Ice nucleation in the atmosphere influences cloud properties, altering precipitation and the
radiative balance, ultimately regulating Earth's climate. An accepted ice nucleation pathway …

Pore condensation and freezing (PCF) is an ice nucleation mechanism that explains ice
formation at low ice supersaturation. It assumes that liquid water condenses in pores of solid …

Atmospheric ice nucleation is crucial for global precipitation and affects the structure, lifetime
and reflectivity of clouds, thereby impacting climate. Ice nucleates in various ways from …

The nucleation of ice crystals in clouds is poorly understood, despite being of critical
importance for our planet's climate. Nucleation occurs largely at rare “active sites” present on …

Nucleation of ice from vapor on atmospheric aerosols has been attributed to the
condensation and freezing of supercooled water in small pores. Here we use wedge pores …

Heterogeneous ice nucleation is an important mechanism for the glaciation of mixed phase
clouds and may also be relevant for cloud formation and dehydration at the cirrus cloud …

Ice nucleation by different types of soot particles is systematically investigated over the
temperature range from 218 to 253 K relevant for both mixed-phase (MPCs) and cirrus …

In spite of the resurgence in ice nucleation research a comparatively small number of
studies deal with the phenomenon of pre-activation in heterogeneous ice nucleation. Fifty …

Atmospheric ice formation in cirrus clouds is often initiated by aerosol particles that act as ice-
nucleating particles. The aerosol–cloud interactions of soot and associated feedbacks …

The formation of ice particles in the atmosphere strongly affects cloud properties and the
climate. While mineral dust is known to be an effective ice nucleating particle, the role of …