Jennifer Burney’s research while affiliated with University of California, San Diego and other places

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Publications (25)


Fig. 1. National-and state-level relative disparities in air pollution exposure by race and ethnicity in the contiguous United States. (A) Bars indicate national (Top)-and state-level disparities for each racial/ethnic group. The bar color indicates the average absolute exposure to respirable particulate matter (PM 2.5 ) of each group within each state in the 2010s. The red triangles show 2010 (light red) and 2019 (dark red) disparities, estimated from fitting a linear trend through annual disparities. (B) Maps of the contribution of each tract to national disparities, which is calculated as the product of tract PM 2.5 concentration and the population of the specified group in each tract, divided by the total national population of that group. The sum of the national contributions values yields the population-weighted exposures for each group.
Fig. 2. Exposures and disparities of PM 2.5 after implementing idealized policy priorities to meet emission reduction targets. (A) Total average national PM exposure, (B) national disparities by demographic group, (C) annualized costs of mitigation, and (D) absolute exposure difference by demographic group. Absolute exposure difference refers to the difference in exposure from the Unmodified 2017 total exposure in (A). All pathways lead to reductions in absolute PM 2.5 exposures and entail annualized costs of $190 to 340 billion. The No Industry and No Agriculture simulations, marked with asterisks, are not NDC constrained and do not have cost estimates.
Fig. 3. Sectoral influence in randomized experiments. National POC exposure as a function of cost, colored by reductions in residential emissions (A), and national population-average exposure colored by reductions in transportation emissions (B). There is little relationship between cost and POC exposure, but POC exposure and total exposure are strongly correlated. Costs in the randomized experiments are strongly dependent on the residential sector (A) and POC exposures tend to be lower when more transportation emissions are reduced (B).
Fig. 4. Disparity and exposure changes and transportation influence in randomized experiments. (A) Distributions of changes in national disparity relative to the Unmodified 2017 case for each randomized experiment (N = 300 per distribution) (B) Distribution of state disparities (N = 48 per distribution) in each randomized experiment (faint solid lines, N = 300 distributions) and the Unmodified 2017 case (darker dashed lines). (D and E) Equivalent distributions as for (A) and (B), using exposure instead of disparity. (C and F) Distributions of state-level linear regression coefficients (N = 48 per distribution) from modeling disparity (C) and exposure (F) using fractional change in all the four sectors; only transportation coefficients are shown as they have the most disparate impact.
Air quality equity in US climate policy
  • Article
  • Full-text available

June 2023

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75 Reads

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20 Citations

Proceedings of the National Academy of Sciences

Pascal Polonik

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Katharine Ricke

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Sean Reese

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Jennifer Burney

The United States government has indicated a desire to advance environmental justice through climate policy. As fossil fuel combustion produces both conventional pollutants and greenhouse gas (GHG) emissions, climate mitigation strategies may provide an opportunity to address historical inequities in air pollution exposure. To test the impact of climate policy implementation choices on air quality equity, we develop a broad range of GHG reduction scenarios that are each consistent with the US Paris Accord target and model the resulting air pollution changes. Using idealized decision criteria, we show that least cost and income-based emission reductions can exacerbate air pollution disparities for communities of color. With a suite of randomized experiments that facilitates exploration of a wider climate policy decision space, we show that disparities largely persist despite declines in average pollution exposure, but that reducing transportation emissions has the most potential to reduce racial inequities.

