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dc.date.accessioned2020-06-29T18:26:14Z
dc.date.available2020-06-29T18:26:14Z
dc.date.created2020-02-06T14:06:19Z
dc.date.issued2019
dc.identifier.citationAamaas, Borgar Berntsen, Terje Koren Samset, Bjørn Hallvard . The regional temperature implications of strong air quality measures. Atmospheric Chemistry and Physics. 2019, 19(24), 15235-15245
dc.identifier.urihttp://hdl.handle.net/10852/77301
dc.description.abstractAbstract. Anthropogenic emissions of short-lived climate forcers (SLCFs) affect both air quality and climate. How much regional temperatures are affected by ambitious SLCF emission mitigation policies is, however, still uncertain. We investigate the potential temperature implications of stringent air quality policies by applying matrices of regional temperature responses to new pathways for future anthropogenic emissions of aerosols, methane (CH4), and other short-lived gases. These measures have only a minor impact on CO2 emissions. Two main options are explored, one with climate optimal reductions (i.e., constructed to yield a maximum global cooling) and one with the maximum technically feasible reductions. The temperature response is calculated for four latitude response bands (90–28∘ S, 28∘ S–28∘ N, 28–60∘ N, and 60–90∘ N) by using existing absolute regional temperature change potential (ARTP) values for four emission regions: Europe, East Asia, shipping, and the rest of the world. By 2050, we find that global surface temperature can be reduced by -0.3±0.08 ∘C with climate-optimal mitigation of SLCFs relative to a baseline scenario and as much as −0.7 ∘C in the Arctic. Cutting CH4 and black carbon (BC) emissions contributes the most. The net global cooling could offset warming equal to approximately 15 years of current global CO2 emissions. On the other hand, mitigation of other SLCFs (e.g., SO2) leads to warming. If SLCFs are mitigated heavily, we find a net warming of about 0.1 ∘C, but when uncertainties are included a slight cooling is also possible. In the climate optimal scenario, the largest contributions to cooling come from the energy, domestic, waste, and transportation sectors. In the maximum technically feasible mitigation scenario, emission changes from the industry, energy, and shipping sectors will cause warming. Some measures, such as those in the agriculture waste burning, domestic, transport, and industry sectors, have large impacts on the Arctic, especially by cutting BC emissions in winter in areas near the Arctic.
dc.languageEN
dc.publisherCopernicus GmbH
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleThe regional temperature implications of strong air quality measures
dc.typeJournal article
dc.creator.authorAamaas, Borgar
dc.creator.authorBerntsen, Terje Koren
dc.creator.authorSamset, Bjørn Hallvard
cristin.unitcode185,15,22,70
cristin.unitnameMeteorologi og oseanografi
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.cristin1791639
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric Chemistry and Physics&rft.volume=19&rft.spage=15235&rft.date=2019
dc.identifier.jtitleAtmospheric Chemistry and Physics
dc.identifier.volume19
dc.identifier.issue24
dc.identifier.startpage15235
dc.identifier.endpage15245
dc.identifier.doihttps://doi.org/10.5194/acp-19-15235-2019
dc.identifier.urnURN:NBN:no-80382
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn1680-7316
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/77301/2/acp-19-15235-2019.pdf
dc.type.versionPublishedVersion


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