The potential for atmospheric aerosol particles to exist as metastable aqueous droplets
instead of in their thermodynamically favoured crystalline solid phase has many implications …

Secondary organic aerosol (SOA) particles are formed in the atmosphere from condensable
oxidation products of anthropogenic and biogenic volatile organic compounds (VOCs) …

Traditional Köhler theory describes the equilibrium vapour-pressure relationship between
liquid solution particles and humid air. Here we present the concept of multiphase …

Anthropogenic aerosols are intricately linked to the climate system and to the hydrologic
cycle. The net effect of aerosols is to cool the climate system by reflecting sunlight …

Understanding the properties of clouds in the Earth's atmosphere is currently limited by
difficulties at the fundamental level of adequately describing the processes of cloud droplet …

Aerosol formation in the atmosphere is an important process to understand, in that such
particles may act as the cloud condensation nuclei responsible for the 'cloud–climate'effect …

Aerosol particles produced over forested areas may affect climate by acting as nuclei for
cloud condensation, but their composition (and hence the chemical species that drive their …

The spontaneous growth of cloud condensation nuclei (CCN) into cloud droplets under
supersaturated water vapour conditions is described by classic Köhler theory,. This …

Atmospheric aerosols counteract the warming effects of anthropogenic greenhouse gases
by an uncertain, but potentially large, amount. This in turn leads to large uncertainties in the …

Anthropogenic aerosols enhance cloud reflectivity by increasing the number concentration
of cloud droplets, leading to a cooling effect on climate known as the indirect aerosol effect …