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 />

Box 1-3. Time Scales in <strong>Aviation</strong> <strong>and</strong> <strong>the</strong> <strong>Atmosphere</strong><br />

Underst<strong>and</strong>ing <strong>the</strong> time scales of <strong>the</strong> processes involved is important in assessing <strong>the</strong> impact aviation can have on <strong>the</strong> atmosphere now <strong>and</strong> in <strong>the</strong> future. It<br />

takes many years for a new aircraft design to progress from <strong>the</strong> drawing board into service. Once aircraft are operative, <strong>the</strong>ir emissions remain in <strong>the</strong><br />

atmosphere for periods ranging from days to centuries, with some climatic effects felt on even longer time scales. Fur<strong>the</strong>rmore, although new technologies<br />

would have an immediate effect on emissions from new aircraft, any impact on <strong>the</strong> global abundance of short-lived atmospheric constituents would be limited<br />

by <strong>the</strong> rate of introduction of <strong>the</strong> new technology into <strong>the</strong> global fleet. A rough idea of <strong>the</strong> various time scales involved is provided. The processes that remove<br />

trace species from <strong>the</strong> atmosphere can be chemical (e.g., <strong>the</strong> oxidation of methane), physical (e.g., in rain or by dry deposition onto l<strong>and</strong> or sea), or biological<br />

(e.g., <strong>the</strong> uptake of CO 2 by plants). The rate of each process typically varies with season <strong>and</strong> location in <strong>the</strong> atmosphere. These rates can be combined to<br />

produce a rough estimate of how long each constituent remains in <strong>the</strong> atmosphere. A constituent with a short lifetime responds quickly to any change in<br />

emissions. A trace species with a long lifetime responds slowly to a change in emissions. The atmospheric effects of H 2 O, NO x , SO x O, <strong>and</strong> soot are all<br />

relatively short-lived. Broadly speaking, <strong>the</strong> tropospheric lifetimes of <strong>the</strong>se constituents are a couple of weeks or less; that of any ozone produced by NO x is a<br />

month or so. The stratospheric time scales involved are longer but are all well under a decade. By contrast, emissions of carbon dioxide affect <strong>the</strong><br />

atmosphere for a long time (about 100 years), with little difference for emissions into <strong>the</strong> stratosphere or troposphere. The main factors affecting how quickly<br />

new aircraft are introduced are technological feasibility, certification, <strong>and</strong> commercial viability. Typically, new technology is likely to be a decade in its<br />

gestation, although this time scale may be reduced if <strong>the</strong>re are significant market opportunities. The project launch of a new aircraft type by an airframe<br />

manufacturer is normally concurrent with <strong>the</strong> launch of new engines supplied by competing manufacturers. Development of <strong>the</strong> engine culminates in<br />

airworthiness <strong>and</strong> emissions certification, usually 3-5 years later-but <strong>the</strong> time scale for entry into service is dictated by <strong>the</strong> airframe manufacturer <strong>and</strong> its<br />

customer airlines. Once <strong>the</strong> engine has achieved airworthiness certification, it is installed on <strong>the</strong> airframe, <strong>and</strong> <strong>the</strong> aircraft typically <strong>the</strong>n takes ano<strong>the</strong>r year to<br />

complete <strong>the</strong> airworthiness <strong>and</strong> noise certification process before initial deliveries are made to customers. With commercial airlines, individual aircraft will<br />

operate for 25 years or more in revenue service. A good product, including its derivatives, will have a substantial production period (possibly 25 years or<br />

longer); <strong>the</strong>refore, <strong>the</strong> overall time scale between introduction into service of an aircraft type <strong>and</strong> withdrawal from service may exceed 50 years. Development<br />

of <strong>the</strong> infrastructure for air transportation (airports, air traffic control, etc.) can take years or even decades. This development is driven by overall increased<br />

dem<strong>and</strong> for air transportation, both for passengers <strong>and</strong> freight. It is limited by <strong>the</strong> availability of financial resources <strong>and</strong> local environmental concerns about<br />

noise <strong>and</strong> increased ground traffic around new or exp<strong>and</strong>ed airports.<br />

The future growth of aviation will depend heavily on factors such as economic growth (at global <strong>and</strong> regional levels), <strong>the</strong> dem<strong>and</strong> for travel (in an age of rapid advances<br />

in information technology), <strong>the</strong> development of infrastructure to support air travel <strong>and</strong> available flight technology, <strong>and</strong> <strong>the</strong> availability <strong>and</strong> cost of fuel. Increases in<br />

dem<strong>and</strong> will not translate directly into increases in emissions. Changes in engine efficiency, airplane design (size <strong>and</strong> shape), <strong>and</strong> operational practice are all expected<br />

to lead to more efficient use of fuel because <strong>the</strong>re are strong commercial reasons for airlines <strong>and</strong> o<strong>the</strong>r operators to keep fuel costs down.<br />

The scenarios used in this report have been developed using models of passenger dem<strong>and</strong> on a regional <strong>and</strong> global basis that assume future economic growth rates<br />

as found in <strong>the</strong> IS92 scenarios (particularly IS92a). In all cases, it is assumed that infrastructure (e.g., airports) <strong>and</strong> technology will be developed so that this growth is<br />

not constrained. Different aircraft types <strong>and</strong> fuel use are included, so CO 2 <strong>and</strong> H 2 O emissions-which depend solely on <strong>the</strong> amount of fuel burned-can be calculated<br />

directly. SO 2 emissions are estimated simply by assuming what <strong>the</strong> sulfur composition in <strong>the</strong> fuel will be. Emissions of NO x , CO, <strong>and</strong> hydrocarbons depend strongly on<br />

combustor technology-particularly <strong>the</strong> mixing of fuel <strong>and</strong> air in <strong>the</strong> combustion chamber, as well as temperature <strong>and</strong> pressure. These emissions are estimated using<br />

semi-empirical relationships between in-flight fuel flow <strong>and</strong> emissions of NO x , CO, <strong>and</strong> hydrocarbons derived from ICAO engine certifications toge<strong>the</strong>r with determined<br />

flight patterns. Emissions of all of <strong>the</strong>se compounds for global air traffic are produced on a 3-D grid (latitude, longitude, altitude) that can be used in global atmospheric<br />

models. Little equivalent information regarding emissions exists for particulates o<strong>the</strong>r than total sulfur emissions.<br />

http://www.ipcc.ch/ipccreports/sres/aviation/017.htm (2 von 3)08.05.2008 02:41:31

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

Saved successfully!

Ooh no, something went wrong!