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Multimodel emission metrics for regional emissions of short lived climate forcers.

Authors :
Aamaas, B.
Berntsen, T. K.
Fuglestvedt, J. S.
Shine, K. P.
Bellouin, N.
Source :
Atmospheric Chemistry & Physics; 2015, Vol. 15 Issue 19, p26089-26130, 42p, 3 Charts, 9 Graphs
Publication Year :
2015

Abstract

For short lived climate forcers (SLCFs), the impact of emissions depends on where and when the emissions take place. Comprehensive new calculations of various emission metrics for SLCFs are presented based on radiative forcing (RF) values calculated in four different (chemistry-transport or coupled-chemistry climate) models. We distinguish between emissions during summer (May-October) and winter season (November-April) for emissions from Europe, East Asia, as well as the global shipping sector. The species included in this study are aerosols and aerosols precursors (BC, OC, SO<subscript>2</subscript>, NH<subscript>3</subscript>), and ozone precursors (NO<subscript>x</subscript>, CO, VOC), which also influence aerosols, to a lesser degree. Emission metrics for global climate responses of these emissions, as well as for CH<subscript>4</subscript>, have been calculated relative to CO<subscript>2</subscript>, using Global Warming Potential (GWP) and Global Temperature change Potential (GTP), based on dedicated RF simulations by four global models. The emission metrics include indirect cloud effects of aerosols and the semi-direct forcing for BC. In addition to the standard emission metrics for pulse and sustained emissions, we have also calculated a new emission metric designed for an emission profile consisting of a ramp up period of 15 years followed by sustained emissions, which is more appropriate for a gradual implementation of mitigation policies. For the aerosols, the emission metric values are larger in magnitude for Europe than East Asia and for summer than winter. A variation is also observed for the ozone precursors, with largest values in East Asia and winter for CO and in Europe and summer for VOC. In general, the variations between the emission metrics derived from different models are larger than the variations between regions and seasons, but the regional and seasonal variations for the best estimate also hold for most of the models individually. Further, the estimated climate impact of a mitigation policy package is robust even when accounting for correlations. For the ramp up emission metrics, the values are generally larger than for pulse or sustained emissions, which holds for all SLCFs. For a potential SLCFs mitigation policy, the dependency of metric values on the region and season of emission should be considered. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
16807316
Volume :
15
Issue :
19
Database :
Complementary Index
Journal :
Atmospheric Chemistry & Physics
Publication Type :
Academic Journal
Accession number :
110320772
Full Text :
https://doi.org/10.5194/acpd-15-26089-2015