos. Chem. Phys., 20, 3459-3481, doi:10.5194/acp-20-3459-2020
Karrer, M., Seifert, A., Siewert, C., Ori, D., von Lerber, A., & Kneifel, S., 2020. Ice particle properties inferred from aggregation modelling. J. Adv. Mod. Earth Sys., 12, e2020MS002066. https://doi.org/10.1029/2020MS002066
Schemann, V. and K. Ebell, 2020: Simulations of mixed-phase clouds with the ICON-LEM in the complex Arctic environment around Ny–Ålesund, Atmos. Chem. Phys., 20, 475–485, https://doi.org/10.5194/acp-20-475-2020
2019
2018
Leinonen, J., S. Kneifel, and R.J. Hogan, 2018: Evaluation of the Rayleigh–Gans Approximation for Microwave Scattering by Rimed Snowflakes, Q. J. Roy. Meteorol. Soc., doi:10.1002/qj.3093
Küchler, N., S. Kneifel, U. Löhnert, P. Kollias, H. Czekala, and T. Rose, 2017: A W-band radar-radiometer system for accurate and continuous monitoring of clouds and precipitation, J. Atmos. Oceanic Technol., doi:10.1175/JTECH-D-17-0019.1
Project Poster
Phase III Evaluation poster 2023
Phase II Evaluation poster 2019
Phase I Evaluation poster 2015
