Claudia Mohr
0000-0002-3291-9295
16 papers found
Refreshing results…
Variation in chemical composition and volatility of oxygenated organic aerosol in different rural, urban, and mountain environments
Analysis of atmospheric particle growth based on vapor concentrations measured at the high-altitude GAW station Chacaltaya in the Bolivian Andes
Arctic observations of hydroperoxymethyl thioformate (HPMTF) – seasonal behavior and relationship to other oxidation products of dimethyl sulfide at the Zeppelin Observatory, Svalbard
Volatility of aerosol particles from NO3 oxidation of various biogenic organic precursors
Revealing the chemical characteristics of Arctic low-level cloud residuals – in situ observations from a mountain site
Measurement report: Molecular-level investigation of atmospheric cluster ions at the tropical high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes
Particle-phase processing of α-pinene NO3 secondary organic aerosol in the dark
Highly time-resolved chemical speciation and source apportionment of organic aerosol components in Delhi, India, using extractive electrospray ionization mass spectrometry
Photolytically induced changes in composition and volatility of biogenic secondary organic aerosol from nitrate radical oxidation during night-to-day transition
Insights into the molecular composition of semi-volatile aerosols in the summertime central Arctic Ocean using FIGAERO-CIMS
Size-segregated particle number and mass concentrations from different emission sources in urban Beijing
Deconvolution of FIGAERO–CIMS thermal desorption profiles using positive matrix factorisation to identify chemical and physical processes during particle evaporation
On the fate of oxygenated organic molecules in atmospheric aerosol particles
Heterogeneous ice nucleation of α‐pinene SOA particles before and after ice cloud processing
Molecular composition and volatility of isoprene photochemical oxidation secondary organic aerosol under low and high NO<sub>x</sub> conditions
Primary and secondary organic aerosol origin by combined gas-particle phase source apportionment
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