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download - Climate Change and Air Quality Unit - Europa

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Workshop “Atmospheric monitoring <strong>and</strong> inverse modelling for verification of national <strong>and</strong> EU bottom-up GHG inventories” - reportWorkshop "Atmospheric monitoring <strong>and</strong> inverse modelling for verification of national <strong>and</strong> EU bottomupGHG inventories " - reportchlorinated solvents (CCl 4 , CH 3 CCl 3 ), brominated organic compounds (halons,CH 3 Br) <strong>and</strong> HFCs (hydrofluorocarbons). Due to its broad coverage of Europe itprovides an important link between the global <strong>and</strong> regionally representativebackground concentrations.As an example the data series of HFC-134a is shown in Figure 2, where a commontrend in the background concentrations is overlaid by higher peak values atJungfraujoch <strong>and</strong> Monte Cimone, which are located nearer to important Europeansource regions in comparison to the more remote site of Mace Head <strong>and</strong> the Arcticsite of Ny-Alesund.HFC 134a200150ppt10050Monte CimoneJungfraujochMace HeadNy-Alesund02000 2001 2002 2003 2004Figure 2: Continuous in-situ measurements of HFC-134a at the four SOGE sites.Thus, as European sources can be detected at the SOGE stations, they providemeasurements which can be used are in support of the Kyoto <strong>and</strong> the Montrealprotocols, in assessing the compliance of European regions with the protocolrequirements. In particular the observation system has been set up to (i) detecttrends in the concentrations of greenhouse active <strong>and</strong> ozone-destroying halocarbons,(ii) verify reported emissions <strong>and</strong> validate emission inventories for a series ofhalocarbons for Europe as a whole as well as for certain regions, (iii) developobservational capacity for all halocarbons included in the Kyoto protocol for whichthis was previously not existing, <strong>and</strong> (iv) develop a strategy for a cost-effective longtermobservation system for halocarbons in Europe. The second objective has beento predict <strong>and</strong> assess impacts of the halocarbons on the climate <strong>and</strong> on the ozonelayer. This implies extensive exploitation of existing data.The European emissions of halocarbons are regularly estimated within SOGE withinseveral publications. For example, HCFC-141b emissions have been shown to have36

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