Potential impact of a US climate policy and air quality regulations on future air quality and climate change
We have investigated how future air quality and climate change are influenced by the US air quality regulations that existed or were proposed in 2013 and a hypothetical climate mitigation policy that aims to reduce 2050 CO<sub>2</sub> emissions to be 50 % below 2005 emissions. Using t...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-04-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/16/5323/2016/acp-16-5323-2016.pdf |
Summary: | We have investigated how future air quality and climate change are influenced by the
US air quality regulations that existed or were proposed in 2013 and a
hypothetical climate mitigation policy that aims to reduce 2050 CO<sub>2</sub>
emissions to be 50 % below 2005 emissions. Using the NASA GISS ModelE2
general circulation model, we look at the impacts for year 2030 and 2055. The
US energy-sector emissions are from the GLIMPSE project (GEOS-Chem LIDORT
Integrated with MARKAL (MARKet ALlocation) for the Purpose of
Scenario Exploration), and other US emissions data sets and the rest of
the world emissions data sets are based on the RCP4.5 scenario. The US air
quality regulations are projected to have a strong beneficial impact on US
air quality and public health in year 2030 and 2055 but result in positive
radiative forcing. Under this scenario, no more emission constraints are
added after 2020, and the impacts on air quality and climate change are
similar between year 2030 and 2055. Surface particulate matter with a diameter
smaller than 2.5 µm (PM<sub>2.5</sub>) is reduced by ∼ 2 µg m<sup>−3</sup> on
average over the USA, and surface ozone by ∼ 8 ppbv. The improved air
quality prevents about 91 400 premature deaths in the USA, mainly due to the
PM<sub>2.5</sub> reduction (∼ 74 200 lives saved). The air quality
regulations reduce the light-reflecting aerosols (i.e., sulfate and organic
matter) more than the light-absorbing species (i.e., black carbon and ozone),
leading to a strong positive radiative forcing (RF) over the USA by both
aerosols' direct and indirect forcing: the total RF is
∼ 0.04 W m<sup>−2</sup> over the globe, and ∼ 0.8 W m<sup>−2</sup> over
the USA. Under the hypothetical climate policy, a future CO<sub>2</sub> emissions
cut is achieved in part by relying less on coal, and thus SO<sub>2</sub> emissions
are noticeably reduced. This provides air quality co-benefits, but it could
lead to potential climate disbenefits over the USA. In 2055, the US mean
total RF is +0.22 W m<sup>−2</sup> due to positive aerosol direct and indirect
forcing, while the global mean total RF is −0.06 W m<sup>−2</sup> due to the
dominant negative CO<sub>2</sub> RF (instantaneous RF). To achieve a regional-scale
climate benefit via a climate policy, it is critical (1) to have
multinational efforts to reduce greenhouse gas (GHG) emissions and (2) to
simultaneously target emission reduction of light-absorbing species (e.g., BC
and O<sub>3</sub>) on top of long-lived species. The latter is very desirable as
the resulting climate benefit occurs faster and provides co-benefits to air
quality and public health. |
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ISSN: | 1680-7316 1680-7324 |