Sidhant J Pai1, Therese S Carter1, Colette L Heald1,2, Jesse H Kroll1,3. 1. Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States. 2. Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States. 3. Department of Chemical Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States.
Abstract
The World Health Organization recently updated their air quality guideline for annual fine particulate matter (PM2.5) exposure from 10 to 5 μg m-3, citing global health considerations. We explore if this guideline is attainable across different regions of the world using a series of model sensitivity simulations for 2019. Our results indicate that >90% of the global population is exposed to PM2.5 concentrations that exceed the 5 μg m-3 guideline and that only a few sparsely populated regions (largely in boreal North America and Asia) experience annual average concentrations of <5 μg m-3. We find that even under an extreme abatement scenario, with no anthropogenic emissions, more than half of the world's population would still experience annual PM2.5 exposures above the 5 μg m-3 guideline (including >70% and >60% of the African and Asian populations, respectively), largely due to fires and natural dust. Our simulations demonstrate the large heterogeneity in PM2.5 composition across different regions and highlight how PM2.5 composition is sensitive to reductions in anthropogenic emissions. We thus suggest the use of speciated aerosol exposure guidelines to help facilitate region-specific air quality management decisions and improve health-burden estimates of fine aerosol exposure.
The World Health Organization recently updated their air quality guideline for annual fine particulate matter (PM2.5) exposure from 10 to 5 μg m-3, citing global health considerations. We explore if this guideline is attainable across different regions of the world using a series of model sensitivity simulations for 2019. Our results indicate that >90% of the global population is exposed to PM2.5 concentrations that exceed the 5 μg m-3 guideline and that only a few sparsely populated regions (largely in boreal North America and Asia) experience annual average concentrations of <5 μg m-3. We find that even under an extreme abatement scenario, with no anthropogenic emissions, more than half of the world's population would still experience annual PM2.5 exposures above the 5 μg m-3 guideline (including >70% and >60% of the African and Asian populations, respectively), largely due to fires and natural dust. Our simulations demonstrate the large heterogeneity in PM2.5 composition across different regions and highlight how PM2.5 composition is sensitive to reductions in anthropogenic emissions. We thus suggest the use of speciated aerosol exposure guidelines to help facilitate region-specific air quality management decisions and improve health-burden estimates of fine aerosol exposure.
Exposure
to fine particulate matter (PM2.5) has a harmful
impact on human health and is a leading environmental source of premature
mortality, responsible for millions of deaths every year.[1,2] Degraded air quality also impacts quality of life and human welfare.[3−7] As a result, many countries have made efforts over the past few
decades to set targeted air quality regulations and implement emission
abatement technologies.To provide general guidance for decreasing
global air pollution
and associated mortality, the World Health Organization (WHO) has
released global air quality guidelines (AQGs) since 1987. These AQGs
serve as science-based benchmarks to inform country-level policies
and regulations. The 1987 AQGs were subsequently updated in 1997 and
2005.[8] However, despite their broad acceptance
among the international scientific community, annual PM2.5 exposure levels in many regions have remained significantly higher
than the annual 2005 WHO guideline of 10 μg m–3.[9]The WHO recently (September 2021)
updated their air quality guidelines,
recommending a more stringent limit on annual PM2.5 exposure
(5 μg m–3) due to additional evidence of the
detrimental impact of PM2.5 on health, especially at low
exposure levels.[10] The broad objective
of this new guideline is to promote the regulation and elimination
of anthropogenic emissions to improve global air quality. However,
much of the global population lives in polluted regions that exceed
even the older 2005 AQG for annual PM2.5 exposure.[9,11]Given the global importance of the WHO AQGs, we conduct a
series
of global model sensitivity simulations to explore the viability of
achieving the updated PM2.5 guidelines worldwide under
different emission abatement scenarios.
