Claudia Mohr

Claudia Mohr

Auto-generated profile, based on publicly available information

Claudia Mohr

Department of Environmental Science, Stockholm University

Research Focus & Metrics

Academic Career Length

21Years (2006-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
15 May 2008 in Environmental Science & Technology
Verified
Journal Article
Closed access
Allison C. AikenAllison C. Aiken
Allison C. Aiken
PDPeter F. DeCarlo
Peter F. DeCarlo
JKJesse H. Kroll
Jesse H. Kroll
DWDouglas R. Worsnop
Douglas R. Worsnop
JHJ. Alex Huffman
J. Alex Huffman
JJJose L. Jimenez
Jose L. Jimenez

7 May 2014 in Environmental Science & Technology
Verified
Journal Article
Closed access
BLBen H. Lee
Ben H. Lee
FLFelipe D. Lopez-Hilfiker
Felipe D. Lopez-Hilfiker
CMClaudia Mohr
Claudia Mohr
TKTheo Kurtén
Theo Kurtén
DWDouglas R. Worsnop
Douglas R. Worsnop
JTJoel A. Thornton
Joel A. Thornton

15 April 2014 in Atmospheric Measurement Techniques
Verified
Journal Article
Open access
FLF. D. Lopez-Hilfiker
F. D. Lopez-Hilfiker
CMC. Mohr
C. Mohr
MEM. Ehn
M. Ehn
FRF. Rubach
F. Rubach
EKE. Kleist
E. Kleist
JTJ. A. Thornton
J. A. Thornton
We describe a novel inlet that allows measurement of both gas and particle molecular composition when coupled to mass spectrometric, chromatographic, or optical sensors: the Filter Inlet for Gases and AEROsols (FIGAERO). The design goals for the FIGAERO are to allow unperturbed observation of ambient air while simultaneously analyzing gases and collecting particulate matter on a Teflon® (hereafter Teflon) filter via an entirely separate sampling port. The filter is analyzed periodically by the same sensor on hourly or faster timescales using temperature-programmed thermal desorption. We assess the performance of the FIGAERO by coupling it to a high-resolution time-of-flight chemical-ionization mass spectrometer (HRToF-CIMS) in laboratory chamber studies of α-pinene oxidation and field measurements at a boreal forest location. Low instrument backgrounds give detection limits of ppt or lower for compounds in the gas-phase and in the picogram m−3 range for particle phase compounds. The FIGAERO-HRToF-CIMS provides molecular information about both gases and particle composition on the 1 Hz and hourly timescales, respectively for hundreds of compounds. The FIGAERO thermal desorptions are highly reproducible (better than 10%), allowing a calibrated assessment of the effective volatility of desorbing compounds and the role of thermal decomposition during the desorption process. We show that the often multi-modal desorption thermograms arising from secondary organic aerosol (SOA) provide additional insights into molecular composition and/or particle morphology, and exhibit changes with changes in SOA formation or aging pathways.

15 February 2012 in Atmospheric Chemistry and Physics
Verified
Journal Article
Open access
PDF file
CMC. Mohr
C. Mohr
PDP. F. DeCarlo
P. F. DeCarlo
MHM. F. Heringa
M. F. Heringa
RCR. Chirico
R. Chirico
JSJ. G. Slowik
J. G. Slowik
APA. S. H. Prévôt
A. S. H. Prévôt
PM1 (particulate matter with an aerodynamic diameter <1 μm) non-refractory components and black carbon were measured continuously together with additional air quality and atmospheric parameters at an urban background site in Barcelona, Spain, during March 2009 (campaign DAURE, Determination of the sources of atmospheric Aerosols in Urban and Rural Environments in the western Mediterranean). Positive matrix factorization (PMF) was conducted on the organic aerosol (OA) data matrix measured by an aerosol mass spectrometer, on both unit mass (UMR) and high resolution (HR) data. Five factors or sources could be identified: LV-OOA (low-volatility oxygenated OA), related to regional, aged secondary OA; SV-OOA (semi-volatile oxygenated OA), a fresher oxygenated OA; HOA (hydrocarbon-like OA, related to traffic emissions); BBOA (biomass burning OA) from domestic heating or agricultural biomass burning activities; and COA (cooking OA). LV-OOA contributed 28% to OA, SV-OOA 27%, COA 17%, HOA 16%, and BBOA 11%. The COA HR spectrum contained substantial signal from oxygenated ions (O:C: 0.21) whereas the HR HOA spectrum had almost exclusively contributions from chemically reduced ions (O:C: 0.03). If we assume that the carbon in HOA is fossil while that in COA and BBOA is modern, primary OA in Barcelona contains a surprisingly high fraction (59%) of non-fossil carbon. This paper presents a method for estimating cooking organic aerosol in ambient datasets based on the fractions of organic mass fragments at m/z 55 and 57: their data points fall into a V-shape in a scatter plot, with strongly influenced HOA data aligned to the right arm and strongly influenced COA data points aligned to the left arm. HR data show that this differentiation is mainly driven by the oxygen-containing ions C3H3O+ and C3H5O+, even though their contributions to m/z 55 and 57 are low compared to the reduced ions C4H7+ and C4H9+. A simple estimation method based on the markers m/z 55, 57, and 44 is developed here and allows for a first-order-estimation of COA in urban air. This study emphasizes the importance of cooking activities for ambient air quality and confirms the importance of chemical composition measurements with a high mass and time resolution.

23 January 2013 in Atmospheric Chemistry and Physics
Verified
Journal Article
Open access
PDF file
MCM. Crippa
M. Crippa
PDP. F. DeCarlo
P. F. DeCarlo
JSJ. G. Slowik
J. G. Slowik
CMC. Mohr
C. Mohr
MHM. F. Heringa
M. F. Heringa
UBU. Baltensperger
U. Baltensperger
The effect of a post-industrial megacity on local and regional air quality was assessed via a month-long field measurement campaign in the Paris metropolitan area during winter 2010. Here we present source apportionment results from three aerosol mass spectrometers and two aethalometers deployed at three measurement stations within the Paris region. Submicron aerosol composition is dominated by the organic fraction (30–36%) and nitrate (28–29%), with lower contributions from sulfate (14–16%), ammonium (12–14%) and black carbon (7–13%). Organic source apportionment was performed using positive matrix factorization, resulting in a set of organic factors corresponding both to primary emission sources and secondary production. The dominant primary sources are traffic (11–15% of organic mass), biomass burning (13–15%) and cooking (up to 35% during meal hours). Secondary organic aerosol contributes more than 50% to the total organic mass and includes a highly oxidized factor from indeterminate and/or diverse sources and a less oxidized factor related to wood burning emissions. Black carbon was apportioned to traffic and wood burning sources using a model based on wavelength-dependent light absorption of these two combustion sources. The time series of organic and black carbon factors from related sources were strongly correlated. The similarities in aerosol composition, total mass and temporal variation between the three sites suggest that particulate pollution in Paris is dominated by regional factors, and that the emissions from Paris itself have a relatively low impact on its surroundings.

4 March 2009 in Environmental Science & Technology
Verified
Journal Article
Closed access
CMClaudia Mohr
Claudia Mohr
JHJ. Alex Huffman
J. Alex Huffman
MCMichael J. Cubison
Michael J. Cubison
Allison C. AikenAllison C. Aiken
Allison C. Aiken
KDKenneth S. Docherty
Kenneth S. Docherty
JJJose L. Jimenez
Jose L. Jimenez