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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Main Authors: 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
Format: Article
Language:English
Published: Copernicus Publications 2015-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/715/2015/acp-15-715-2015.pdf
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spelling 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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