https://acp.copernicus.org/articles/22/3763/2022/

The effect of marine ice-nucleating particles on mixed-phase clouds
Tomi Raatikainen, Marje Prank, Jaakko Ahola, Harri Kokkola, Juha Tonttila, and
Sami Romakkaniemi

*Abstract*

Shallow marine mixed-phase clouds are important for the Earth's radiative
balance, but modelling their formation and dynamics is challenging. These
clouds depend on boundary layer turbulence and cloud top radiative cooling,
which is related to the cloud phase. The fraction of frozen droplets
depends on the availability of suitable ice-nucleating particles (INPs),
which initiate droplet freezing. While mineral dust is the dominating INP
type in most regions, high-latitude boundary layer clouds can be dependent
on local marine INP emissions, which are often related to biogenic sources
including phytoplankton. Here we use high resolution large eddy simulations
to examine the potential effects of marine emissions on boundary layer INP
concentrations and their effects on clouds. Surface emissions have a direct
effect on INP concentration in a typical well-mixed boundary layer whereas
a steep inversion can block the import of background INPs from the free
troposphere. The importance of the marine source depends on the background
INP concentration, so that marine INP emissions become more important with
lower background INP concentrations. For the INP budget it is also
important to account for INP recycling. Finally, with the high-resolution
model we show how ice nucleation hotspots and high INP concentrations are
focused on updraught regions. Our results show that marine INP emissions
contribute directly to the boundary layer INP budget and therefore have an
influence on mixed-phase clouds.
[image: image.png]

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