Organic aerosol components observed in Northern Hemispheric datasets from Aerosol Mass Spectrometry

We use this definition to estimate the constraints for each of the two, hourly-averaged SW CRF changes (within 20 %) due to a factor of two change in aerosol concentration from

The C-ToF-AMS usually have two different operational mode: The MS (Mass Spectrum) mode which is used to collect averaged mass spectra of the non-refractory aerosol and can provide

3.2 Sulfate as a predominant component of the background Antarctic aerosol number population If the externally mixed sulfate mode observed in the AMS is, in fact, the primary

by the AMS, and the estimated number losses, OA density, and collection e ffi ciency. ambient sample), [OA] is the mass concentration of organic aerosol, [Sulfates] is the

We report first results obtained from chamber produced secondary organic aerosol (SOA) from ozonolysis of isoprenoids and from ambient aerosol as measured during the

L.: Mexico City aerosol analysis during MILAGRO using high resolution aerosol mass spectrometry at the urban supersite (T0) – Part 1: Fine particle composition and organic

The real part of the refractive indices and effective densities for chemically segregated ambient aerosols in Guangzhou measured by a single-particle aerosol mass spectrometer..

than the OOA components of ambient aerosols (in particular, the OOA-1 component) in part due to higher precursor concentrations, perhaps arising from increased particle-