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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • ship emissions
  • plume chemistry
  • ITCT 2002

Index Terms

  • Atmospheric Composition and Structure: Constituent sources and sinks
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Atmospheric Composition and Structure: Aerosols and particles
Abstract
Cited By (4)
 

Abstract

An investigation of the chemistry of ship emission plumes during ITCT 2002

G. Chen

NASA Langley Research Center, Hampton, Virginia, USA

L. G. Huey

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

M. Trainer

Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA

D. Nicks

Ball Aerospace, Boulder, Colorado, USA

J. Corbett

Marine Policy Program, Graduate College of Marine Studies, University of Delaware, Newark, Delaware, USA

T. Ryerson

Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA

D. Parrish

Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA

J. A. Neuman

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

J. Nowak

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

D. Tanner

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

J. Holloway

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

C. Brock

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

J. Crawford

NASA Langley Research Center, Hampton, Virginia, USA

J. R. Olson

NASA Langley Research Center, Hampton, Virginia, USA

A. Sullivan

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

R. Weber

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

S. Schauffler

Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA

S. Donnelly

Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA

E. Atlas

Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA

J. Roberts

Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA

F. Flocke

Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA

G. Hübler

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

F. Fehsenfeld

Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA

A ship emission plume experiment was conducted about 100 km off the California coast during the NOAA Intercontinental Transport and Chemical Transformation (ITCT) 2K2 airborne field campaign. Measurements of chemical species were made from the NOAA WP-3D aircraft in eight consecutive transects of a ship plume around midday during 2.5 hours of flight. The measured species include NOx, HNO3, peroxyacetylnitrate (PAN), SO2, H2SO4, O3, CO, CO2, nonmethane hydrocarbons (NMHC), and particle number and size distributions. Observations demonstrate a NOx lifetime of ∼1.8 hours inside the ship plume compared to ∼6.5 hours (at noontime) in the moderately polluted background marine boundary layer of the experiment. This confirms the earlier hypothesis of highly enhanced in-plume NOx destruction. Consequently, one would expect the impact of ship emissions is much less severe than those predicted by global models that do not include rapid NOx destruction. Photochemical model calculations suggest that more than 80% of the NOx loss was due to the NO2 + OH reaction; the remainder was by PAN formation. The model underestimated in-plume NOx loss rate by about 30%. In addition, a comparison of measured to predicted H2SO4 in the plumes suggests that the photochemical model predicts OH variability reasonably well but may underestimate actual values. Predictions of in-plume O3 production agree well with the observations, suggesting that model-predicted peroxy radical (HO2 + RO2) levels are reasonable. The model estimated ozone production efficiency ranges from 6 to 30. The largest model bias was seen in the comparison with measured HNO3. The model overestimated in-plume HNO3 by about a factor of 6. This is most likely caused by underestimated HNO3 sinks possibly involving particle scavenging. However, limited data availability precluded a conclusive test of this possible loss process.

Received 15 July 2004; accepted 28 December 2004; published 20 May 2005.

Citation: Chen, G., et al. (2005), An investigation of the chemistry of ship emission plumes during ITCT 2002, J. Geophys. Res., 110, D10S90, doi:10.1029/2004JD005236.

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