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Aviation and the Global Atmosphere

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

This section describes <strong>the</strong> scenarios for supersonic aircraft in 2015 <strong>and</strong> 2050 that were evaluated for this assessment. The premise for <strong>the</strong> future supersonic (proposed<br />

hypo<strong>the</strong>tical HSCT) aircraft fleet is given in Chapter 9, along with descriptions of actual emissions databases. A subsonic fleet is included in all scenarios but is<br />

modified when an HSCT fleet is also present. The background atmosphere for <strong>the</strong> model scenarios was appropriate to ei<strong>the</strong>r 2015 or 2050, though parametric studies<br />

of reactive chlorine (Cl y ) concentration <strong>and</strong> background SAD were also performed.<br />

4.3.2.1. Background <strong>Atmosphere</strong>s<br />

Boundary conditions for <strong>the</strong> background atmosphere for long-lived gases for 1992, 2015, <strong>and</strong> 2050 (Table 4-8) are based on <strong>the</strong> IPCC IS92a scenario (IPCC, 1992,<br />

1995). The boundary conditions used for halocarbons correspond to (a) 3.7, 3.0, <strong>and</strong> 2.0 ppbv of Cl y in <strong>the</strong> upper stratosphere at 50 km at <strong>the</strong> Equator for 1992, 2015,<br />

<strong>and</strong> 2050, respectively; <strong>and</strong> (b) 15, 12.5, <strong>and</strong> 11.1 pptv of reactive bromine (Br y ) in <strong>the</strong> upper stratosphere at 50 km at <strong>the</strong> Equator for 1992, 2015, <strong>and</strong> 2050,<br />

respectively.<br />

Background sulfate SAD was supplied for <strong>the</strong> unperturbed stratospheric aerosol case as described in Table 8-8 in WMO (1992). This case is designated SA0 aerosols.<br />

To approximate <strong>the</strong> effects of an active period of volcanic eruptions (e.g., <strong>the</strong> past 2 decades), some scenarios also evaluate <strong>the</strong> effects of 4xSA0. Treatments of PSCs<br />

<strong>and</strong> associated chemical <strong>and</strong> dynamical processes differ among models.<br />

4.3.2.2. Aircraft Emission Scenarios<br />

Table 4-11: Percentage changes in total column ozone for each assessment model. The top value is for <strong>the</strong> Nor<strong>the</strong>rn Hemisphere average; <strong>the</strong> bottom value is for <strong>the</strong><br />

Sou<strong>the</strong>rn Hemisphere average. The cruise altitude for most HSCT scenarios is at a st<strong>and</strong>ard (Std) height. Source gas boundary conditions are for <strong>the</strong> year 2015.<br />

Model results have been rounded off to one significant figure for clarity.<br />

IPCC<br />

Scenario<br />

S1a<br />

No H 2 O<br />

S1b<br />

H 2 O only<br />

S1c<br />

S1d<br />

S1e<br />

Cly (ppbv)<br />

3.0<br />

3.0<br />

3.0<br />

3.0<br />

3.0<br />

Fleet<br />

Size<br />

500<br />

500<br />

500<br />

500<br />

500<br />

EI(NO x ) Altitude<br />

(km)<br />

5<br />

0<br />

5<br />

10<br />

15<br />

Std<br />

Std<br />

Std<br />

Std<br />

Std<br />

http://www.ipcc.ch/ipccreports/sres/aviation/049.htm (6 von 13)08.05.2008 02:42:26<br />

SAD Desc. Ref.<br />

Atm.<br />

SA0<br />

SA0<br />

SA0<br />

SA0<br />

SA0<br />

D<br />

D<br />

D<br />

D<br />

D<br />

AER -2D GSFC-2D UNIVAQ-2D LLNL-2D CSIRO-2D THINAIR-2D SLIMCAT-3D SCTM1-3D LARC-3D<br />

-0.07<br />

-0.03<br />

-0.6<br />

-0.3<br />

-0.3<br />

-0.1<br />

-0.3<br />

-0.1<br />

-0.3<br />

-0.05<br />

-0.1<br />

+0.03<br />

-0.4<br />

-0.8<br />

-0.4<br />

-0.8<br />

-0.6<br />

-0.7<br />

-0.8<br />

-0.7<br />

+0.2<br />

+0.1<br />

-0.4<br />

-0.2<br />

-0.002<br />

+0.02<br />

+0.2<br />

+0.1<br />

+0.4<br />

+0.2<br />

-0.01<br />

+0.1<br />

-0.3<br />

-0.3<br />

-0.2<br />

-0.2<br />

-0.3<br />

-0.1<br />

-0.4<br />

-0.01<br />

-0.09<br />

-0.07<br />

-0.3<br />

-0.07<br />

-0.2<br />

-0.1<br />

-0.3<br />

-0.2<br />

-0.5<br />

-0.3<br />

-<br />

-<br />

-<br />

-<br />

-0.2<br />

-0.2<br />

-0.5<br />

-0.3<br />

-0.9<br />

-0.5<br />

-0.2<br />

-0.09<br />

-0.6<br />

-0.7<br />

-0.4<br />

-0.6<br />

-0.5<br />

-0.7<br />

-<br />

-<br />

-0.2<br />

-0.007<br />

-<br />

-<br />

-0.3<br />

-0.1<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-0.05<br />

-0.1<br />

+0.07<br />

-0.03<br />

-<br />

-

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