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Changes in crop CalP, CF, CalY and cropland area during 1979–2018
Here, different regions are defined by FAO. Each time series is normalized using data points at year 1979. Note different y axis scale for South America.
Response of CF, CalY and CalP to temperature
a–c, Response function of CF (a), CalY (b) and CalP (c) to Tmean with and without irrigation. Response functions are established on the basis of bootstrap. The 1,000 estimated regression coefficients are then used to determine the 95% CI (shaded areas) of model-estimated coefficients. The medians of the coefficients are used to determine the response curves. Two response curves corresponding to without and with irrigation are determined through setting irrigation fraction as zero and historical global mean, respectively. The 2.5th and 97.5th percentiles are used to define the lower and upper bounds of the 95% CI. Here, the curves are shifted vertically so that the peak values of CF, CalY and CalP under no irrigation are 1. Triangles on the x axis indicate the optimal temperature with different levels of irrigation. d, Marginal effect of 1 °C warming on global average CF, CalY and CalP estimated with eight panel models (the numbers under the line correspond to the models in Methods). The global average of marginal effect of 1 °C warming is a country crop area weighted average of warming effects in each country. Error bars represent 95% CI of each estimation. The ensemble mean of eight panel models estimation is indicated by the horizontal line with shaded area as the 95% CI of ensemble mean.
Effect of warming and irrigation on CF, CalY and CalP
a–c, Marginal effect of 1 °C warming on CF (a), CalY (b) and CalP (c) for each country estimated with baseline model. The marginal effect of 1 °C warming was estimated as the difference between predicted CF, CalY or CalP with uniform 1 °C warming and the original CF, CalY or CalP, based on model M1 and historical irrigation fraction. d–f, Sensitivity of CF (d), CalY (e) and CalP (f) to irrigation area fraction, estimated with the baseline model M1 (∂Yi,t∂Irrii,t=β3Tmeani,t+β6Prcpi,t\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\frac{{\partial Y_{i,t}}}{{\partial \mathrm{Irri}_{i,t}}} = \beta _3\mathrm{Tmean}_{i,t} + \beta _6\mathrm{Prcp}_{i,t}$$\end{document}). Sensitivity for each country can be obtained with multiyear mean climate variables during 1979–2018. As Yi,t\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$Y_{i,t}$$\end{document} is logged, the estimated sensitivities indicate the percentage change in CF (CalY or CalP) with unit percentage change in irrigation area fraction. The insets in d–f show the sensitivity of CF, CalY and CalP to irrigation fraction in climate space, which is delineated by country-level annual precipitation (x axis) and annual mean temperature (y axis) during 1979–2018. Colours in each climate space indicate the sensitivity of CF, CalY and CalP to irrigation fraction.
Projected changes in CF, CalY and CalP for 2031–2070 relative to the reference period 1979–2018
a,b, Boxplot of global and continental changes in CF, CalY and CalP under SSP 126 and SSP 585 estimated with baseline model. Boxplots indicate the median (horizontal line), 25–75th percentile (box) and 5–95th percentile (whiskers) of estimated change of all year and country combinations relative to historical period (1979–2018). c–h, Projected changes in country-level CF (c,d), CalY (e,f) and CalP (g,h) under SSP 126 and SSP 585 for 2031–2070 relative to the reference period 1979–2018.
Projected irrigation area fraction to offset climate change-induced decline in CalP
a,b, The irrigation area fraction required to offset climate change-induced decline in CalP is projected with baseline model M1 driven by ensemble mean of future (2031–2017) climate models outputs under SSP 126 (a) and SSP 585 (b) and historical reference period (1979–2018) climate dataset.
Warming reduces global agricultural production by decreasing cropping frequency and yields

October 2022

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1,865 Reads

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121 Citations

Nature Climate Change

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Jennifer Burney

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[...]

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Annual food caloric production is the product of caloric yield, cropping frequency (CF, number of production seasons per year) and cropland area. Existing studies have largely focused on crop yield, whereas how CF responds to climate change remains poorly understood. Here, we evaluate the global climate sensitivity of caloric yields and CF at national scale. We find a robust negative association between warming and both caloric yield and CF. By the 2050s, projected CF increases in cold regions are offset by larger decreases in warm regions, resulting in a net global CF reduction (−4.2 ± 2.5% in high emission scenario), suggesting that climate-driven decline in CF will exacerbate crop production loss and not provide climate adaptation alone. Although irrigation is effective in offsetting the projected production loss, irrigation areas have to be expanded by >5% in warm regions to fully offset climate-induced production losses by the 2050s.


