Biological particles in the Earth's atmosphere are a distinctive category of ice nucleating
particles (INPs) due to their capability of facilitating ice crystal formation in clouds at …

Predicting the formation of ice in the atmosphere presents one of the great challenges in
physical sciences with important implications for the chemistry and composition of the …

The Arctic is warming faster than anywhere else on Earth, prompting glacial melt, permafrost
thaw, and sea ice decline. These severe consequences induce feedbacks that contribute to …

This chapter reviews the history of the discovery of cloud nuclei and their impacts on cloud
microphysics and the climate system. Pioneers including John Aitken, Sir John Mason …

Aeolian dusts serve as ice nucleating particles in mixed-phase clouds, and thereby alter the
cloud properties and lifetime. Glacial outwash plains are thought to be a major dust source …

Ice-nucleating particles (INPs) are rare atmospheric aerosols that initiate primary ice
formation, but accurately simulating their concentrations and variability in large-scale climate …

Sea spray aerosol (SSA) generated by bubble bursting at the ocean surface is an important
component of aerosol‐cloud interactions over remote oceans, providing the atmosphere …

The second phase of the Fifth International Ice Nucleation Workshop (FIN-02) involved the
gathering of a large number of researchers at the Karlsruhe Institute of Technology's Aerosol …

Aerosols that are efficient ice-nucleating particles (INPs) are crucial for the formation of cloud
ice via heterogeneous nucleation in the atmosphere. The distribution of INPs on a large …

The Arctic region is sensitive to climate change and is warming faster than the global
average. Aerosol particles change cloud properties by acting as cloud condensation nuclei …