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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 />

D8 2015 3.0 Included Sulfate microphysics with SO 2 gas-to-particle<br />

D9 2050 2.0 Included SA0<br />

conversion of 100%<br />

The following heterogeneous reactions were identified in DeMore et al. (1997) as possible reactions on sulfate or PSC. Most models assume that <strong>the</strong> rate constant is in<br />

<strong>the</strong> form gvA/4, where g is <strong>the</strong> reaction probability, v is <strong>the</strong> <strong>the</strong>rmal velocity of <strong>the</strong> reactant, <strong>and</strong> A is <strong>the</strong> surface area of <strong>the</strong> sulfate or PSC.<br />

N 2 O 5 + H 2 O 2HNO 3<br />

ClONO 2 + H 2 O HNO 3 +<br />

HOCl<br />

BrONO2 + H2O HNO3 +<br />

HOBr<br />

ClONO 2 + HCl HNO 3 + Cl 2<br />

HOCl + HCl Cl 2 + H 2 O<br />

HOBr + HCl BrCl + H 2 O<br />

These reactions occur on <strong>the</strong> surface of particles (sulfate or PSC). In addition, all but two of <strong>the</strong> nine models (LLNL <strong>and</strong> UNIVAQ) include <strong>the</strong> reaction N2O5 + HCl '<br />

HNO3 + ClNO2 on PSC. In most cases, H2O <strong>and</strong> HCl molecules are adsorbed or dissolved in <strong>the</strong> particles, <strong>and</strong> <strong>the</strong> reaction proceeds as <strong>the</strong> o<strong>the</strong>r reactant collides<br />

with <strong>the</strong> particle. There are slight variations in <strong>the</strong> temperature dependence of g for reactions on sulfate particles used in <strong>the</strong> various models. Previous analyses<br />

(Murphy <strong>and</strong> Ravishankara, 1994; Borrmann et al., 1997; Michelsen et al., 1999) have shown that g is very sensitive to temperature for some reactions. As <strong>the</strong> air<br />

parcel goes around <strong>the</strong> globe, it experiences temperatures that are both lower <strong>and</strong> higher than <strong>the</strong> zonal mean temperature. Ignoring zonal asymmetry in temperature<br />

by using zonal mean values in calculations may underestimate <strong>the</strong> O3 impact from HSCT (Pitari et al., 1993; Considine et al., 1994; Grooß et al. 1994; Weisenstein et<br />

al., 1998). Because <strong>the</strong> sulfate surface area is specified in <strong>the</strong> calculations, <strong>the</strong> temperature-dependence comes from g <strong>and</strong> v. Some models compute an effective gv<br />

based on a temperature-weighted g <strong>and</strong> v from zonal-mean temperature, whereas o<strong>the</strong>r models compute a temperature-weighted product of gv. Some of <strong>the</strong> listed<br />

reactions also occur on type I PSCs (assumed to be nitric acid trihydrate (NAT)) or type II PSCs (assumed to be "ice"). Exact treatments in each model vary; see <strong>the</strong><br />

Technical Report on Supersonic Aircraft Effects for details.<br />

4.3.2. Definition of Scenarios<br />

http://www.ipcc.ch/ipccreports/sres/aviation/049.htm (5 von 13)08.05.2008 02:42:26

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