Fig. 1. Pathways of impact for NO 2 (NO x ) on crop yields. NO x is itself a phytotoxin, and increased levels lead to decreased plant growth and lower yields. NO x can also lead to formation of ozone, which is also toxic for crops, but the ozone dynamics depend on the local pollution regime. In areas that are NO x limited but have high available reactive VOCs, increased NO x leads to more ozone formation and decreased yields. In areas that are NO x saturated (i.e., have low VOC:NO x ratios), increased NO x levels titrate ozone out of the atmosphere, lowering levels and resulting in increased yields. Last, increased NO x in the presence of ammonia or SO 2 can lead to aerosol formation. These aerosols reflect and scatter incoming sunlight, reducing the amount of light available for photosynthesis and lowering yields. The net impact of NO 2 (NO x ) on crop yields, i.e., the sum of direct, ozone, and aerosol pathways, thus depends on the local pollution regime. We leverage different ozone regimes around the world to evaluate the relative importance of ozone pathway.
Fig. 2. Regional crop exposures to NO 2 . (A) A map of average TROPOMI NO 2 values for the peak of the winter crop season for the world (April and May) and for the winter season for five regions of interest in this study. Regional insets only show pixels where wheat is more than 2% of the land area from which we sample data for our analysis. (B) Histograms of NO 2 values for the winter season for each region and year. The months associated with each region are given in table S2. A comparable figure for the summer season is shown in the Supplementary Materials (fig. S7).
Fig. 3. Illustration of the fixed-effect regression approach. In each region and season, points are sampled throughout the region and split into local 0.5° × 0.5° grid cells (A) (which shows NO 2 and NIRv values for 2020 in winter in China as an example). The deviations of NO 2 and NIRv values for each point from their grid cell average are then calculated (B), and the deviations for all grid cells are then combined into a single regression (C). Blue line in (C) shows best-fit linear regression line fit to all points. By taking deviations from the local averages, we reduce the chance that a third variable is correlated spatially with both NO 2 and NIRv, which could potentially lead to omitted variable bias.
Fig. 4. Higher NO 2 is consistently associated with lower crop greenness. Points indicate the estimated effect of a 1-U increase of NO 2 on the NIRv, a measure of crop growth. Error bars show the 95% confidence interval based on SEs clustered at 0.5° × 0.5° grid cells. Solid colors denote estimates significant at P < 0.05. The figure shows the results of 10 separate regressions, one for each region and season, with multiple years pooled together. Figure S4 shows results of regressions run for individual years.
Fig. 5. NO 2 impacts are higher in NO x -limited ozone regimes but persist even in non-NO x limited regimes. (A and B) The distribution of the ratio of HCHO:NO 2 from TROPOMI for 2020 winter and summer cropping seasons in each region. Values above 2 are used to indicate NO x -limited regimes. (C and D) Estimated sensitivity of greenness to NO 2 for two different subsets of points, with points split by the ozone regime. The point sizes are proportional to the percentage of points by regime type in each region. Error bars indicate the 95% confidence intervals.
Globally ubiquitous negative effects of nitrogen dioxide on crop growth

June 2022

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178 Reads

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54 Citations

Science Advances

Nitrogen oxides (NOx) are among the most widely emitted pollutants in the world, yet their impacts on agriculture remain poorly known. NOx can directly damage crop cells and indirectly affect growth by promoting ozone (O3) and aerosol formation. We use satellite measures of both crop greenness and NOx during 2018-2020 to evaluate crop impacts for five major agricultural regions. We find consistent negative associations between NO2 and greenness across regions and seasons. These effects are strongest in conditions where O3 formation is NOx limited but remain significant even in locations where this pathway is muted, suggesting a role for direct NOx damage. Using simple counterfactuals and leveraging published relationships between greenness and growth, we estimate that reducing NOx levels to the current fifth percentile in each region would raise yields by ~25% for winter crops in China, ~15% for summer crops in China, and up to 10% in other regions.


