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

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 …

Cloud properties are strongly influenced by ice formation; hence, we need to understand the
sources of ice-nucleating particles (INPs) around the globe. Boreal forests are known as …

Mixed-phase clouds (MPCs) can have a net warming or cooling radiative effect on Earth's
climate influenced by the phase and concentration of cloud particles. They have received …

The amount of ice versus supercooled water in clouds is important for their radiative
properties and role in climate feedbacks. Hence, knowledge of the concentration of ice …

Detailed knowledge of the physical and chemical properties and sources of particles that
form clouds is especially important in pristine areas like the Arctic, where particle …

The Arctic is warming two to three times faster than the global average, and the role of
aerosols is not well constrained. Aerosol number concentrations can be very low in remote …

Ice-nucleating particles (INPs) are atmospheric aerosol particles that can strongly influence
the radiative properties and precipitation onset in mixed-phase clouds by triggering ice …

Airborne microorganisms transported from forested areas can influence cloud formation by
forming ice nuclei. However, the vertical transportation of airborne microorganisms over …

Ice particle activation and evolution have important atmospheric implications for cloud
formation, initiation of precipitation and radiative interactions. In many cases the initial …