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Dive into the research topics where Michael K. Trainer is active.

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Featured researches published by Michael K. Trainer.


Journal of Geophysical Research | 1998

Measurements of PAN, PPN, and MPAN made during the 1994 and 1995 Nashville Intensives of the Southern Oxidant Study: Implications for regional ozone production from biogenic hydrocarbons

James M. Roberts; J. Williams; Karsten Baumann; M. P. Buhr; Paul D. Goldan; John S. Holloway; G. Hübler; William C. Kuster; S. A. McKeen; Thomas B. Ryerson; Michael K. Trainer; Eric J. Williams; F. C. Fehsenfeld; Steven B. Bertman; George Nouaime; Craig Seaver; Gil Grodzinsky; Michael O. Rodgers; V. Young

Isoprene and a variety of other reactive hydrocarbons are released in large quantities by vegetation in forested regions and are thought to participate in the NOx-catalyzed production of ozone, a serious air quality problem in North America and Europe [National Research Council, 1991]. The determination of the fraction of O3 formed from anthropogenic NOx and biogenic hydrocarbons (BHC) is a crucial step in the formulation of effective control strategies. Peroxymethacrylic nitric anhydride (MPAN, CH2C(CH3)C(O)OONO2) is formed almost entirely from the atmospheric oxidation of isoprene in the presence of NOx and is an excellent indicator of recent ozone production from isoprene and therefore biogenic hydrocarbons. Measurements are presented here of MPAN, peroxyacetic nitric anhydride (PAN, CH3C(O)OONO2), peroxypropionic nitric anhydride (PPN, CH3CH2C(O)OONO2) and ozone from separate data sets acquired during the 1994 and 1995 Nashville intensive studies of the Southern Oxidant Study. It was found that PAN, a general product of HC-NOx photochemistry, could be well represented as a simple linear combination of contributions from BHC and anthropogenic hydrocarbon (AHC) chemistries as indicated by MPAN and PPN, respectively. The PAN:MPAN ratios found to be characteristic of BHC-dominated chemistry ranged from 6 to 10. The PAN:PPN ratios found to be characteristic of AHC-dominated chemistry ranged from 5.8 to 7.4. These BHC and AHC attributions were used to estimate the contributions of anthropogenic and biogenic hydrocarbons to regional tropospheric ozone production, and substantial BHC-O3 (50–60 ppbv) was estimated in cases where high NOx from power plants was present in areas of high BHC emission. This estimation method provides direct evidence of significant photochemical ozone production from the oxidation of biogenic hydrocarbons in the presence of NOx.


Nature Geoscience | 2017

Transition from high- to low-NOx control of night-time oxidation in the southeastern US

P. M. Edwards; K. C. Aikin; William P. Dubé; Juliane L. Fry; J. B. Gilman; J. A. de Gouw; Martin Graus; T. F. Hanisco; John R. Holloway; G. Hübler; Jennifer Kaiser; Frank N. Keutsch; J. A. Neuman; D. D. Parrish; J. Peischl; I. B. Pollack; A. R. Ravishankara; James M. Roberts; T. B. Ryerson; Michael K. Trainer; P. R. Veres; G. M. Wolfe; Carsten Warneke; Steven S. Brown


Journal of Geophysical Research | 2012

Airborne and ground-based observations of a weekend effect in ozone, precursors, and oxidation products in the California South Coast Air Basin: SOCAB WEEKEND OZONE EFFECT

I. B. Pollack; T. B. Ryerson; Michael K. Trainer; D. D. Parrish; Arlyn Elizabeth Andrews; E. Atlas; D. R. Blake; Steven S. Brown; R. Commane; Bruce C. Daube; J. A. de Gouw; William P. Dubé; James Flynn; G. J. Frost; J. B. Gilman; N. Grossberg; John S. Holloway; Jonathan Kofler; Eric A. Kort; William C. Kuster; Patricia M. Lang; Barry Lee Lefer; R. A. Lueb; J. A. Neuman; J. B. Nowak; Paul C. Novelli; J. Peischl; A. E. Perring; James M. Roberts; Gregory W. Santoni


