Quantifying uncertainties in determining morphological variables of ice crystals

Morphological variables (e.g., maximum dimension D max , projected area, perimeter, width, and roundness) of ice crystals are fundamental information to represent microphysical and radiative properties of ice clouds in numerical models, which can be derived via in-situ aircraft measurements. Convent...

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Main Authors: Park, S., Um, J., Järvinen, E., Schnaiter, M., McFarquhar, G., Kim, J.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019025
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5019025 2023-09-26T15:15:08+02:00 Quantifying uncertainties in determining morphological variables of ice crystals Park, S. Um, J. Järvinen, E. Schnaiter, M. McFarquhar, G. Kim, J. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019025 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2859 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019025 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2859 2023-08-27T23:42:01Z Morphological variables (e.g., maximum dimension D max , projected area, perimeter, width, and roundness) of ice crystals are fundamental information to represent microphysical and radiative properties of ice clouds in numerical models, which can be derived via in-situ aircraft measurements. Conventional airborne cloud probes are limited to a single observation angle to measure morphological variables. Non-spherical ice crystals may have different measured morphological variables depending on the observation angle, which causes uncertainties in the calculation of the microphysical and radiative properties of ice clouds. Thus, it is necessary to quantify uncertainties that depend on observation angles for determining the morphological variables of ice crystals. In this study, differences in determining the morphological variables of the ice crystals depending on observation angles were quantified using measurements of Particle Habit Imaging and Polar Scattering (PHIPS) probe that were acquired during the Arctic CLoud Observation Using airborne measurements during polar Day field campaign and the Southern Ocean Clouds Radiation Aerosol Transport Experimental Study field campaign. The PHIPS is a probe that provides stereo images of the sampled ice crystal from two different observation angles that are 120° apart. Morphological variables and habits of ice crystals were determined based on PHIPS stereo images. The uncertainties in determining morphological variables of ice crystals were quantified by calculating relative differences in morphological variables of ice crystals depending on observation angles. The nonsphericity of ice crystals sampled during ACLOUD and SOCRATES caused an average 14.69% (22.75%; 14.57%; 16.67%; 18.76%) uncertainty in determining Dmax (projected area; perimeter; width; roundness). Conference Object Arctic Southern Ocean GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Southern Ocean
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Morphological variables (e.g., maximum dimension D max , projected area, perimeter, width, and roundness) of ice crystals are fundamental information to represent microphysical and radiative properties of ice clouds in numerical models, which can be derived via in-situ aircraft measurements. Conventional airborne cloud probes are limited to a single observation angle to measure morphological variables. Non-spherical ice crystals may have different measured morphological variables depending on the observation angle, which causes uncertainties in the calculation of the microphysical and radiative properties of ice clouds. Thus, it is necessary to quantify uncertainties that depend on observation angles for determining the morphological variables of ice crystals. In this study, differences in determining the morphological variables of the ice crystals depending on observation angles were quantified using measurements of Particle Habit Imaging and Polar Scattering (PHIPS) probe that were acquired during the Arctic CLoud Observation Using airborne measurements during polar Day field campaign and the Southern Ocean Clouds Radiation Aerosol Transport Experimental Study field campaign. The PHIPS is a probe that provides stereo images of the sampled ice crystal from two different observation angles that are 120° apart. Morphological variables and habits of ice crystals were determined based on PHIPS stereo images. The uncertainties in determining morphological variables of ice crystals were quantified by calculating relative differences in morphological variables of ice crystals depending on observation angles. The nonsphericity of ice crystals sampled during ACLOUD and SOCRATES caused an average 14.69% (22.75%; 14.57%; 16.67%; 18.76%) uncertainty in determining Dmax (projected area; perimeter; width; roundness).
format Conference Object
author Park, S.
Um, J.
Järvinen, E.
Schnaiter, M.
McFarquhar, G.
Kim, J.
spellingShingle Park, S.
Um, J.
Järvinen, E.
Schnaiter, M.
McFarquhar, G.
Kim, J.
Quantifying uncertainties in determining morphological variables of ice crystals
author_facet Park, S.
Um, J.
Järvinen, E.
Schnaiter, M.
McFarquhar, G.
Kim, J.
author_sort Park, S.
title Quantifying uncertainties in determining morphological variables of ice crystals
title_short Quantifying uncertainties in determining morphological variables of ice crystals
title_full Quantifying uncertainties in determining morphological variables of ice crystals
title_fullStr Quantifying uncertainties in determining morphological variables of ice crystals
title_full_unstemmed Quantifying uncertainties in determining morphological variables of ice crystals
title_sort quantifying uncertainties in determining morphological variables of ice crystals
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019025
geographic Arctic
Southern Ocean
geographic_facet Arctic
Southern Ocean
genre Arctic
Southern Ocean
genre_facet Arctic
Southern Ocean
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2859
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019025
op_doi https://doi.org/10.57757/IUGG23-2859
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