On the geometry of aggregate snowflakes

Fuente: arXiv
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Main Authors: Seifert, Axel, Siewert, Christoph, Jakub, Fabian, von Terzi, Leonie, Kneifel, Stefan
Format: Preprint
Published: 2026
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author Seifert, Axel
Siewert, Christoph
Jakub, Fabian
von Terzi, Leonie
Kneifel, Stefan
author_facet Seifert, Axel
Siewert, Christoph
Jakub, Fabian
von Terzi, Leonie
Kneifel, Stefan
contents Snowflakes play a crucial role in weather and climate. A significant portion of precipitation that reaches the surface originates as ice, even when it ultimately falls as rain. Contrary to the popular image of symmetric, dendritic crystals, most large snowflakes are irregular aggregates formed through the collision of primary ice crystals, such as hexagonal plates, columns, and dendrites. These aggregates exhibit complex, fractal-like structures, particularly at large sizes. Despite this structural complexity, each aggregate snowflake is unique, with properties that vary significantly around the mean - variability that is typically neglected in weather and climate models. Using a physically based aggregation model, we generate millions of synthetic snowflakes to investigate their geometric properties. The resulting dataset reveals that, for a given monomer number (cluster size) and mass, the maximum dimension follows approximately a lognormal distribution. We present a parameterization of aggregate geometry that captures key statistical properties, including maximum dimension, aspect ratio, cross-sectional area, and their joint correlations. This formulation enables a stochastic representation of aggregate snowflakes in Lagrangian particle models. Incorporating this variability improves the realism of simulated fall velocities, enhances growth rates by aggregation, and broadens Doppler radar spectra in closer agreement with observations.
format Preprint
id arxiv_https___arxiv_org_abs_2601_10608
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle On the geometry of aggregate snowflakes
Seifert, Axel
Siewert, Christoph
Jakub, Fabian
von Terzi, Leonie
Kneifel, Stefan
Atmospheric and Oceanic Physics
Snowflakes play a crucial role in weather and climate. A significant portion of precipitation that reaches the surface originates as ice, even when it ultimately falls as rain. Contrary to the popular image of symmetric, dendritic crystals, most large snowflakes are irregular aggregates formed through the collision of primary ice crystals, such as hexagonal plates, columns, and dendrites. These aggregates exhibit complex, fractal-like structures, particularly at large sizes. Despite this structural complexity, each aggregate snowflake is unique, with properties that vary significantly around the mean - variability that is typically neglected in weather and climate models. Using a physically based aggregation model, we generate millions of synthetic snowflakes to investigate their geometric properties. The resulting dataset reveals that, for a given monomer number (cluster size) and mass, the maximum dimension follows approximately a lognormal distribution. We present a parameterization of aggregate geometry that captures key statistical properties, including maximum dimension, aspect ratio, cross-sectional area, and their joint correlations. This formulation enables a stochastic representation of aggregate snowflakes in Lagrangian particle models. Incorporating this variability improves the realism of simulated fall velocities, enhances growth rates by aggregation, and broadens Doppler radar spectra in closer agreement with observations.
title On the geometry of aggregate snowflakes
topic Atmospheric and Oceanic Physics
url https://arxiv.org/abs/2601.10608