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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 2) Peer-Reviewed
The interactions between biogenic volatile organic compounds (BVOCs), like isoprene and monoterpenes, and anthropogenic emissions of nitrogen and sulfur oxides lead to high concentrations of secondary organic aerosol...
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From:Atmospheric Chemistry and Physics (Vol. 16, Issue 16) Peer-ReviewedWe investigate the time evolution of the Local Boundary Layer (LBL) for the first time over a mountain ridge at Nainital (79.5°â¯E, 29.4°â¯N,...
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From:Atmospheric Chemistry and Physics (Vol. 17, Issue 15) Peer-ReviewedDuring the summertime CYPHEX campaign (CYprus PHotochemical EXperiment 2014) in the eastern Mediterranean, multiple volatile organic compounds (VOCs) were measured from a 650 m hilltop site in western Cyprus (34°...
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From:Atmospheric Chemistry and Physics (Vol. 16, Issue 22) Peer-ReviewedCharacterization of daytime sources of nitrous acid (HONO) is crucial to understand atmospheric oxidation and radical cycling in the planetary boundary layer. HONO and numerous other atmospheric trace constituents were...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 18) Peer-Reviewed
Hydrogen peroxide (H.sub.2 O.sub.2) plays a significant role in the oxidizing capacity of the atmosphere. It is an efficient oxidant in the liquid phase and serves as a temporary reservoir for the hydroxyl radical...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 6) Peer-ReviewedBioaerosols are produced by biological processes and directly emitted into the atmosphere, where they contribute to ice nucleation and the formation of precipitation. Previous studies have suggested that fungal spores...