One barrier to predicting biogenic secondary organic aerosol (SOA) formation in a changing
climate can be attributed to the complex nature of plant volatile emissions. Plant volatile …

Leaf mechanical wounding triggers a rapid release—within minutes—of a blend of volatile
organic compounds. A wounding-induced VOC blend is mainly composed of oxygenated …

Biogenic volatile organic compounds (BVOCs) emitted from terrestrial plants contribute
substantially to ozone (O3) and secondary organic aerosol (SOA) formation in the …

The introduction of new crops to agroecosystems can change the chemical composition of
the atmosphere by altering the amount and type of plant‐derived biogenic volatile organic …

Emissions of biogenic volatile organic compounds (BVOC) from urban trees during and after
blooming were measured during spring and early summer 2009 in Boulder, Colorado. Air …

Biogenic emissions supply the largest fraction of non-methane volatile organic compounds
(VOC) from the biosphere to the atmospheric boundary layer, and typically comprise a …

Abstract Background and Aims Volatile organic compound (VOC) emissions from biogenic
sources are important contributors to chemical reactions in the air. Soil/forest floor VOCs …

Biogenic volatile organic compounds (BVOCs) are known to play an important role in
atmospheric chemistry due to their high reactivity and high emission rates. Therefore, in …

The biogenic organic precursors which are of relevance in secondary organic aerosol
formation are primarily isoprene, monoterpenes, sesquiterpenes (SQTs) and their …

Despite the significant contribution of biogenic volatile organic compounds (BVOCs) to
organic aerosol formation and ozone production and loss, there are few long-term, year …