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 …

Atmospheric ice‐nucleating particles (INPs) play a critical role in cloud freezing processes,
with important implications for precipitation formation and cloud radiative properties, and …

Atmospheric soot and organic particles from fossil fuel combustion and biomass burning
modify Earth's climate through their interactions with solar radiation and through …

Multiphase chemistry plays a vital role in the Earth system, climate, and health. Chemical
reactions, mass transport, and phase transitions between gases, liquids, and solids are …

Ice nucleating particles (INPs) are vital for ice initiation in, and precipitation from, mixed-
phase clouds. A source of INPs from oceans within sea spray aerosol (SSA) emissions has …

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 amount of ice present in clouds can affect cloud lifetime, precipitation and radiative
properties,. The formation of ice in clouds is facilitated by the presence of airborne ice …

Atmospheric aerosols, solid or liquid particles suspended in the atmosphere, range in size
from 1 nm to> 100 μm and come from a wide variety of sources. 1 As such, aerosols have a …

Organic aerosol particles play a key role in climate by serving as nuclei for clouds and
precipitation. Their sources and composition are highly variable, and their phase state …

Although too small to be seen with the human eye, atmospheric particulate matter has major
impacts on the world around us, from our health to global climate. Understanding the …