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Paul J. Crutzen

Researcher at Max Planck Society

Publications -  462
Citations -  87634

Paul J. Crutzen is an academic researcher from Max Planck Society. The author has contributed to research in topics: Stratosphere & Ozone. The author has an hindex of 130, co-authored 461 publications receiving 80651 citations. Previous affiliations of Paul J. Crutzen include University of Oxford & National Oceanic and Atmospheric Administration.

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Emissions of volatile organic compounds from Quercus ilex L. measured by Proton Transfer Reaction Mass Spectrometry under different environmental conditions

TL;DR: In this article, the authors used a fast Proton Transfer Reaction Mass Spectrometry (PTR-MS) instrument for analysis of the Mediterranean holm oak (Quercus ilex L).
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Average concentrations of OH in the troposphere, and the budgets of CH 4, CO, H 2 and CH 3CCl 3

TL;DR: An average tropospheric OH concentration in the Northern Hemisphere of about 3 × 105 cm −3 is not in disagreement with present photokinetic information as mentioned in this paper, implying an increase in H 2O concentrations and a decrease in ozone concentrations in the upper stratosphere.
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A model for studies of tropospheric ozone and nonmethane hydrocarbons: Model evaluation of ozone-related species

TL;DR: In this paper, a global three-dimensional model for studies of the tropospheric chemistry of H ox, ozone, and their precursors is thoroughly evaluated with available observations of 15 species from surface stations and/or aircraft campaigns.
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Mass-independent oxygen isotope fractionation in atmospheric CO as a result of the reaction CO + OH

TL;DR: The occurrence of mass-independent fractionation in the reaction of CO with OH raises fundamental questions about kinetic processes and is a useful marker for the degree to which CO in the atmosphere has been reacting with OH.
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Photochemically produced ozone in the emission from large-scale tropical vegetation fires

TL;DR: In this paper, an aircraft measurement program was undertaken in the savanna regions of central South America in the dry season of 1980 to investigate the atmospheric effects of large-scale biomass burning, and smoke from the fires was found to be largely confined within an approximately 3-km-deep boundary layer capped by a subsidence inversion or a stable layer.