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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 />

in this context refers to an atmosphere derived from a calculation that includes all expected<br />

inputs o<strong>the</strong>r than those attributable to aircraft emissions. The calculated impacts of aviation<br />

on ozone for 1992, 2015, <strong>and</strong> 2050 are provided by Chapter 4. The small effect calculated<br />

for 1970 is deduced from <strong>the</strong> 1992 calculations, as discussed in Section 5.4.1.2.<br />

The starting point for subsequent calculations is <strong>the</strong> representation of ozone columns <strong>and</strong><br />

profiles for 1992. For this chapter, <strong>the</strong> columns have been derived from archived TOMS<br />

version 7 measurements (Herman et al., 1996). UV calculations have been performed at<br />

local noon for January, April, July, <strong>and</strong> October at <strong>the</strong> following latitudes: 65°S, 45°S, 30°S,<br />

0, 30°N, 45°N, <strong>and</strong> 65°N. The monthly averaged <strong>and</strong> zonally averaged ozone columns<br />

derived from <strong>the</strong> TOMS data for <strong>the</strong>se months <strong>and</strong> latitudes for <strong>the</strong> 10-year period 1983 to<br />

1992 are shown in Table 5-1.<br />

Because <strong>the</strong> values shown in Table 5-1 are averages of measured values, <strong>the</strong>y already<br />

include <strong>the</strong> effects of present-day aircraft emissions on ozone. In o<strong>the</strong>r words, to obtain <strong>the</strong><br />

1992 background atmosphere, <strong>the</strong> effects of emissions from aircraft have to be removed<br />

from <strong>the</strong> values shown in Table 5-1. The manner in which this has been done for <strong>the</strong>se<br />

calculations <strong>and</strong> <strong>the</strong> extension of <strong>the</strong> methods applied to obtain <strong>the</strong> required information for<br />

<strong>the</strong> years 1970, 2015, <strong>and</strong> 2050 are illustrated in Figure 5-3.<br />

Figure 5-3: Illustration of <strong>the</strong> derivation of columns used for UV<br />

All calculations ultimately have averaged values for ozone given in Table 5-1 as <strong>the</strong>ir<br />

calculations.<br />

reference. These 1992 values are represented by 1992ss (where <strong>the</strong> subscript defines an<br />

atmosphere containing emissions from a fleet of subsonic aircraft) in Figure 5-3. Chemical transport calculations are carried out to generate model atmospheres for<br />

1992 that (a) do not include inputs attributable to aviation <strong>and</strong> (b) do include <strong>the</strong>se inputs. Comparison of <strong>the</strong> results of <strong>the</strong>se calculations allows one to determine <strong>the</strong><br />

absolute differences in ozone concentrations predicted by <strong>the</strong> model.<br />

Table 5-2: Brief scenario description.<br />

http://www.ipcc.ch/ipccreports/sres/aviation/059.htm (3 von 7)08.05.2008 02:42:41

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