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 …

Forests emit large quantities of volatile organic compounds (VOCs) to the atmosphere. Their
condensable oxidation products can form secondary organic aerosol, a significant and …

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

Secondary organic aerosol contributes to the atmospheric particle burden with implications
for air quality and climate. Biogenic volatile organic compounds such as terpenoids emitted …

It has been suggested that volatile organic compounds (VOCs) are involved in organic
aerosol formation, which in turn affects radiative forcing and climate. The most abundant …

Declining growth rates and injury to foliage have been observed in forests at high elevations
in areas of Europe and North America1, 2; in such areas the trees are regularly enveloped in …

Atmospheric acidity is increasingly determined by carbon dioxide and organic acids,–.
Among the latter, formic acid facilitates the nucleation of cloud droplets and contributes to …

THE presence in Norway of long-range transported air pollutants from the European
continent and England is well established. In particular, SO2 and other inorganic …

Pathways for the transfer of pollutants from the atmosphere to vegetation by gaseous
absorption (dry deposition) and in rain (wet deposition) have been studied extensively. Here …