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Citation: Ascher, Benjamin and Hoffmann, Fabian: Model data to recreate figures seen in the manuscript "Impacts of Environmental Conditions and Ice Nuclei Recycling on Arctic Mixed-Phase Cloud Properties.". 14. November 2025. Open Data LMU. 10.5282/ubm/data.720

Model data to recreate figures seen in the manuscript "Impacts of Environmental Conditions and Ice Nuclei Recycling on Arctic Mixed-Phase Cloud Properties."
Model data to recreate figures seen in the manuscript "Impacts of Environmental Conditions and Ice Nuclei Recycling on Arctic Mixed-Phase Cloud Properties."

Radiatively driven Arctic stratocumulus clouds have important climactic impacts due to their effects on surface radiative balance. The presence of both liquid and ice within Arctic stratocumulus, and their interaction through the Wegener-Bergeron-Findeisen (WBF) process, strongly affects the properties and lifetimes of these clouds. To assess the impacts of mixed-phase microphysical processes in Arctic Stratocumulus, we use a Langrangian cloud microphysical model within a large eddy simulation framework to simulate a single-layer cloud under varying free-tropospheric humidity and above-cloud inversion strength. We also run two simulations in which precipitating ice crystals have their IN re-injected into the model domain, rather than removed. We find that IN recycling plays a critical role in maintaining the presence of ice in the mixed-phase cloud. The simulations with drier free-tropospheric air experience greater sublimation of ice crystals below cloud, recycling of ice crystals, and a higher ice water path than simulations with more humid free-tropospheric air. We also find that the impact of inversion strength on cloud microphysical characteristics is strongly modulated by free-tropospheric relative humidity, with decreased inversion strength resulting in both increased and decreased liquid water path under high and low free-tropospheric relative humidity, respectively.

Code to the Jupyter notebook: https://doi.org/10.5281/zenodo.17662940

Atmospheric Science, ice microphysics, aerosol-cloud interactions, atmospheric modeling, mixed-phase stratocumulus
Ascher, Benjamin
Hoffmann, Fabian
2025

[thumbnail of Time-Height NetCDF for the CONTROL simulation] Other (Time-Height NetCDF for the CONTROL simulation)
ISDAC_chen_control.nc - Submitted Version

255MB
[thumbnail of Time-Height NetCDF for the DRY simulation] Other (Time-Height NetCDF for the DRY simulation)
ISDAC_chen_dry.nc - Submitted Version

255MB
[thumbnail of Time-Height NetCDF for the WEAKINV simulation] Other (Time-Height NetCDF for the WEAKINV simulation)
ISDAC_chen_weakinv.nc - Submitted Version

255MB
[thumbnail of Time-Height NetCDF for the INFLUX simulation] Other (Time-Height NetCDF for the INFLUX simulation)
ISDAC_chen_influx.nc - Submitted Version

255MB
[thumbnail of Time-Height NetCDF for the DRY_WEAKINV simulation] Other (Time-Height NetCDF for the DRY_WEAKINV simulation)
ISDAC_chen_dry_weakinv.nc - Submitted Version

255MB
[thumbnail of Time-Height NetCDF for the DRY_INFLUX simulation] Other (Time-Height NetCDF for the DRY_INFLUX simulation)
ISDAC_chen_dry_influx.nc - Submitted Version

255MB
[thumbnail of 3D Output NetCDF for CONTROL] Other (3D Output NetCDF for CONTROL)
ISDAC_chen_control_merged.nc - Submitted Version

4GB
[thumbnail of Data Reproduction Guide for Jupyter]
Preview
PDF (Data Reproduction Guide for Jupyter)
Data_Reproduction_Guide.pdf - Supplemental Material

54kB
[thumbnail of Readme to Impacts of Environmental Conditions and Ice Nuclei Recycling] Other (Readme to Impacts of Environmental Conditions and Ice Nuclei Recycling)
README.md - Supplemental Material

1kB

DOI: 10.5282/ubm/data.720

This dataset is available unter the terms of the following Creative Commons LicenseCC BY-NC-SA 4.0

Abstract

Radiatively driven Arctic stratocumulus clouds have important climactic impacts due to their effects on surface radiative balance. The presence of both liquid and ice within Arctic stratocumulus, and their interaction through the Wegener-Bergeron-Findeisen (WBF) process, strongly affects the properties and lifetimes of these clouds. To assess the impacts of mixed-phase microphysical processes in Arctic Stratocumulus, we use a Langrangian cloud microphysical model within a large eddy simulation framework to simulate a single-layer cloud under varying free-tropospheric humidity and above-cloud inversion strength. We also run two simulations in which precipitating ice crystals have their IN re-injected into the model domain, rather than removed. We find that IN recycling plays a critical role in maintaining the presence of ice in the mixed-phase cloud. The simulations with drier free-tropospheric air experience greater sublimation of ice crystals below cloud, recycling of ice crystals, and a higher ice water path than simulations with more humid free-tropospheric air. We also find that the impact of inversion strength on cloud microphysical characteristics is strongly modulated by free-tropospheric relative humidity, with decreased inversion strength resulting in both increased and decreased liquid water path under high and low free-tropospheric relative humidity, respectively. Code to the Jupyter notebook: https://doi.org/10.5281/zenodo.17662940

Uncontrolled Keywords

Atmospheric Science, ice microphysics, aerosol-cloud interactions, atmospheric modeling, mixed-phase stratocumulus

Item Type:Data
Contact Person:Ascher, Benjamin
E-Mail of Contact:ben.ascher at lmu.de
Subjects:Geosciences
Dewey Decimal Classification:500 Natural sciences and mathematics
500 Natural sciences and mathematics > 550 Earth sciences
ID Code:720
Deposited By: Benjamin Ascher
Deposited On:26. Nov 2025 09:30
Last Modified:26. Nov 2025 09:31

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