Proton-transfer-reaction time-of-flight mass spectrometry (PTR-ToF-MS) is a technique
commonly used to measure ambient volatile organic compounds (VOCs) in urban, rural, and …

The exchange of trace gases between the biosphere and the atmosphere is an important
process that controls both chemical and physical properties of the atmosphere with …

Volatile organic compound (VOC) emissions and subsequent oxidation contribute to the
formation of secondary pollutants and poor air quality in general. As more VOCs at lower …

We present direct measurements of biogenic volatile organic compound (BVOC)-induced
nitrate radical (NO 3) reactivity (k VOC) through the diel cycle in the suburban, temperate …

A primary sink of air pollutants and their precursors is dry deposition. Dry deposition
estimates differ across chemical transport models, yet an understanding of the model spread …

Biogenic and anthropogenic organic vapors are crucial precursors of ozone and secondary
organic aerosol (SOA) in the atmosphere. Here we conducted real-time measurements of …

Dry deposition of ozone (O 3) to the ocean surface and the ozonolysis of organics in the sea
surface microlayer (SSML) are potential sources of volatile organic compounds (VOCs) to …

We use observations from dual high‐resolution mass spectrometers to characterize
ecosystem‐atmosphere fluxes of reactive carbon across an extensive range of volatile …

The decomposition of plant litter, most of which is found in forests, is an important element of
the global carbon cycle, as a result of which carbon enters the atmosphere in the form of not …

In general, NPF is controlled by different chemical and physical processes. NPF events are
commonly observed in spring and autumn in the boreal forest and have been connected to …