Dentener, F and Stevenson, D and Ellingsen, K and van Noije, T and Schultz, M and Amann, M and Atherton, C and Bell, N and Bergmann, D and Bey, I and Bouwman, L and Butler, T and Cofala, J and Collins, B and Drevet, J and Doherty, R and Eickhout, B and Eskes, H and Fiore, A and Gauss, M and Hauglustaine, D and Horowitz, L and Isaksen, I S A and Josse, B and Lawrence, M and Krol, M and Lamarque, J F and Montanaro, V and Muller, J F and Peuch, V H and Pitari, G and Pyle, J and Rast, S and Rodriguez, J and Sanderson, M and Savage, N H and Shindell, D and Strahan, S and Szopa, S and Sudo, K and Van Dingenen, R and Wild, O and Zeng, G (2006) The global atmospheric environment for the next generation. Environmental Science and Technology, 40 (11). pp. 3586-3594. ISSN 0013-936XFull text not available from this repository.
Air quality, ecosystem exposure to nitrogen deposition, and climate change are intimately coupled problems: we assess changes in the global atmospheric environment between 2000 and 2030 using 26 state-of-the-art global atmospheric chemistry models and three different emissions scenarios. The first (CLE) scenario reflects implementation of current air quality legislation around the world, while the second (MFR) represents a more optimistic case in which all currently feasible technologies are applied to achieve maximum emission reductions. We contrast these scenarios with the more pessimistic IPCC SRES A2 scenario. Ensemble simulations for the year 2000 are consistent among models and show a reasonable agreement with surface ozone, wet deposition, and NO2 satellite observations. Large parts of the world are currently exposed to high ozone concentrations and high deposition of nitrogen to ecosystems. By 2030, global surface ozone is calculated to increase globally by 1.5 +/- 1.2 ppb (CLE) and 4.3 +/- 2.2 ppb (A2), using the ensemble mean model results and associated +/- 1 sigma standard deviations. Only the progressive MFR scenario will reduce ozone, by -2.3 +/- 1.1 ppb. Climate change is expected to modify surface ozone by -0.8 +/- 0.6 ppb, with larger decreases over sea than over land. Radiative forcing by ozone increases by 63 +/- 15 and 155 +/- 37 mW m(-2) for CLE and A2, respectively, and decreases by -45 +/- 15 mW m(-2) for MFR. We compute that at present 10.1% of the global natural terrestrial ecosystems are exposed to nitrogen deposition above a critical load of 1 g N m(-2) yr(-1). These percentages increase by 2030 to 15.8% (CLE), 10.5% (MFR), and 25% (A2). This study shows the importance of enforcing current worldwide air quality legislation and the major benefits of going further. Nonattainment of these air quality policy objectives, such as expressed by the SRES-A2 scenario, would further degrade the global atmospheric environment.
|Journal or Publication Title:||Environmental Science and Technology|
|Uncontrolled Keywords:||NITROGEN DEPOSITION ; TROPOSPHERIC OZONE ; SURFACE OZONE ; IMPACT ; AFRICA|
|Departments:||Faculty of Science and Technology > Lancaster Environment Centre|
|Deposited On:||07 Sep 2011 11:35|
|Last Modified:||24 Jan 2017 02:07|
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