Shape dependence of snow crystal fall speed

Improved snowfall predictions require accurate knowledge of the properties of ice crystals and snow particles, such as their size, cross-sectional area, shape, and fall speed. The fall speed of ice particles is a critical parameter for the representation of ice clouds and snow in atmospheric numeric...

Full description

Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Vázquez-Martín, Sandra, Kuhn, Thomas, Eliasson, Salomon
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/acp-21-7545-2021
https://acp.copernicus.org/articles/21/7545/2021/
id ftcopernicus:oai:publications.copernicus.org:acp90261
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:acp90261 2023-05-15T17:04:22+02:00 Shape dependence of snow crystal fall speed Vázquez-Martín, Sandra Kuhn, Thomas Eliasson, Salomon 2021-05-18 application/pdf https://doi.org/10.5194/acp-21-7545-2021 https://acp.copernicus.org/articles/21/7545/2021/ eng eng doi:10.5194/acp-21-7545-2021 https://acp.copernicus.org/articles/21/7545/2021/ eISSN: 1680-7324 Text 2021 ftcopernicus https://doi.org/10.5194/acp-21-7545-2021 2021-05-24T16:22:15Z Improved snowfall predictions require accurate knowledge of the properties of ice crystals and snow particles, such as their size, cross-sectional area, shape, and fall speed. The fall speed of ice particles is a critical parameter for the representation of ice clouds and snow in atmospheric numerical models, as it determines the rate of removal of ice from the modelled clouds. Fall speed is also required for snowfall predictions alongside other properties such as ice particle size, cross-sectional area, and shape. For example, shape is important as it strongly influences the scattering properties of these ice particles and thus their response to remote sensing techniques. This work analyzes fall speed as a function of particle size (maximum dimension), cross-sectional area, and shape using ground-based in situ measurements. The measurements for this study were done in Kiruna, Sweden, during the snowfall seasons of 2014 to 2019, using the ground-based in situ instrument Dual Ice Crystal Imager (D-ICI). The resulting data consist of high-resolution images of falling hydrometeors from two viewing geometries that are used to determine particle size (maximum dimension), cross-sectional area, area ratio, orientation, and the fall speed of individual particles. The selected dataset covers sizes from about 0.06 to 3.2 mm and fall speeds from 0.06 to 1.6 m s −1 . Relationships between particle size, cross-sectional area, and fall speed are studied for different shapes. The data show in general low correlations to fitted fall speed relationships due to large spread observed in fall speed. After binning the data according to size or cross-sectional area, correlations improve, and we can report reliable parameterizations of fall speed vs. particle size or cross-sectional area for part of the shapes. For most of these shapes, the fall speed is better correlated with cross-sectional area than with particle size. The effects of orientation and area ratio on the fall speed are also studied, and measurements show that vertically oriented particles fall faster on average. However, most particles for which orientation can be defined fall horizontally. Text Kiruna Copernicus Publications: E-Journals Kiruna Atmospheric Chemistry and Physics 21 10 7545 7565
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Improved snowfall predictions require accurate knowledge of the properties of ice crystals and snow particles, such as their size, cross-sectional area, shape, and fall speed. The fall speed of ice particles is a critical parameter for the representation of ice clouds and snow in atmospheric numerical models, as it determines the rate of removal of ice from the modelled clouds. Fall speed is also required for snowfall predictions alongside other properties such as ice particle size, cross-sectional area, and shape. For example, shape is important as it strongly influences the scattering properties of these ice particles and thus their response to remote sensing techniques. This work analyzes fall speed as a function of particle size (maximum dimension), cross-sectional area, and shape using ground-based in situ measurements. The measurements for this study were done in Kiruna, Sweden, during the snowfall seasons of 2014 to 2019, using the ground-based in situ instrument Dual Ice Crystal Imager (D-ICI). The resulting data consist of high-resolution images of falling hydrometeors from two viewing geometries that are used to determine particle size (maximum dimension), cross-sectional area, area ratio, orientation, and the fall speed of individual particles. The selected dataset covers sizes from about 0.06 to 3.2 mm and fall speeds from 0.06 to 1.6 m s −1 . Relationships between particle size, cross-sectional area, and fall speed are studied for different shapes. The data show in general low correlations to fitted fall speed relationships due to large spread observed in fall speed. After binning the data according to size or cross-sectional area, correlations improve, and we can report reliable parameterizations of fall speed vs. particle size or cross-sectional area for part of the shapes. For most of these shapes, the fall speed is better correlated with cross-sectional area than with particle size. The effects of orientation and area ratio on the fall speed are also studied, and measurements show that vertically oriented particles fall faster on average. However, most particles for which orientation can be defined fall horizontally.
format Text
author Vázquez-Martín, Sandra
Kuhn, Thomas
Eliasson, Salomon
spellingShingle Vázquez-Martín, Sandra
Kuhn, Thomas
Eliasson, Salomon
Shape dependence of snow crystal fall speed
author_facet Vázquez-Martín, Sandra
Kuhn, Thomas
Eliasson, Salomon
author_sort Vázquez-Martín, Sandra
title Shape dependence of snow crystal fall speed
title_short Shape dependence of snow crystal fall speed
title_full Shape dependence of snow crystal fall speed
title_fullStr Shape dependence of snow crystal fall speed
title_full_unstemmed Shape dependence of snow crystal fall speed
title_sort shape dependence of snow crystal fall speed
publishDate 2021
url https://doi.org/10.5194/acp-21-7545-2021
https://acp.copernicus.org/articles/21/7545/2021/
geographic Kiruna
geographic_facet Kiruna
genre Kiruna
genre_facet Kiruna
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-21-7545-2021
https://acp.copernicus.org/articles/21/7545/2021/
op_doi https://doi.org/10.5194/acp-21-7545-2021
container_title Atmospheric Chemistry and Physics
container_volume 21
container_issue 10
container_start_page 7545
op_container_end_page 7565
_version_ 1766058441555574784