Archive | 2002

The Behavior of the Hydroxyl and Hydroperoxyl Radicals During PROPHET2000

Maria Martinez; H. Harder; William H. Brune; Pietro di Carlo; Edward J. Williams; Daniel Hereid; T. B. Jobson; William C. Kuster; Jay Roberts; Michael K. Trainer; F. C. Fehsenfeld; Spencer R. Hall; Richard E. Shetter; Eric C. Apel; Daniel D. Riemer; A. Geyer; J. Stutz; K. Baumann


Geophysical Research Letters | 2012

Gasoline emissions dominate over diesel in formation of secondary organic aerosol mass: GASOLINE DOMINATES SOA FORMATION

R. Bahreini; Ann M. Middlebrook; J. A. de Gouw; Carsten Warneke; Michael K. Trainer; C. A. Brock; Harald Stark; Steven S. Brown; William P. Dubé; J. B. Gilman; K. Hall; John S. Holloway; William C. Kuster; A. E. Perring; André S. H. Prévôt; J. P. Schwarz; J. R. Spackman; Soenke Szidat; N. L. Wagner; R. J. Weber; P. Zotter; D. D. Parrish


Archive | 2007

Determination of Biogenic Emissions from Aircraft Measurements During TEXAQS2006 and ICARTT2004 Campaigns and Comparison with Biogenic Emission Inventories

Carsten Warneke; S. A. McKeen; Joost A. de Gouw; Lori Ann del Negro; J. Brioude; Harald Stark; Michael K. Trainer; F. C. Fehsenfeld; Christine Wiedinmyer; U. Vanchindorj; Alex B. Guenther


Archive | 2004

Fast time resolution airborne measurements of PANs during the New England Air Quality Study 2004 intensive

F. M. Flocke; Aaron L. Swanson; Jay Roberts; Greg Huey; David J. Tanner; T. B. Ryerson; A. J. Neuman; John S. Holloway; J. A. Degouw; Carsten Warneke; Elliot Atlas; Stephen George Donnelly; Sue M. Schauffler; V. F. Stroud; Michael K. Trainer


Archive | 2002

Enhancement of VOCs in a Fresh and an Aged Forest Fire Plume

Carsten Warneke; Joost A. de Gouw; D. B. Parrish; John S. Holloway; T. B. Ryerson; D. K. Nicks; Michael K. Trainer; F. C. Fehsenfeld


Archive | 2002

Measurements of marine vessel emissions and resulting plume chemistry off of the California coast during ITCT 2002.

James J. Corbett; D. K. Nicks; John S. Holloway; T. B. Ryerson; J. A. Neuman; J. B. Nowak; C. A. Brock; Michael K. Trainer; G. Hübler; D. B. Parrish; Katherine King Perkins; E. J. Dunlea; Donna Sueper; F. C. Fehsenfeld


Journal of Geophysical Research | 2012

Observations of ozone transport from the free troposphere to the Los Angeles basin: OZONE TRANSPORT TO THE LOS ANGELES BASIN

J. A. Neuman; Michael K. Trainer; K. C. Aikin; Wayne M. Angevine; J. Brioude; Steven S. Brown; J. A. de Gouw; William P. Dubé; James Flynn; Martin Graus; John S. Holloway; Barry Lee Lefer; Philippe Nedelec; J. B. Nowak; D. D. Parrish; I. B. Pollack; James M. Roberts; T. B. Ryerson; H. Smit; V. Thouret; N. L. Wagner

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Dive into the Michael K. Trainer's collaboration.

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F. C. Fehsenfeld

National Oceanic and Atmospheric Administration

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Elliot Atlas

National Center for Atmospheric Research

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J. A. Neuman

Cooperative Institute for Research in Environmental Sciences

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J. B. Nowak

Langley Research Center

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Carsten Warneke

Cooperative Institute for Research in Environmental Sciences

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J. Peischl

Cooperative Institute for Research in Environmental Sciences

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F. M. Flocke

National Center for Atmospheric Research

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D. K. Nicks

National Oceanic and Atmospheric Administration

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Joost A. de Gouw

Cooperative Institute for Research in Environmental Sciences

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G. Hübler

National Oceanic and Atmospheric Administration

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