Pollution and demographic data used in this study
a,b, Average surface PM2.5 (a) and tropospheric NO2 (b) concentrations in the pre-shutdown period of 2020 in California, United States. c, Median household income (US$) in each CBG from the US Census Bureau 2018 5 yr American Community Survey (ACS). d–f, Share of the population in each CBG that is Hispanic (d), Asian (e) or Black (f), from the ACS. g, Schematic showing both slower-changing (assumed to be static over shorter periods) and higher-frequency factors that contribute to heterogeneous pollution exposures. Symbols in g courtesy of Noun Project: Automobile by Symbolon; Income and Highway by Vectors Point; Urban by Eucalup; weather by asianson.design; List by Richard Kunák; inequality by b farias.
The COVID-19 ‘mobility shock’
a, Percentage-point difference in time spent at home pre-shutdown and during the shutdown at the CBG level in California, with an inset for the Los Angeles region. b, Mobility reductions for the median of the upper and lower 10% of three different population subsets. Shading indicates the 25th and 75th percentiles within each group. Vertical lines indicate the beginning and end of the transition (4 March 2020 and 19 March 2020) period excluded from our dynamic analysis. Average pre-/post-shutdown percentages are given in Supplementary Table 1.
Impact of the economic shutdown on (left) PM2.5 concentrations and (right) mobility
Points show heterogeneous changes across CBG characteristics estimated from difference-in-differences models, along with 95% confidence intervals. Intervals that include zero indicate that there was no differential reduction in exposures across the given gradient. a, Changes in daily PM2.5 concentration across the shutdown estimated for various socioeconomic variables. The coefficient for mobility is the estimated difference between 0 and 100% of time spent at home; the coefficients for (ln) income, road and population density each represent the impact of an approximate doubling for each variable. b, Similar estimates with mobility as the dependent variable. c,e, Changes in PM2.5 concentrations over the shutdown period across different racial and ethnic population shares, estimated with different physical and socioeconomic control variables (labels on left). The coefficients correspond to the expected changes between 0 and 100% population share at the CBG level. See Supplementary Tables 2 and 3 for values. d,f, Similar estimates, but with mobility as the outcome instead of PM2.5. Values are given in Supplementary Tables 4 and 5. All four panels compare the post-shutdown difference from 2020 to 2019 to the pre-shutdown difference to account for seasonality. In addition, estimates were weighted to reflect the distribution of incomes, population shares and other location characteristics across all block groups in California and correct for the endogenous sampling of ground station locations (Extended Data Fig. 2b, Methods and Supplementary Information). The ‘Base’ model includes CBG and day-of-year fixed effects, as well as weather controls; other models incorporate the noted controls, or exclude weather, and ‘All’ includes everything.
Disparate air pollution reductions during California’s COVID-19 economic shutdown

June 2022

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78 Reads

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26 Citations

Nature Sustainability

Minority communities in the United States often experience higher-than-average exposures to air pollution. However, the relative contribution of institutional biases to these disparities can be difficult to disentangle from other factors. Here, we use the economic shutdown associated with the 2020 COVID-19 shelter-in-place orders to causally estimate pollution exposure disparities caused by the in-person economy in California. Using public and citizen-science ground-based monitor networks for respirable particulate matter, along with satellite records of nitrogen dioxide, we show that sheltering in place produced disproportionate air pollution reductions for non-White (especially Hispanic and Asian) and low-income communities. We demonstrate that these racial and ethnic effects cannot be explained by weather patterns, geography, income or local economic activity as measured by local changes in mobility. They are instead driven by regional economic activity, which produces local harms for diffuse economic benefits. This study thus provides indirect, yet substantial, evidence of systemic racial and ethnic bias in the generation and control of pollution from the portion of the economy most impacted in the early pandemic period.