Materials and Methods
We model global annual PM2.5 exposures under four emission
scenarios, using the GEOS-Chem chemical transport model (version 13.2.0)
at a horizontal grid resolution of 2° × 2.5° (see the Supporting Information for additional details,
including a description of emission inventories). We use 2019 as a
representative year that is not influenced by the COVID-19 pandemic,
is a reasonably typical fire year, and includes recent updates to
anthropogenic emissions inventories.[12]We conduct a baseline simulation to estimate exposure under “ModernDay” (2019) emissions and three further sensitivity
simulations: excluding global fossil fuel and biofuel emissions (noFossil), excluding all anthropogenic emissions from fossil
fuels, biofuels, and agricultural, crop, and livestock sources and
anthropogenic dust from fugitive, industrial, and combustion sources
(noAnthro; also termed extreme abatement), and excluding all anthropogenic and fire emissions (noAnthro&noFire). Pyrogenic emissions from wildfires, prescribed burns, and agricultural
burning challenge our demarcation of natural and anthropogenic activities,
because human activity has modified nearly every component of the
fire system.[13−17] Thus, the noAnthro&noFire simulation is limited
to emissions from biotic sources (e.g., vegetation, soil, and oceans),
non-anthropogenic dust, sea salt, lightning, and volcanoes.Our approach follows previous state-of-the-science approaches for
PM2.5 source attribution at the global scale.[9,18] For instance, a recent study by McDuffie et al. used the same global
model for source apportionment, in combination with high-resolution
satellite observations, to estimate local-level PM2.5 exposures
and anthropogenic source attributions for 2017. Given our goals of
(1) contrasting the importance of natural and anthropogenic sources
and (2) exploring the role of aerosol composition, in the context
of meeting the WHO AQG on national to global scales, we present our
results at the native model resolution (2° × 2.5°).
McDuffie et al. also show that population-weighted PM2.5 exposures generally increase when global models are downscaled using
higher-resolution satellite data. As a result, the exposure estimates
from this study are at the low end of previous estimates of global
PM2.5 exposure using the same model,[9,11,19] suggesting that our estimates of PM2.5 exposure (and the resulting conclusions) can be viewed
as conservative.To evaluate the simulation, we compare the
annual mean simulated
surface PM2.5 concentrations with surface measurements
from regulatory instruments at 578 sites worldwide (Figure S2). We acknowledge the limits of this evaluation,
in that existing PM2.5 monitoring locations do not adequately
capture many regions of the world.[20]Figure S2b shows that the model, as configured,
captures much of the observed variability, with a relatively low bias
worldwide (R2 of 0.61 and an NMB of −0.095). Figure S2c suggests that the model underestimates
PM2.5 at the cleanest sites, while reproducing the overall
distribution and median PM2.5 levels worldwide. While our
exposure estimates are based on a global model with inherent uncertainties,
this evaluation provides some confidence in the use of GEOS-Chem to
estimate annual mean exposures. Our results below are presented as
lower limits with limited quantitative precision.
Results and Discussion
Annual-average continental PM2.5 concentrations for
the ModernDay simulation range from 1 to 163 μg
m–3, with North America and Australia experiencing
the cleanest conditions and Africa and Asia subject to the highest
PM2.5 concentrations (Figure a). These PM2.5 concentrations
and spatial patterns are broadly consistent with the findings of previous
work.[9,18,21] The dark green
shading in Figure a demonstrates that only a few regions (e.g., parts of boreal North
America and Asia) currently meet the 5 μg m–3 WHO guideline.
Figure 1
Annual PM2.5 model-derived concentrations under
the
(a) ModernDay emission scenario and (b) extreme abatement
scenario (noAnthro). Panel c highlights the relative
importance of different sources by plotting WHO PM2.5 exceedance
areas by scenario type. The ModernDay, noFossil, noAnthro, and noAnthro&noFire scenarios are nested subsets in that order, meaning that an exceedance
in one scenario denotes an exceedance in all scenarios to its left
on the legend. For example, the noAnthro&noFire designation means that even without any anthropogenic and fire emissions,
the grid boxes in beige still exceed 5 μg m–3 due to the natural background. This also means that these grid boxes
exceed the 5 μg m–3 guideline for all other
scenarios (ModernDay, noFossil,
and noAnthro). Figures S4–S6 provide supporting information and an alternate version using the
