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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 />

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

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

2.3. Uncertainties in <strong>the</strong> Impact Assessment of Present <strong>Aviation</strong>: Implications for Use of Models in Predicting Future Change<br />

2.3.1. Uncertainties in Modeling <strong>Aviation</strong> Impacts<br />

2.3.1.1. Key Issues <strong>and</strong> Processes for Tropospheric Models<br />

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

In performing assessments of <strong>the</strong> impacts of subsonic aircraft NOx emissions on tropospheric composition, <strong>the</strong> modeling studies have pointed out several key issues<br />

<strong>and</strong> processes that have to be adequately addressed:<br />

Model spatial <strong>and</strong> time resolution<br />

Time resolution of meteorological data<br />

Subgrid-scale processes (e.g., plume processes)<br />

Tropospheric NO x <strong>and</strong> NOy sources<br />

Tropospheric gas-phase <strong>and</strong> heterogeneous chemistry<br />

Stratospheric gas-phase <strong>and</strong> heterogeneous chemistry<br />

Stratosphere-troposphere exchange<br />

Upper troposphere-lower stratosphere dynamics <strong>and</strong> convective transport<br />

Sources <strong>and</strong> sinks of water <strong>and</strong> NOy.<br />

These issues <strong>and</strong> processes are discussed in general terms in <strong>the</strong> paragraphs that follow. A detailed description of process representation in <strong>the</strong> assessment models<br />

is given in Chapter 4.<br />

Over <strong>the</strong> years, <strong>the</strong>re has been a steady increase in <strong>the</strong> spatial resolution of <strong>the</strong> models used in <strong>the</strong> assessment of subsonic aircraft impacts on tropospheric<br />

composition. Initially, <strong>the</strong> assessment models were one-dimensional (altitude), averaged around latitude circles <strong>and</strong> from north to south poles. Relatively quickly,<br />

researchers realized that interhemispheric gradients were crucial for ozone <strong>and</strong> anthropogenic trace gases, so much of <strong>the</strong> assessment work has been carried out with<br />

2-D (altitude <strong>and</strong> latitude) models that average around latitude circles. With NO x lifetimes of days or less <strong>and</strong> transport times around latitude circles of up to 2 weeks,<br />

http://www.ipcc.ch/ipccreports/sres/aviation/028.htm (1 von 11)08.05.2008 02:41:47

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