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\begin{document}

\title{Understanding the history of complex ice crystal habits deduced from a
holographic imager}



\author[1]{Julie Thérèse Pasquier}%
\author[2]{Jan Henneberger}%
\author[3]{Alexei Korolev}%
\author[4]{Fabiola Ramelli}%
\author[5]{Jörg Wieder}%
\author[6]{Annika Lauber}%
\author[1]{Guangyu Li}%
\author[7]{Robert Oscar David}%
\author[7]{Tim Carlsen}%
\author[8]{Rosa Gierens}%
\author[9]{Marion Maturilli}%
\author[2]{Ulrike Lohmann}%
\affil[1]{Institute for Atmospheric and Climate Science, ETH Zürich}%
\affil[2]{ETH Zurich}%
\affil[3]{Environment Canada}%
\affil[4]{Swiss Federal Institute of Technology in Zurich}%
\affil[5]{Institute for Atmospheric and Climate Science}%
\affil[6]{Center for Climate Systems Modeling (C2SM)}%
\affil[7]{University of Oslo}%
\affil[8]{University of Cologne}%
\affil[9]{Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research}%


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  \date{May 26, 2024}


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\begin{abstract}
The sizes and shapes of ice crystals influence the radiative properties
of clouds, as well as precipitation initiation and aerosol scavenging.
However, ice crystal growth mechanisms remain only partially
characterized. We present the growth processes of two complex ice
crystal habits observed in Arctic mixed-phase clouds during the NASCENT
campaign. First, are capped-columns with multiple columns growing out of
the plates' corners that we define as columns on capped-columns (CCC).
These ice crystals originated from cycling through the columnar and
plate temperature growth regimes, during their vertical transport by
in-cloud circulation. Second, is aged rime on the surface of ice
crystals having grown into faceted columns or plates depending on the
environmental conditions. Despite their complexity, the shapes of these
ice crystals allow to infer their growth history and provide information
about the in-cloud conditions. Additionally, these ice crystals exhibit
complex shapes and could enhance aggregation and secondary ice
production.%
\end{abstract}%



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