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page 126 of 142 <strong>RIVM</strong> <strong>report</strong> 773301 001 / NRP <strong>report</strong> 410200 051<br />
calculation methods. By first validating and then calibrating European emissions to the<br />
CORINAIR'90 inventory EDGAR will achieve comparable regional emissions for global and<br />
continental atmospheric models, and will be consistent with emission figures used for continental air<br />
pollution issues such as acidification. Another way of validating the data is by comparison with<br />
independently developed inventories of the Global Emission Inventory Activity (GEIA) project. A<br />
number of GEIA inventories are compilations of databases produced elsewhere, while EDGAR uses<br />
activity levels and emission factors whenever possible. Differences between the two approaches will<br />
highlight uncertainties in specific regions of the world, and may lead to corrections in the EDGAR<br />
and/or GEIA approach. Another method of validation is to investigate sources and sinks by<br />
atmospheric modelling using a forward or inverse modelling approach. Both types require good a-<br />
priori emission estimates of all sources.<br />
Furthermore, for model application as well as for policy development, there is a need to assess<br />
(roughly) the uncertainties in emissions inventories: to determine the uncertainty in calculated<br />
concentrations, in regional or sectoral contributions to global emissions and in emission scenarios as<br />
well as in the effectiveness of policy options. There is controversy about the relative importance of<br />
sources such as landfills, wet rice fields and natural wetlands in the global CH4 budget; the sources<br />
in the N2O budget are even more uncertain. For other (indirect) greenhouse gases uncertainties are<br />
also quite large, in particular for emissions in developing countries. Each global inventory has its<br />
specific uncertainty, related to the quality of data or to the method of extrapolation.<br />
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Monitoring of emission trends, which is important for science and policy applications, is done by (a)<br />
annually estimating the development of key sources of direct GHGs based on new data, and (b)<br />
periodically updating the inventories by using recent activity level data, national GHG emission<br />
estimates, NRP results and new emission calculation methodologies.<br />
The results will be used for an evaluation of the key regions/countries, sectors and compounds which<br />
determine the global growth of GHG emissions. Also, national emission inventories prepared for the<br />
FCCC and the UNEP secretariat to the Montreal Protocol may be used, but these do not cover all<br />
countries nor do they cover all sources and gases. Such an analysis will identify areas where reduction<br />
policies appear to be most effective and whether improved calculation methodologies lead to a<br />
shift in policy planning with respect to key regions and key source categories. Ad hoc advice to the<br />
government, IPCC/FCCC or GEIA on emissions, calculation methodology and the effectiveness of<br />
reduction options is also possible, using the analytical structure of EDGAR as a bridge between<br />
science and policy makers.<br />
Results of NRP 1 and 2 will yield new insights for a number of emission source categories. However,<br />
to determine the applicability for emission factors, time profiles and temporal distributions RQ D<br />
JOREDOVFDOH is often not straightforward. Results of NRP may help to evaluate the state of knowledge<br />
in specific fields.<br />
In general, the dissemination of cross sections of (updated) emissions data to other NRP projects will<br />
enlarge the integration within the NRP and thus enhance the comparability of NRP results. Results<br />
from EDGAR will be provided to the IMAGE 2 model to improve and its emission calculation<br />
module. Standard data of current inventories are available to other (NRP) projects; updates of<br />
inventories will be provided to GEIA.<br />
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Remarks of NRP participants and the results of the validation of EDGAR as developed in NRP 1<br />
showed an apparent need for some additions to improve the applicability for policy and scientific<br />
purposes:<br />
- 7HPSRUDOGLVWULEXWLRQ of the annual data. Many atmospheric models have specific requirements in<br />
terms of a temporal distribution of the annual emissions data, e.g. the seasonally or monthly<br />
variation within a calendar year. In other words, there is a need for compilation of time profiles<br />
suitable for application in conjunction of the annual sectoral emission files extracted from<br />
EDGAR.