Land-use emissions embodied in international trade

May 2022

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859 Reads

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136 Citations

Science

International trade separates consumption of goods from related environmental impacts, including greenhouse gas emissions from agriculture and land-use change (together referred to as “land-use emissions”). Through use of new emissions estimates and a multiregional input-output model, we evaluated land-use emissions embodied in global trade from 2004 to 2017. Annually, 27% of land-use emissions and 22% of agricultural land are related to agricultural products ultimately consumed in a different region from where they were produced. Roughly three-quarters of embodied emissions are from land-use change, with the largest transfers from lower-income countries such as Brazil, Indonesia, and Argentina to more industrialized regions such as Europe, the United States, and China. Mitigation of global land-use emissions and sustainable development may thus depend on improving the transparency of supply chains.


Untangling irrigation effects on maize water and heat stress alleviation using satellite data

February 2022

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191 Reads

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50 Citations

Irrigation has important implications for sustaining global food production by enabling crop water demand to be met even under dry conditions. Added water also cools crop plants through transpiration; irrigation might thus play an important role in a warmer climate by simultaneously moderating water and high temperature stresses. Here we used satellite-derived evapotranspiration estimates, land surface temperature (LST) measurements, and crop phenological stage information from Nebraska maize to quantify how irrigation relieves both water and temperature stresses. Unlike air temperature metrics, satellite-derived LST revealed a significant irrigation-induced cooling effect, especially during the grain filling period (GFP) of crop growth. This cooling appeared to extend the maize growing season, especially for GFP, likely due to the stronger temperature sensitivity of phenological development during this stage. Our analysis also revealed that irrigation not only reduced water and temperature stress but also weakened the response of yield to these stresses. Specifically, temperature stress was significantly weakened for reproductive processes in irrigated maize. Attribution analysis further suggested that water and high temperature stress alleviation was responsible for 65±10 % and 35±5.3 % of the irrigation yield benefit, respectively. Our study underlines the relative importance of high temperature stress alleviation in yield improvement and the necessity of simulating crop surface temperature to better quantify heat stress effects in crop yield models. Finally, considering the potentially strong interaction between water and heat stress, future research on irrigation benefits should explore the interaction effects between heat and drought alleviation.


Flowchart describing the overall layout of data acquisition.
Maps of extreme summer daytime surface urban heat ΔT within the US and selected counties. Shown is average ΔT of all developed areas within a census tract. Inset areas show the heterogeneity within urban areas (Selected counties are A: King County, Washington (Seattle); B: Hennepin County, Minnesota (Minneapolis); C: Kings County, New York (Brooklyn, NYC); D: Maricopa County, Arizona (Phoenix); and E: Miami‐Dade County, Florida.) For each inset, the corresponding dot‐and‐ellipse plots show the distributions of daytime and nighttime ΔT by income quartiles, with dots showing the quartile mean for all census tracts within that county. The size of the dot shows the mean income of the corresponding quartile, since income distributions vary across the country.
Difference in daytime and nighttime ΔT for highest and lowest quartiles of nine demographic variables for all 1,056 counties analyzed in this study. Each dot represents the difference in first and last quartile of a county for the corresponding demographic variable. The size of the dot represents the size of the county as its number of developed census tracts. The color gives information on the interquartile range (IQR) of the demographic variable in each county. The histograms below each plot show the distribution of counties with the lowest (blue) and highest (magenta) 25% of IQRs. Percentages in the corners gives percentage of counties with significant differences in daytime ΔT for each side.
Difference in daytime and nighttime ΔT residuals for highest and lowest quartiles of eight demographic variables for all 1,056 counties analyzed in this study, after controlling for income. Each dot represents the difference in first and last quartile of a county for the corresponding demographic variable. The size of the dot represents the size of the county as its number of developed census tracts. The color gives information on the interquartile range (IQR) of the demographic variable in each county. The histograms below each plot show the distribution of counties with the lowest (blue) and highest (magenta) 25% of IQRs. Percentages in the corners gives percentage of counties with significant differences in daytime ΔT residuals for each side.
Effects of urban design parameters on daytime and nighttime ΔT and their distribution for lowest and highest quartile of income and selected demographic variables after controlling for income. Shown are deviation from county average for built‐up index (NDBI), vegetation index (NDVI), albedo (BSA), and population density (at the log scale).
Widespread Race and Class Disparities in Surface Urban Heat Extremes Across the United States

