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Multi-gas assessment of the Kyoto protocol

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dc.contributor Reilly, John M. en_US
dc.contributor Prinn, Ronald G. en_US
dc.contributor Harnisch, Jochen. en_US
dc.contributor Fitzmaurice, Jean. en_US
dc.contributor Jacoby, Henry D. en_US
dc.contributor Kicklighter, David W. en_US
dc.contributor Stone, Peter H. en_US
dc.contributor Sokolov, Andrei P. en_US
dc.contributor Wang, Chien. en_US
dc.date.accessioned 2003-10-24T14:56:51Z
dc.date.available 2003-10-24T14:56:51Z
dc.date.issued 1999-01 en_US
dc.identifier.other no. 45 en_US
dc.identifier.uri http://mit.edu/globalchange/www/abstracts.html#a45 en_US
dc.identifier.uri http://hdl.handle.net/1721.1/3602
dc.description Includes bibliographical references (p. 13-14). en_US
dc.description Abstract in HTML and technical report in HTML and PDF available on the Massachusetts Institute of Technology Joint Program on the Science and Policy of Global Change website (http://mit.edu/globalchange/www/) en_US
dc.description.abstract The Kyoto Protocol is an international agreement aimed at limiting emissions of several greenhouse gases (GHGs; specifically: CO2, CH4, N2O, PFCs, HFCs, and SF6), and allows credit for approved sinks for CO2. It does not include consideration of several other trace atmospheric constituents that have important indirect effects on the radiative budget of the atmosphere. Here we show that inclusion of other GHGs and CO2 sinks greatly reduces the cost of achieving CO2 emissions reductions specified under the agreement. The Kyoto Protocol extrapolated to 2100 reduces predicted warming by only about 17%. The errors caused by simulating other GHGs with scaled amounts of CO2 on atmospheric composition, climate, and ecosystems are small. Larger errors come from failure to account for interactive and climatic effects of gases that affect atmospheric composition but are not included in the protocol (CO, NOx, and SOx). Over the period to 2100, the Global Warming Potential (GWP) indices based on a 100-year time horizon as specified in the protocol appear to be an adequate representation of trace gas climatic effects. The principal reason for the success of this simplified GWP approach in our calculations is that the mix of gas emissions resulting from a carbon-only rather than a multi-gas control strategy does not change by a large amount. en_US
dc.format.extent 14 p. en_US
dc.format.extent 80212 bytes
dc.format.mimetype application/pdf
dc.language.iso eng en_US
dc.publisher MIT Joint Program on the Science and Policy of Global Change en_US
dc.relation.ispartofseries Report no. 45 en_US
dc.subject.lcc QC981.8.C5 M58 no.45 en_US
dc.title Multi-gas assessment of the Kyoto protocol en_US


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