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
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Other (Time-Height NetCDF for the CONTROL simulation)
ISDAC_chen_control.nc - Submitted Version 255MB | |
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Other (Time-Height NetCDF for the DRY simulation)
ISDAC_chen_dry.nc - Submitted Version 255MB | |
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Other (Time-Height NetCDF for the WEAKINV simulation)
ISDAC_chen_weakinv.nc - Submitted Version 255MB | |
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Other (Time-Height NetCDF for the INFLUX simulation)
ISDAC_chen_influx.nc - Submitted Version 255MB | |
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Other (Time-Height NetCDF for the DRY_WEAKINV simulation)
ISDAC_chen_dry_weakinv.nc - Submitted Version 255MB | |
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Other (Time-Height NetCDF for the DRY_INFLUX simulation)
ISDAC_chen_dry_influx.nc - Submitted Version 255MB | |
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Other (3D Output NetCDF for CONTROL)
ISDAC_chen_control_merged.nc - Submitted Version 4GB | |
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PDF (Data Reproduction Guide for Jupyter)
Data_Reproduction_Guide.pdf - Supplemental Material 54kB |
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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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