13.12.2012 Views

Aviation and the Global Atmosphere

Aviation and the Global Atmosphere

Aviation and the Global Atmosphere

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

<strong>Aviation</strong> <strong>and</strong> <strong>the</strong> <strong>Global</strong> <strong>Atmosphere</strong><br />

<strong>Aviation</strong> <strong>and</strong> <strong>the</strong> <strong>Global</strong> <strong>Atmosphere</strong><br />

Table of contents | Previous page | Next page<br />

2.1. Relating Aircraft Emissions to Atmospheric Ozone<br />

2.1.1. Introduction<br />

O<strong>the</strong>r reports in this collection<br />

The chemical products of aircraft jet fuel combustion are emitted at <strong>the</strong> engine nozzle exit plane as part of a high-velocity plume. This gaseous <strong>and</strong> particulate stream<br />

is subject to chemical <strong>and</strong> dynamical processes that influence downstream composition. Eventually, plume constituents irreversibly mix with, <strong>and</strong> are diluted by,<br />

ambient air. Subsequently, some of <strong>the</strong> emitted species act in concert with o<strong>the</strong>r natural <strong>and</strong> anthropogenic chemicals to change ozone abundances in <strong>the</strong> Earth's<br />

atmosphere. The ultimate fates of <strong>the</strong>se aircraft-derived species are determined by larger-scale chemical <strong>and</strong> transport processes.<br />

Concerns about NO <strong>and</strong> NO2 (i.e., NOx ) emissions from present-generation subsonic <strong>and</strong> supersonic aircraft operating in <strong>the</strong> upper troposphere (UT) <strong>and</strong> lower<br />

stratosphere (LS) were raised more than 20 years ago by Hidalgo <strong>and</strong> Crutzen (1977) because <strong>the</strong>se emissions could change ozone levels locally by several percent<br />

or so. Despite extensive research <strong>and</strong> evaluation during <strong>the</strong> intervening years, WMO-UNEP (1995) concluded that assessments of ozone changes related to aviation<br />

remained uncertain <strong>and</strong> depended critically on NOx chemistry <strong>and</strong> its representation in complex models. Because of large uncertainties in present knowledge of <strong>the</strong><br />

tropospheric NO x budget, little confidence has been placed in previous assessments of quantitative model results of subsonic aircraft effects on atmospheric ozone.<br />

Assessment tools <strong>and</strong> <strong>the</strong>ir input data continue to improve, however, <strong>and</strong> reconsideration is appropriate in <strong>the</strong> light of <strong>the</strong> extensive research results published since<br />

<strong>the</strong> WMO-UNEP (1995) assessment.<br />

The research results published since <strong>the</strong> WMO-UNEP (1995) assessment have addressed a number of issues relevant to <strong>the</strong> assessment of ozone impacts of present<br />

aviation. These issues have included <strong>the</strong> development of improved aircraft NO x emission inventories, updating of evaluated chemical kinetic <strong>and</strong> photochemical<br />

databases, studies of aircraft plume chemistry, <strong>and</strong> <strong>the</strong> development of three-dimensional (3-D) modeling tools. Reviews have also been published of U.S. (Friedl,<br />

1997) <strong>and</strong> European (Schumann et al., 1997; Brasseur et al., 1998) research programs addressing ozone <strong>and</strong> o<strong>the</strong>r environmental impacts of present aviation.<br />

In this chapter we evaluate, from a qualitative <strong>and</strong> quantitative st<strong>and</strong>point, <strong>the</strong> impact on atmospheric ozone of aircraft exhaust species, emitted ei<strong>the</strong>r directly from<br />

engines or produced as secondary products of processes occurring in aircraft plumes. Our evaluation is based primarily on global model calculations ra<strong>the</strong>r than ozone<br />

trends because expected changes are not easily discerned from observations, as discussed below. We use intermodel comparisons <strong>and</strong> atmospheric observations of<br />

http://www.ipcc.ch/ipccreports/sres/aviation/022.htm (1 von 5)08.05.2008 02:41:36

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!