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.
Keywords: PM2.5, aerosols, exposure, WHO guideline, composition, health, PM2.5 mortality
Introduction
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.20Figure 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 1a). 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 1a demonstrates that only a few regions (e.g., parts of boreal North America and Asia) currently meet the 5 μg m–3 WHO guideline.
Recent work has attributed millions of PM2.5-related deaths to modern day fossil fuel sources19 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 1b). These results challenge our expectations of realistically achieving clean air (as defined by the current WHO AQG) using purely anthropogenic controls.
Figure 1c 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 1c)]. In addition, the noFossil and noAnthro scenarios in Figure 1c 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 2a 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 2a) 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 2a), 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 2b 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 1b,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 India24), 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 3a). 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 3a).
There is a clear relationship between regional aerosol sources (Figure 1c) and the resulting PM2.5 composition (Figure 3a), 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 3b) 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 3b 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 transport32 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 1c) and the consequent composition (Figure 3b) 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.
Acknowledgments
This work was supported by the U.S. National Science Foundation (AGS 1936642).
Supporting Information Available
The Supporting Information is available free of charge at https://pubs.acs.org/doi/10.1021/acs.estlett.2c00203.
Additional supporting data (PDF)
Author Contributions
∥ S.J.P. and T.S.C. are co-first authors.
The authors declare no competing financial interest.
Supplementary Material
References
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