https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018JD029815

A Process Study on Thinning of Arctic Winter Cirrus Clouds With
High‐Resolution ICON‐ART Simulations
Simon Gruber Ulrich Blahak Florian Haenel Christoph Kottmeier Thomas
Leisner … See all authors
First published: 22 April 2019
https://doi.org/10.1029/2018JD029815
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Abstract
In this study, cloud‐resolving simulations of a case study for a limited
area of the hibernal Arctic were performed with the atmospheric modeling
system ICON‐ART (ICOsahedral Nonhydrostatic‐Aerosol and Reactive Trace
gases). A thorough comparison with data both from satellite as well as
aircraft measurement is presented to validate the simulations. In addition,
the model is applied to clarify the microphysical processes occurring when
introducing artificial aerosol particles into the upper troposphere with
the aim of modifying cirrus clouds in the framework of climate engineering.
Former modeling studies investigating the climate effect of this method
were performed with simplifying assumptions and much coarser resolution,
reaching partly contradicting conclusions concerning the method's
effectiveness. The primary effect of seeding is found to be a reduction of
ice crystal number concentrations in cirrus clouds, leading to increased
outgoing longwave radiative fluxes at the top of the atmosphere, thereby
creating a cooling effect. Furthermore, a secondary effect is found, as ice
crystals formed from the injected seeding aerosol particles lead to
enhanced riming of cloud droplets within the planetary boundary layer. This
effectively reduces the coverage of mixed‐phase clouds, thus generating
additional cooling by increased upward longwave radiative fluxes at the
surface. The efficacy of seeding cirrus clouds proves to be relatively
independent from the atmospheric background conditions, scales with the
number concentrations of seeding particles, and is highest for large
aerosol particles.

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