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Transport patterns of global aviation NO<sub><i>x</i></sub> and their short-term O<sub>3</sub> radiative forcing – a machine learning approach
oleh: J. Maruhashi, V. Grewe, V. Grewe, C. Frömming, P. Jöckel, I. C. Dedoussi
| Format: | Article |
|---|---|
| Diterbitkan: | Copernicus Publications 2022-11-01 |
Deskripsi
<p>Aviation produces a net climate warming contribution that comprises multiple forcing terms of mixed sign. Aircraft NO<span class="inline-formula"><sub><i>x</i></sub></span> emissions are associated with both warming and cooling terms, with the short-term increase in O<span class="inline-formula"><sub>3</sub></span> induced by NO<span class="inline-formula"><sub><i>x</i></sub></span> emissions being the dominant warming effect. The uncertainty associated with the magnitude of this climate forcer is amongst the highest out of all contributors from aviation and is owed to the nonlinearity of the NO<span class="inline-formula"><sub><i>x</i></sub></span>–O<span class="inline-formula"><sub>3</sub></span> chemistry and the large dependency of the response on space and time, i.e., on the meteorological condition and background atmospheric composition. This study addresses how transport patterns of emitted NO<span class="inline-formula"><sub><i>x</i></sub></span> and their climate effects vary with respect to regions (North America, South America, Africa, Eurasia and Australasia) and seasons (January–March and July–September in 2014) by employing global-scale simulations. We quantify the climate effects from NO<span class="inline-formula"><sub><i>x</i></sub></span> emissions released at a representative aircraft cruise altitude of 250 hPa (<span class="inline-formula">∼10 400</span> m) in terms of radiative forcing resulting from their induced short-term contributions to O<span class="inline-formula"><sub>3</sub></span>. The emitted NO<span class="inline-formula"><sub><i>x</i></sub></span> is transported with Lagrangian air parcels within the ECHAM5/MESSy Atmospheric Chemistry (EMAC) model. To identify the main global transport patterns and associated climate impacts of the 14 000 simulated air parcel trajectories, the unsupervised QuickBundles clustering algorithm is adapted and applied. Results reveal a strong seasonal dependence of the contribution of NO<span class="inline-formula"><sub><i>x</i></sub></span> emissions to O<span class="inline-formula"><sub>3</sub></span>. For most regions, an inverse relationship is found between an air parcel's downward transport and its mean contribution to O<span class="inline-formula"><sub>3</sub></span>. NO<span class="inline-formula"><sub><i>x</i></sub></span> emitted in the northern regions (North America and Eurasia) experience the longest residence times in the upper midlatitudes (40 %–45 % of their lifetime), while those beginning in the south (South America, Africa and Australasia) remain mostly in the Tropics (45 %–50 % of their lifetime). Due to elevated O<span class="inline-formula"><sub>3</sub></span> sensitivities, emissions in Australasia induce the highest overall radiative forcing, attaining values that are larger by factors of 2.7 and 1.2 relative to Eurasia during January and July, respectively. The location of the emissions does not necessarily correspond to the region that will be most affected – for instance, NO<span class="inline-formula"><sub><i>x</i></sub></span> over North America in July will induce the largest radiative forcing in Europe. Overall, this study highlights the spatially and temporally heterogeneous nature of the NO<span class="inline-formula"><sub><i>x</i></sub></span>–O<span class="inline-formula"><sub>3</sub></span> chemistry from a global perspective, which needs to be accounted for in efforts to minimize aviation's climate impact, given the sector's resilient growth.</p>