Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models
European CH<sub>4</sub> and N<sub>2</sub>O emissions are estimated for 2006 and 2007 using four inverse modelling systems, based on different global and regional Eulerian and Lagrangian transport models. This ensemble approach is designed to provide more realistic est...
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doaj-a1d7560cd73d4f11ba4fa85ce72534732020-11-24T23:13:07ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-01-0115271573610.5194/acp-15-715-2015Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse modelsP. Bergamaschi0M. Corazza1U. Karstens2M. Athanassiadou3R. L. Thompson4I. Pison5A. J. Manning6P. Bousquet7A. Segers8A. T. Vermeulen9G. Janssens-Maenhout10M. Schmidt11M. Ramonet12F. Meinhardt13T. Aalto14L. Haszpra15J. Moncrieff16M. E. Popa17D. Lowry18M. Steinbacher19A. Jordan20S. O'Doherty21S. Piacentino22E. Dlugokencky23European Commission Joint Research Centre, Institute for Environment and Sustainability, Ispra, ItalyEuropean Commission Joint Research Centre, Institute for Environment and Sustainability, Ispra, ItalyMax-Planck-Institute for Biogeochemistry, Jena, GermanyMet Office, Exeter, UKLaboratoire des Sciences du Climat et de l' Environnement (LSCE), Gif sur Yvette, FranceLaboratoire des Sciences du Climat et de l' Environnement (LSCE), Gif sur Yvette, FranceMet Office, Exeter, UKLaboratoire des Sciences du Climat et de l' Environnement (LSCE), Gif sur Yvette, FranceEuropean Commission Joint Research Centre, Institute for Environment and Sustainability, Ispra, ItalyEnergy Research Centre of the Netherlands (ECN), Petten, the NetherlandsEuropean Commission Joint Research Centre, Institute for Environment and Sustainability, Ispra, ItalyLaboratoire des Sciences du Climat et de l' Environnement (LSCE), Gif sur Yvette, FranceLaboratoire des Sciences du Climat et de l' Environnement (LSCE), Gif sur Yvette, FranceUmweltbundesamt, Messstelle Schauinsland, Kirchzarten, GermanyFinnish Meteorological Institute (FMI), Helsinki, FinlandHungarian Meteorological Service, Budapest, HungarySchool of GeoSciences, The University of Edinburgh, Edinburgh, UKMax-Planck-Institute for Biogeochemistry, Jena, GermanyDept. of Earth Sciences, Royal Holloway, University of London (RHUL), Egham, UKSwiss Federal Laboratories for Materials Science and Technology (Empa), Dübendorf, SwitzerlandMax-Planck-Institute for Biogeochemistry, Jena, GermanyAtmospheric Chemistry Research Group, University of Bristol, Bristol, UKItalian National Agency for New Technologies, Energy and Sustainable Development (ENEA), Rome, ItalyNOAA Earth System Research Laboratory, Global Monitoring Division, Boulder, CO, USAEuropean CH<sub>4</sub> and N<sub>2</sub>O emissions are estimated for 2006 and 2007 using four inverse modelling systems, based on different global and regional Eulerian and Lagrangian transport models. This ensemble approach is designed to provide more realistic estimates of the overall uncertainties in the derived emissions, which is particularly important for verifying bottom-up emission inventories. <br><br> We use continuous observations from 10 European stations (including 5 tall towers) for CH<sub>4</sub> and 9 continuous stations for N<sub>2</sub>O, complemented by additional European and global discrete air sampling sites. The available observations mainly constrain CH<sub>4</sub> and N<sub>2</sub>O emissions from north-western and eastern Europe. The inversions are strongly driven by the observations and the derived total emissions of larger countries show little dependence on the emission inventories used a priori. <br><br> Three inverse models yield 26–56% higher total CH<sub>4</sub> emissions from north-western and eastern Europe compared to bottom-up emissions reported to the UNFCCC, while one model is close to the UNFCCC values. In contrast, the inverse modelling estimates of European N<sub>2</sub>O emissions are in general close to the UNFCCC values, with the overall range from all models being much smaller than the UNFCCC uncertainty range for most countries. Our analysis suggests that the reported uncertainties for CH<sub>4</sub> emissions might be underestimated, while those for N<sub>2</sub>O emissions are likely overestimated.http://www.atmos-chem-phys.net/15/715/2015/acp-15-715-2015.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
