| HAL : hal-00671784, version 1 |
| Code Bibliographique ADS : 2010AGUFM.A43D0249G |
| Fiche détaillée | Récupérer au format |
|
|
| American Geophysical Union, Fall Meeting 2010, San Francisco : États-Unis (2010) |
|
|
|
|
| Evolution of anthropogenic emissions at the global and regional scale during the past three decades |
|
|
| Claire Granier 1, 2, 3B. Bessagnet 4 |
|
|
| (12/2010) |
|
|
| The knowledge of the distributions of surface emissions of gases and aerosols is essential for an accurate modeling and analysis of the distribution and evolution of the concentration of gaseous and particulate chemical species. The quantification of surface fluxes by source of origin is furthermore central to the assessment of effects and the development of control measures. Over the past few years, different ranges of emission fluxes have been proposed by several studies, which have provided emissions at different spatial and temporal scales. We have compared the emissions of several chemical compounds, i.e. carbon monoxide, nitrogen oxides, sulfur dioxide and black carbon, as provided by global and regional emissions inventories in different regions of the world for the past thirty years. The presentation will focus on the United States, Europe and China. Significant differences between the datasets providing emissions in these regions have been identified, reaching for example 60% and 35% for anthropogenic emissions of carbon monoxide and nitrogen oxides in both regions, respectively. We will assess the current uncertainties on surface emissions and their recent trends. This analysis is often hindered because of differences in base years and in species considered in the different datasets. Current work aiming at compiling comparable metrics for such species for the analysis of regional and global emission datasets will be discussed. |
|
|
|
|
|
|
|
|
|
|
| 1 : | Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) |
| CNRS : UMR8190 – Université Pierre et Marie Curie [UPMC] - Paris VI – Université de Versailles Saint-Quentin-en-Yvelines – INSU | |
| 2 : | Institut Pierre-Simon-Laplace (IPSL) |
| CNRS : FR636 – Institut de recherche pour le développement [IRD] – CEA – CNES – INSU – Université Pierre et Marie Curie [UPMC] - Paris VI – Université de Versailles Saint-Quentin-en-Yvelines – Ecole normale supérieure de Paris - ENS Paris | |
| 3 : | NOAA Earth System Research Laboratory (NOAA ESRL) |
| U.S. Department of Commerce – National Oceanic & Atmospheric Administration | |
| 4 : | Institut National de l'Environnement Industriel et des Risques (INERIS) |
| INERIS | |
| 5 : | Univ. of Illinois-Champagne |
| Univ. of Illinois-Champagne | |
| 6 : | Institute for Energy and Climate Research (IEK) |
| Forschungszentrum Jülich | |
| 7 : | European Centre for Medium Range Weather Forecast (ECMWF) |
| ECMWF | |
| 8 : | Max Planck Institut für Meteorologie (MPI-M) |
| Max Planck Institut | |
| 9 : | International Institute for Applied Systems Analysis (IIASA) |
| International Institute for Applied Systems Analysis | |
| 10 : | National Center for Atmospheric Research (NCAR) |
| The University Corporation for Atmospheric Research | |
| 11 : | Laboratoire d'aérologie (LA) |
| CNRS : UMR5560 – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III | |
| 12 : | Osaka University |
| Osaka University | |
| 13 : | Joint Global Change research Institute |
| University of Maryland at College Park | |
| 14 : | European Commission |
| European Commission | |
|
|
|
|
|
|
|
|
| tact |
|
|
|
|
| Domaine | : | Physique/Physique/Physique Atmosphérique et Océanique Sciences de l'environnement/Environnement et Société |
|
|
| Atmospheric Composition – Pollution: urban and regiona – Atmospheric Structure – Troposphere: composition and chemistry |
| hal-00671784, version 1 | |
| http://hal.archives-ouvertes.fr/hal-00671784 | |
| oai:hal.archives-ouvertes.fr:hal-00671784 | |
| Contributeur : Catherine Cardon | |
| Soumis le : Samedi 18 Février 2012, 18:49:29 | |
| Dernière modification le : Samedi 18 Février 2012, 18:49:29 | |