2018
DOI: 10.5194/acp-18-16979-2018
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Elucidating real-world vehicle emission factors from mobile measurements over a large metropolitan region: a focus on isocyanic acid, hydrogen cyanide, and black carbon

Abstract: A mobile laboratory equipped with state-of-the-art gaseous and particulate instrumentation was deployed across the Greater Toronto Area (GTA) during two seasons. A high-resolution time-of-flight chemical ionization mass spectrometer (HR-TOF-CIMS) measured isocyanic acid (HNCO) and hydrogen cyanide (HCN), and a high-sensitivity laserinduced incandescence (HS-LII) instrument measured black carbon (BC). Results indicate that on-road vehicles are a clear source of HNCO and HCN and that their impact is more pronoun… Show more

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Cited by 24 publications
(19 citation statements)
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References 111 publications
(191 reference statements)
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“…This instrument also uses so ionisation through proton transfer but from hydronium ions (H 3 O + ) and can detect HNCO mixing ratios from low ppbv up to 1000s of ppbv. [23][24][25][51][52][53] Online CIMS techniques with acetate and iodide reagent ions and PTR-MS instruments have facilitated atmospheric measurements of HNCO providing observations from eld campaigns from 10 locations across three continents (Pasadena, California; 19 Erie, Colorado; 26,54 La Jolla, California; 55 Fort Collins, Colorado; 26 Toronto, Ontario; 30,56 Calgary, Alberta; 50 the marine boundary layer in the Canadian Arctic Archipelago; 57 Mohali, India; 51 Kathmandu Valley, Nepal; 52 and Manchester, UK 58 ) ( Table 1). The number of ambient measurements continues to grow, yet long term datasets are still missing (Fig.…”
Section: Ambient Measurementsmentioning
confidence: 99%
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“…This instrument also uses so ionisation through proton transfer but from hydronium ions (H 3 O + ) and can detect HNCO mixing ratios from low ppbv up to 1000s of ppbv. [23][24][25][51][52][53] Online CIMS techniques with acetate and iodide reagent ions and PTR-MS instruments have facilitated atmospheric measurements of HNCO providing observations from eld campaigns from 10 locations across three continents (Pasadena, California; 19 Erie, Colorado; 26,54 La Jolla, California; 55 Fort Collins, Colorado; 26 Toronto, Ontario; 30,56 Calgary, Alberta; 50 the marine boundary layer in the Canadian Arctic Archipelago; 57 Mohali, India; 51 Kathmandu Valley, Nepal; 52 and Manchester, UK 58 ) ( Table 1). The number of ambient measurements continues to grow, yet long term datasets are still missing (Fig.…”
Section: Ambient Measurementsmentioning
confidence: 99%
“…Wren et al (2018) conducted a mobile study using a CIMS operated in a mobile lab to measure real time HNCO and HCN mixing ratios of on-road vehicles. 56 They found that on-road vehicles were clear emitters of HNCO to the atmosphere, with higher emissions observed in winter than in summer. Algorithms were used to calculate both plume-based and timed-based emission factors from the combined diesel and gasoline emissions.…”
Section: Fossil Fuel Combustionmentioning
confidence: 99%
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“…The observational network was designed to provide environmental conditions at the sport venues sites and to capture meteorological patterns specific to Toronto, such as lake-breeze front tracking (as they can lead to high-impact weather or modify local conditions rapidly, e.g., Mariani et al, 2018), heat stress conditions (monitored by the Wet-Bulb Globe temperature -WBGT-index obtained with black globe thermometers measuring the radiant temperature, e.g., Herdt et al, 2018) or atmospheric pollution (e.g., using vehicle traverse sampling, Wren et al, 2018). Substantial time (years in some cases) was needed to obtain land use licenses or leases required for siting fixed stations.…”
Section: Enhancement Of Ius In the Context Of A Sport Event In Torontomentioning
confidence: 99%
“…They are both products of secondary formation in the atmosphere but are also directly emitted. The transportation sector is an important source of HNCO (Brady et al 2014;Wentzell et al 2013;Wren et al 2018), and emission rates were estimated from the aircraft measurements to be 2.2 ± 0.8 kg hr −1 from SUN, followed by that from the SML facility of 1.5 ± 0.5 kg hr −1 . Figures S3.2a and S3.2b show that by tracking a specific integrated plume downwind, increases in HNCO and LMWOAs can be observed (Liggio et al 2017).…”
Section: Validation Of Emissions From Aircraft Studiesmentioning
confidence: 99%