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J. S. Craven

Researcher at California Institute of Technology

Publications -  37
Citations -  3079

J. S. Craven is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Aerosol & Cloud condensation nuclei. The author has an hindex of 25, co-authored 37 publications receiving 2599 citations. Previous affiliations of J. S. Craven include University of British Columbia.

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Ship impacts on the marine atmosphere: insights into the contribution of shipping emissions to the properties of marine aerosol and clouds

TL;DR: In this article, the authors report properties of marine aerosol and clouds measured in the shipping lanes between Monterey Bay and San Francisco off the coast of Central California using a suite of aerosol instrumentation onboard the CIRPAS Twin Otter aircraft.
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Black Carbon Aerosol over the Los Angeles Basin during CalNex

TL;DR: This paper quantified the mixing state of rBC aerosols through modeling the scattering cross-section with a core-and-shell Mie model to determine coating thickness in the Los Angeles (LA) Basin.
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Investigating the links between ozone and organic aerosol chemistry in a biomass burning plume from a prescribed fire in California chaparral

TL;DR: In this paper, the authors use version 2.1 of the Aerosol Simulation Program (ASP) to simulate the evolution of ozone (O3) and secondary organic aerosol (SOA) within a young biomass burning smoke plume from the Williams prescribed fire in chaparral, which was sampled over California in November 2009.
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Chemical aging of m -xylene secondary organic aerosol: laboratory chamber study

TL;DR: In this article, the formation and evolution of secondary organic aerosol (SOA) from the photooxidation of m-xylene under low-NOx conditions and in the presence of either neutral or acidic seed particles is studied.
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Secondary Organic Aerosol Formation from Low-NOx Photooxidation of Dodecane: Evolution of Multigeneration Gas-Phase Chemistry and Aerosol Composition

TL;DR: Combination of these techniques reveals that particle-phase chemistry leading to peroxyhemiacetal formation is the likely mechanism by which these species are incorporated in the particle phase, relevant toward understanding atmospheric SOA formation and aging from the "unresolved complex mixture," comprising, in part, long-chain alkanes.