2005 WHO guideline of 10 μg m–3.
Annual PM2.5 model-derived concentrations under
the
(a) ModernDay emission scenario and (b) extreme abatement
scenario (noAnthro). Panel c highlights the relative
importance of different sources by plotting WHO PM2.5 exceedance
areas by scenario type. The ModernDay, noFossil, noAnthro, and noAnthro&noFire scenarios are nested subsets in that order, meaning that an exceedance
in one scenario denotes an exceedance in all scenarios to its left
on the legend. For example, the noAnthro&noFire designation means that even without any anthropogenic and fire emissions,
the grid boxes in beige still exceed 5 μg m–3 due to the natural background. This also means that these grid boxes
exceed the 5 μg m–3 guideline for all other
scenarios (ModernDay, noFossil,
and noAnthro). Figures S4–S6 provide supporting information and an alternate version using the
2005 WHO guideline of 10 μg m–3.Recent work has attributed millions of PM2.5-related
deaths to modern day fossil fuel sources[19] and has highlighted the substantial air quality benefits of decarbonization.[22] We find that, under an abatement scenario that
completely eliminates all fossil fuel sources (noFossil), most of North America, much of Europe, southern Africa, parts
of South America, and a smaller fraction of Asia and Australia would
experience annual average PM2.5 concentrations of <5
μg m–3 (Figure S3).However, even in the noFossil scenario,
large
parts of South America, northern Africa, the Middle East, and Asia
would experience PM2.5 levels of >5 μg m–3. While extreme abatement measures that remove all human emissions,
including those from agricultural and anthropogenic dust (noAnthro), substantially reduce PM2.5 concentrations
(particularly over Asia), almost all the regions mentioned above would
continue to experience annual PM2.5 concentrations of >5
μg m–3 (Figure b). These results challenge our expectations of realistically
achieving clean air (as defined by the current WHO AQG) using purely
anthropogenic controls.Figure c highlights
modeled grid box exceedances of the 5 μg m–3 guideline under the different PM2.5 sensitivity scenarios.
Non-pyrogenic natural sources (noAnthro&noFire) alone lead to PM2.5 levels of >5 μg m–3 in several areas, including northern and central Africa, the Amazon,
parts of central Australia, the Arabian Peninsula, and large portions
of Asia. This is largely due to natural dust, along with sea-salt
and biogenic organic aerosol, consistent with the work of Zhao et
al.[23] Many regions (e.g., boreal Asia,
central Africa, and southeast Asia) also exceed the new guidelines
due to the influence of biomass burning sources [noAnthro (Figure c)]. In
addition, the noFossil and noAnthro scenarios in Figure c demonstrate that agricultural emissions and anthropogenic dust
are important contributors to the PM2.5 exceedances in
heavily populated regions in eastern Europe and parts of Asia.Figure a quantifies
annual PM2.5 exposure across the global population. Under
modern day emissions, >75% of the world’s population is
exposed
to >10 μg m–3 (the 2005 AQG) and >90%
is exposed
to >5 μg m–3 (the 2021 ACG), numbers that
are generally consistent with the findings of previous work.[5,9,21] While global fossil fuel abatement
(noFossil) (tan in Figure a) would have limited success in meeting
the WHO guidelines (with >65% of the population still in exceedance),
it significantly reduces the high tail of the ModernDay distribution and decreases annual exposures of >25 μg m–3 from ∼40% to ∼5% of the global population
(Figure a), likely
translating into substantial global health benefits. Removing agricultural
and anthropogenic dust emissions (noAnthro, orange
trace) would further reduce exposure, although >50% the world’s
population would still be exposed to PM2.5 levels of >5
μg m–3. The noAnthro&noFire scenario (shown in purple) demonstrates that global PM2.5 exposure from non-pyrogenic natural sources alone could result in
∼40% of the global population being exposed to PM2.5 levels that are above the revised WHO AQG. To contextualize this
result, in our simulations, 14% of the global population experiences
natural PM2.5 concentrations between 4 and 5 μg m–3 and 8% experiences natural PM2.5 concentrations
between 5 and 6 μg m–3 (Figure S8); our estimates of whether natural sources exceed
the WHO guidelines for these populations may be subject to model bias
in the representation of natural aerosol.
