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 …

The role of marine bioaerosols in cloud formation and climate is currently so uncertain that
even the sign of the climate forcing is unclear. Marine aerosols form through direct …

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 …

The oceans represent a significant global source of atmospheric aerosols. Sea spray
aerosol (SSA) particles comprise sea salts and organic species in varying proportions. In …

A likely important feature of the poorly understood aerosol‐cloud interactions over the
Southern Ocean (SO) is the dominant role of sea spray aerosol, versus terrestrial aerosol …

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 …

Aerosols that serve as ice nucleating particles (INPs) have the potential to modulate cloud
microphysical properties and can therefore impact cloud radiative forcing (CRF) and …

Maritime boundary‐layer clouds over the Southern Ocean (SO) have a large shortwave
radiative effect. Yet, climate models have difficulties in representing these clouds and …

Sea spray aerosol (SSA) is a widely recognized important source of ice-nucleating particles
(INPs) in the atmosphere. However, composition-specific identification, nucleation …