Modeling case studies of ice production in Arctic mixed-phase clouds

In common weather and climate models rime-splintering is the only included secondary ice production process. In addition, assumed concentrations of cloud condensation nuclei or cloud droplet number as well as of ice-nucleating particle are higher in standard models than for Arctic environments. This...

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Main Authors: Schäfer, B., David, R., Dammann, S., Trude, S.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021139
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021139 2023-07-30T04:01:14+02:00 Modeling case studies of ice production in Arctic mixed-phase clouds Schäfer, B. David, R. Dammann, S. Trude, S. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021139 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4731 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021139 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4731 2023-07-16T23:40:25Z In common weather and climate models rime-splintering is the only included secondary ice production process. In addition, assumed concentrations of cloud condensation nuclei or cloud droplet number as well as of ice-nucleating particle are higher in standard models than for Arctic environments. This can lead to a misrepresentation of phase distribution in and precipitation from Arctic mixed-phase clouds. During the Ny-Ålesund Aerosol Cloud Experiment (NASCENT) a holographic probe mounted on a tethered balloon took in-situ measurements of ice crystal and cloud droplet number and mass concentrations in Svalbard, Norway, during fall 2019 and spring 2020. In this study, we use the Weather Research and Forecasting (WRF) model to simulate selected case studies from this campaign in a high vertical and spatial resolution. We test the performance of different microphysical parametrizations and apply a new state-of-the-art secondary ice parametrization. We find that the degree of agreement with observations highly depends on the chosen microphysics settings and that for a case with a lot of observed secondary ice production modeled ice crystal concentrations stay below the measured values even after adding new secondary ice processes to the model. In addition to performing sensitivity studies regarding microphysical parametrizations and the direct comparison with observations from the balloon, we analyze the spatial variability of cloud phase and its dependence on different meteorological parameters. Conference Object Arctic Ny Ålesund Ny-Ålesund Svalbard GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Norway Ny-Ålesund Rime ENVELOPE(6.483,6.483,62.567,62.567) Svalbard
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description In common weather and climate models rime-splintering is the only included secondary ice production process. In addition, assumed concentrations of cloud condensation nuclei or cloud droplet number as well as of ice-nucleating particle are higher in standard models than for Arctic environments. This can lead to a misrepresentation of phase distribution in and precipitation from Arctic mixed-phase clouds. During the Ny-Ålesund Aerosol Cloud Experiment (NASCENT) a holographic probe mounted on a tethered balloon took in-situ measurements of ice crystal and cloud droplet number and mass concentrations in Svalbard, Norway, during fall 2019 and spring 2020. In this study, we use the Weather Research and Forecasting (WRF) model to simulate selected case studies from this campaign in a high vertical and spatial resolution. We test the performance of different microphysical parametrizations and apply a new state-of-the-art secondary ice parametrization. We find that the degree of agreement with observations highly depends on the chosen microphysics settings and that for a case with a lot of observed secondary ice production modeled ice crystal concentrations stay below the measured values even after adding new secondary ice processes to the model. In addition to performing sensitivity studies regarding microphysical parametrizations and the direct comparison with observations from the balloon, we analyze the spatial variability of cloud phase and its dependence on different meteorological parameters.
format Conference Object
author Schäfer, B.
David, R.
Dammann, S.
Trude, S.
spellingShingle Schäfer, B.
David, R.
Dammann, S.
Trude, S.
Modeling case studies of ice production in Arctic mixed-phase clouds
author_facet Schäfer, B.
David, R.
Dammann, S.
Trude, S.
author_sort Schäfer, B.
title Modeling case studies of ice production in Arctic mixed-phase clouds
title_short Modeling case studies of ice production in Arctic mixed-phase clouds
title_full Modeling case studies of ice production in Arctic mixed-phase clouds
title_fullStr Modeling case studies of ice production in Arctic mixed-phase clouds
title_full_unstemmed Modeling case studies of ice production in Arctic mixed-phase clouds
title_sort modeling case studies of ice production in arctic mixed-phase clouds
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021139
long_lat ENVELOPE(6.483,6.483,62.567,62.567)
geographic Arctic
Norway
Ny-Ålesund
Rime
Svalbard
geographic_facet Arctic
Norway
Ny-Ålesund
Rime
Svalbard
genre Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4731
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021139
op_doi https://doi.org/10.57757/IUGG23-4731
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