Figure 2
Cumulative distribution
functions of population exposure to annual
PM2.5 segmented by (a) emission scenarios and (b) geographic
location. Vertical black lines designate the 2005 and 2021 WHO PM2.5 guidelines. See Figure S7 for
a distribution of average annual PM2.5 population exposures
segmented by per capita national income and geographic location.
Cumulative distribution
functions of population exposure to annual
PM2.5 segmented by (a) emission scenarios and (b) geographic
location. Vertical black lines designate the 2005 and 2021 WHO PM2.5 guidelines. See Figure S7 for
a distribution of average annual PM2.5 population exposures
segmented by per capita national income and geographic location.Figure b illustrates
the regional variation in PM2.5 response, with populations
on many continents still exposed to concentrations substantially above
5 μg m–3, even under extreme anthropogenic
emission abatement (noAnthro). The figure shows large
differences in population exposure between the ModernDay (solid lines) and noAnthro (dashed lines) scenarios
over Asia, Europe, South America, and North America, compared to only
moderate reductions in exposures for populations in Africa and Australia,
due to the relative importance of non-anthropogenic sources in those
regions. Under the noAnthro scenario, relatively
small percentages of the population in North America (∼2%)
and South America (∼8%) experience annual PM2.5 exposures
of >5 μg m–3, compared to ∼15% and
∼27% in Europe and Australia, respectively. However, even under
this extreme scenario, >60% and >70% of the population in Asia
and
Africa, respectively, are exposed to >5 μg m–3 of PM2.5, largely due to the impact of fires and natural
dust. We also note that, per the model underestimate of the limited
observations from South American monitoring stations in Figure S2, our estimate of the percentage of
the population exposed to concentrations of >5 μg m–3 in South America is likely a lower estimate.We note that
stringent abatement measures on all anthropogenic
emissions disproportionately reduces PM2.5 exposures in
Asia in both an absolute sense and a relative sense. Such measures
would decrease the proportion of the population of Asia in exceedance
of the revised AQG from >95% to slightly <65%. Proactive fire
and
dust management techniques could further reduce PM2.5 exposures
in Asia and Africa. We also note that the impact from sporadic air
pollution events (such as fires and dust storms) may be partially
mitigated by staying indoors. However, the outsized influence of these
sources makes it challenging, if not impossible, to achieve the 5
μg m–3 exposure guideline in these regions.
Given that Asia and Africa are host to a number of low- and middle-income
countries, our results demonstrate that the regions with the least
resources to tackle air pollution are often also in areas with the
highest levels of non-anthropogenic PM2.5 (Figure b,c).Fine aerosol particles
consist of numerous chemical compounds but
can be broadly classified into the following categories: black carbon
(BC), organic aerosol (OA), sulfate (SO42–), nitrate (NO3–), ammonium (NH4+) aerosol, fine dust (DST), and fine sea salt
(SS). While other species have been shown to be important at regional
scales (e.g., chloride aerosol over India[24]), the vast majority of global PM2.5 is comprised of the
species listed above. The diversity in global PM2.5 sources
and formation mechanisms results in a regionally heterogeneous distribution
of these different PM2.5 aerosol species across the globe
(Figure a). Some regions
(such as the Amazon and northern Africa) are clearly dominated by
certain types of PM2.5 (OA and dust, respectively), while
many regions exceed the 5 μg m–3 guideline
for total PM2.5 across multiple individual species, even
when taken separately (black regions in Figure a).