P. Bergamaschi M. Corazza U. Karstens M. Athanassiadou R. L. Thompson I. Pison A. J. Manning P. Bousquet A. Segers A. T. Vermeulen G. Janssens-Maenhout M. Schmidt M. Ramonet F. Meinhardt T. Aalto L. Haszpra J. Moncrieff M. E. Popa D. Lowry M. Steinbacher A. Jordan S. O'Doherty S. Piacentino E. Dlugokencky |
spellingShingle |
P. Bergamaschi M. Corazza U. Karstens M. Athanassiadou R. L. Thompson I. Pison A. J. Manning P. Bousquet A. Segers A. T. Vermeulen G. Janssens-Maenhout M. Schmidt M. Ramonet F. Meinhardt T. Aalto L. Haszpra J. Moncrieff M. E. Popa D. Lowry M. Steinbacher A. Jordan S. O'Doherty S. Piacentino E. Dlugokencky Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models Atmospheric Chemistry and Physics |
author_facet |
P. Bergamaschi M. Corazza U. Karstens M. Athanassiadou R. L. Thompson I. Pison A. J. Manning P. Bousquet A. Segers A. T. Vermeulen G. Janssens-Maenhout M. Schmidt M. Ramonet F. Meinhardt T. Aalto L. Haszpra J. Moncrieff M. E. Popa D. Lowry M. Steinbacher A. Jordan S. O'Doherty S. Piacentino E. Dlugokencky |
author_sort |
P. Bergamaschi |
title |
Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models |
title_short |
Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models |
title_full |
Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models |
title_fullStr |
Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models |
title_full_unstemmed |
Top-down estimates of European CH<sub>4</sub> and N<sub>2</sub>O emissions based on four different inverse models |
title_sort |
top-down estimates of european ch<sub>4</sub> and n<sub>2</sub>o emissions based on four different inverse models |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2015-01-01 |
description |
European CH<sub>4</sub> and N<sub>2</sub>O emissions are estimated for
2006 and 2007 using four inverse modelling systems,
based on different global and regional Eulerian and Lagrangian
transport models. This ensemble approach is designed to provide more
realistic estimates of the overall uncertainties in the derived
emissions, which is particularly important for verifying bottom-up
emission inventories.
<br><br>
We use continuous observations from 10 European stations (including
5 tall towers) for CH<sub>4</sub> and 9 continuous stations for
N<sub>2</sub>O, complemented by additional European and global discrete air
sampling sites. The available observations mainly constrain
CH<sub>4</sub> and N<sub>2</sub>O emissions from north-western and eastern
Europe. The inversions are strongly driven by the observations and
the derived total emissions of larger countries show little
dependence on the emission inventories used a priori.
<br><br>
Three inverse models yield 26–56% higher total CH<sub>4</sub>
emissions from north-western and eastern Europe compared to
bottom-up emissions reported to the UNFCCC, while one model is close
to the UNFCCC values. In contrast, the inverse modelling estimates
of European N<sub>2</sub>O emissions are in general close to the UNFCCC
values, with the overall range from all models being much smaller
than the UNFCCC uncertainty range for most countries. Our analysis
suggests that the reported uncertainties for CH<sub>4</sub> emissions
might be underestimated, while those for N<sub>2</sub>O emissions are
likely overestimated. |
url |
http://www.atmos-chem-phys.net/15/715/2015/acp-15-715-2015.pdf |
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