This review intends to critically assess recent findings related to nucleation and growth of
atmospheric nanoparticles, with an emphasis on the understanding of these processes at a …

The physical state of a material is described as its phase. Common phases of the molecule
H2O include vapor, liquid water, and ice. Examples of these phases in the atmosphere are …

The atmospheric effects of soot aerosols include interference with radiative transfer, visibility
impairment, and alteration of cloud formation and are highly sensitive to the manner by …

More than three decades have passed since the publication of the last review of the Venus
clouds and hazes. The paper published in 1983 in the Venus book summarized the …

Light absorption by carbon soot increases when the particles are internally mixed with
nonabsorbing materials, leading to increased radiative forcing, but the magnitude of this …

The molecular processes leading to formation of nanoparticles of blue haze over forested
areas are highly complex and not fully understood. We show that the interaction between …

Generalised equations are presented for an extended form of the Pitzer molality-based
thermodynamic model, involving an ionic strength-dependent third virial coefficient …

An important issue for developing a molecular-level mechanism of heterogeneous
interactions at the aqueous interface is determining changes in the interface with changes in …

The hygroscopic properties of submicron soot particles during internal mixing with gaseous
sulfuric acid have been investigated using a combined tandem differential mobility analyzer …

There is extensive evidence to suggest that stratospheric aerosols can remain liquid to very
low stratospheric temperatures, despite being highly supercooled. Even polar stratospheric …