Figure 3
(a) WHO PM2.5 exceedance plots segmented
across three
categories by aerosol composition classes: CARB (black carbon and
organic aerosol), SNA (sulfate, nitrate, and ammonium), and DSTSS
(fine dust and sea salt). The legend describes the colors corresponding
to overlapping regions where multiple categories exceed the 5 μg
m–3 guideline. (b) Compositional representation
of population-weighted PM2.5 exposure for the modern day
emission (ModernDay, MD) scenario and the extreme
abatement (noAnthro, nA) scenario organized by continent.
The numbers on top of each bar correspond to the population-weighted
annual PM2.5 exposure for each continent (with levels that
exceed the WHO guideline in red). See Figure S9 for a version of panel a with the 2005 WHO guideline of 10 μg
m–3.
(a) WHO PM2.5 exceedance plots segmented
across three
categories by aerosol composition classes: CARB (black carbon and
organic aerosol), SNA (sulfate, nitrate, and ammonium), and DSTSS
(fine dust and sea salt). The legend describes the colors corresponding
to overlapping regions where multiple categories exceed the 5 μg
m–3 guideline. (b) Compositional representation
of population-weighted PM2.5 exposure for the modern day
emission (ModernDay, MD) scenario and the extreme
abatement (noAnthro, nA) scenario organized by continent.
The numbers on top of each bar correspond to the population-weighted
annual PM2.5 exposure for each continent (with levels that
exceed the WHO guideline in red). See Figure S9 for a version of panel a with the 2005 WHO guideline of 10 μg
m–3.There is a clear relationship
between regional aerosol sources
(Figure c) and the
resulting PM2.5 composition (Figure a), motivating the need to better understand
how different PM2.5 components respond to individual abatement
measures. This is an important prerequisite to developing region-specific
air quality management strategies that are capable of targeting the
more stringent WHO guideline. For example, increased loadings of SNA
(sulfate, nitrate, and ammonium) aerosol from agricultural sources
(particularly in Europe and Asia) challenge the notion that fossil
fuel reduction alone is sufficient to reduce air pollution in these
regions and point to the need for more sustainable agricultural practices
(e.g., ref (25)).A compositional analysis of PM2.5 exposure across different
continents (Figure b) further demonstrates the large variability in exposure to different
PM2.5 constituents. For instance, a major fraction of PM2.5 over Africa consists of fine dust, compared to North America
where dust plays a relatively minor role and OA is much more significant.Figure b also demonstrates
that the composition of the PM2.5 background (noAnthro) differs significantly from the composition of the baseline PM2.5 (ModernDay) in many regions of the world.
Large-scale emission reductions over the coming century can thus be
expected to continue changing regional aerosol composition, with increasing
fractional contributions from natural sources. Current epidemiological
data are inconclusive with respect to the health impacts of this compositional
diversity in PM2.5 exposure, largely because the specific
toxicity of individual PM2.5 constituents is still poorly
understood.[10] As a result, policy makers
and regulators have developed PM2.5 exposure guidelines
based on epidemiological estimates of disease burdens from unspeciated
PM2.5. However, recent work has indicated that PM2.5 toxicity might vary significantly by aerosol composition and source.[26−31] More research is thus urgently required to estimate the speciated
health burdens of PM2.5 to accurately inform the next generation
of exposure guidelines. The modeled heterogeneity in global PM2.5 composition in this study indicates that estimates of human
health impacts that do not consider PM2.5 composition may
be in considerable error, especially in understudied regions (or under
future emission regimes). There is thus a clear need for more frequent
and widespread measurements of PM2.5 composition.The new WHO guidelines for PM2.5 exposure are largely
unattainable for many parts of the world, even with extreme abatement
efforts, given that the natural background alone often exceeds 5 μg
m–3. Both climate change, by modulating natural
PM2.5 sources, and transboundary transport[32] might further impede efforts to achieve these strict guidelines
at the local level. Nonetheless, there exist large and demonstrable
opportunities for air quality improvement from a reduced reliance
on fossil fuels, particularly over Asia.The variability in aerosol sources (Figure c) and the consequent composition (Figure b) support the need
for a new generation of AQGs that incorporate compositional information.
