Impacts of emission reductions on aerosol radiative effects
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Unique identifierdoi: 10.5194/acp-15-5501-2015
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CitationPietikäinen, J.-P.. Kupiainen, K.. Klimont, Z.. Makkonen, R.. Korhonen, H.. Karinkanta, R.. Hyvärinen, A.-P.. Karvosenoja, N.. Laaksonen, A.. Lihavainen, H.. Kerminen, V.-M.. (2015). Impacts of emission reductions on aerosol radiative effects. Atmospheric Chemistry and Physics 15 (10);, doi: 10.5194/acp-15-5501-2015.
The global aerosol–climate model ECHAM-HAMMOZ was used to investigate changes in the aerosol burden and aerosol radiative effects in the coming decades. Four different emissions scenarios were applied for 2030 (two of them applied also for 2020) and the results were compared against the reference year 2005. Two of the scenarios are based on current legislation reductions: one shows the maximum potential of reductions that can be achieved by technical measures, and the other is targeted to short-lived climate forcers (SLCFs). We have analyzed the results in terms of global means and additionally focused on eight subregions. Based on our results, aerosol burdens show an overall decreasing trend as they basically follow the changes in primary and precursor emissions. However, in some locations, such as India, the burdens could increase significantly. The declining emissions have an impact on the clear-sky direct aerosol effect (DRE), i.e. the cooling effect. The DRE could decrease globally 0.06–0.4 W m−2 by 2030 with some regional increases, for example, over India (up to 0.84 W m−2). The global changes in the DRE depend on the scenario and are smallest in the targeted SLCF simulation. The aerosol indirect radiative effect could decline 0.25–0.82 W m−2 by 2030. This decrease takes place mostly over the oceans, whereas the DRE changes are greatest over the continents. Our results show that targeted emission reduction measures can be a much better choice for the climate than overall high reductions globally. Our simulations also suggest that more than half of the near-future forcing change is due to the radiative effects associated with aerosol–cloud interactions.