Advances in measurement techniques over the past decade now make it
possible to make speciated PM2.5 measurements frequently
and at scale. Due to the associated expense and logistical challenges,
most monitoring networks continue to rely on bulk mass measurements.
However, when viewed against the outsized costs in human health and
welfare loss due to increased PM2.5 exposures,[7] the cost of deploying more sophisticated measurement
networks that also monitor aerosol composition is relatively low.
This would allow different PM2.5 constituents to be regulated,
enabling targeted and region-specific air quality management solutions.
It would also create new opportunities for much-needed epidemiological
research into differential toxicology, feeding back into the development
of improved AQGs. Particle size may provide an alternative and more
feasible indicator of composition and source in some regions, because
natural aerosol dominates the coarse mode. In particular, PM1 measurements and/or the PM2.5:PM10 ratio (Figure S10) may serve as a useful indicator of
anthropogenic aerosol pollution and help constrain the contribution
of natural sources to regional PM2.5 burdens. Overall,
this work suggests that progress toward cleaner air, as envisioned
by the WHO AQG, demands a new perspective on air quality measurement
and regulation to realize the intended epidemiological benefits of
targeted reductions.
Authors: N Andela; D C Morton; L Giglio; Y Chen; G R van der Werf; P S Kasibhatla; R S DeFries; G J Collatz; S Hantson; S Kloster; D Bachelet; M Forrest; G Lasslop; F Li; S Mangeon; J R Melton; C Yue; J T Randerson Journal: Science Date: 2017-06-30 Impact factor: 47.728
Authors: Melanie S Hammer; Aaron van Donkelaar; Chi Li; Alexei Lyapustin; Andrew M Sayer; N Christina Hsu; Robert C Levy; Michael J Garay; Olga V Kalashnikova; Ralph A Kahn; Michael Brauer; Joshua S Apte; Daven K Henze; Li Zhang; Qiang Zhang; Bonne Ford; Jeffrey R Pierce; Randall V Martin Journal: Environ Sci Technol Date: 2020-06-17 Impact factor: 9.028
Authors: Jennifer K Balch; Bethany A Bradley; John T Abatzoglou; R Chelsea Nagy; Emily J Fusco; Adam L Mahood Journal: Proc Natl Acad Sci U S A Date: 2017-02-27 Impact factor: 11.205
Authors: Erin E McDuffie; Randall V Martin; Joseph V Spadaro; Richard Burnett; Steven J Smith; Patrick O'Rourke; Melanie S Hammer; Aaron van Donkelaar; Liam Bindle; Viral Shah; Lyatt Jaeglé; Gan Luo; Fangqun Yu; Jamiu A Adeniran; Jintai Lin; Michael Brauer Journal: Nat Commun Date: 2021-06-14 Impact factor: 14.919
Authors: Richard Burnett; Hong Chen; Mieczysław Szyszkowicz; Neal Fann; Bryan Hubbell; C Arden Pope; Joshua S Apte; Michael Brauer; Aaron Cohen; Scott Weichenthal; Jay Coggins; Qian Di; Bert Brunekreef; Joseph Frostad; Stephen S Lim; Haidong Kan; Katherine D Walker; George D Thurston; Richard B Hayes; Chris C Lim; Michelle C Turner; Michael Jerrett; Daniel Krewski; Susan M Gapstur; W Ryan Diver; Bart Ostro; Debbie Goldberg; Daniel L Crouse; Randall V Martin; Paul Peters; Lauren Pinault; Michael Tjepkema; Aaron van Donkelaar; Paul J Villeneuve; Anthony B Miller; Peng Yin; Maigeng Zhou; Lijun Wang; Nicole A H Janssen; Marten Marra; Richard W Atkinson; Hilda Tsang; Thuan Quoc Thach; John B Cannon; Ryan T Allen; Jaime E Hart; Francine Laden; Giulia Cesaroni; Francesco Forastiere; Gudrun Weinmayr; Andrea Jaensch; Gabriele Nagel; Hans Concin; Joseph V Spadaro Journal: Proc Natl Acad Sci U S A Date: 2018-09-04 Impact factor: 11.205