July 2021

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252 Reads

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102 Citations

Here we use remotely sensed land surface temperature measurements to explore the distribution of the United States’ urban heating burden, both at high resolution (within cities or counties) and at scale (across the whole contiguous United States). While a rich literature has documented neighborhood‐level disparities in urban heat exposures in individual cities, data constraints have precluded comparisons across locations. Here, drawing on urban temperature anomalies during extreme summer surface temperature events from all 1,056 US counties with more than 10 developed census tracts, we find that the poorest tracts (and those with lowest average education levels) within a county are significantly hotter than the richest (and more educated) neighborhoods for 76% of these counties (54% for education); we also find that neighborhoods with higher Black, Hispanic, and Asian population shares are hotter than the more White, non‐Hispanic areas in each county. This holds in counties with both large and small spreads in these population shares, and for 71% of all counties the significant racial urban heat disparities persist even when adjusting for income. Although individual locations have different histories that have contributed to race‐ and class‐based geographies, we find that the physical features of the urban environments driving these surface heat exposure gradients are fairly uniform across the country. Systematically, the disproportionate heat surface exposures faced by minority communities are due to more built‐up neighborhoods, less vegetation, and—to a lesser extent—higher population density.


Overview of data used in this study. Average 1999–2018 (a) maize and (b) soybean yields for individual 30 m × 30 m pixels estimated based on satellite data. (c) Location of power plant facilities and EPA monitoring stations in the study region. Numbers in parentheses indicate the number of unique locations with at least one unit powered by the indicated fuel type. (d) Locations of specific types of pollution monitors. Not all power plant facilities or pollution monitors were active during the entire study period. The total number of unique monitors for each pollutant since 1999 are 387 for Ozone, 391 for PM10, 428 for PM2.5, 290 for SO2, and 118 for NO2.
The estimated effect of each pollutant on maize and soybean yields from panel regressions. Plot shows panel regression coefficients for each pollutant, expressed as the percentage change in yield from a 1 standard deviation increase in each pollutant. The numbers in parentheses indicate the total number of site-years used in the regression. NASS refers to regressions using county-level yields reported by the USDA NASS, and SCYM refers to regressions using the average of satellite-based 30 m resolution yields within 20 km of the monitoring station. Error bars indicate ±2 cluster-robust standard errors, based on clustering at site and year level. These results correspond to the model using AOT70 to measure ozone exposure and PM10 to measure PM exposure. Yield changes are expressed as percent of mean yields, which for NASS are 9.24 t ha⁻¹ for maize and 2.96 t ha⁻¹ for soy. SCYM yields average 10.39 t ha⁻¹ for maize and 3.31 t ha⁻¹ for soy. Standard deviations of pollutant levels are 1055 ppb-hours for AOT70, 9.7 mg m⁻² for PM10, 11.3 ppb for SO2, and 13.2 ppb for NO2.
Pollution and yield gradients help to constrain the response of yields to NO2. Top panels show the dependence of average (a) maize yield residuals (from a regression controlling for weather, soil characteristics, and year) and (b) pollutant levels on distance from the closest power plant facility, based on local polynomial regressions (LOWESS). (c) The average pollutant levels at 30 km, expressed as the percentage change relative to average levels at 1 km. Averages are shown both for all facilities and for the subset of facilities with and without active coal units. Error bars show 5%–95% confidence interval based on bootstrap resampling of facilities. (d) Yield gradients (in t/ha) observed near facilities (gray bars) compared to the yield gradients predicted by the panel regressions for the pollution gradients in O3, PM10, and SO2 shown in panel (c). Error bars show 5%–95% confidence interval based on uncertainty in both pollution gradients and yield sensitivities. Yellow bar indicates the residual yield gradient not explained by the three pollutants, which is then used to estimate the NO2 effect by dividing the residual yield gradient by the NO2 gradient.
Estimated impacts of pollution over time. (a) Temporal evolution of different pollution measures, relative to their value in 1999, and the effects of pollutant levels in each year on (b) maize and (c) soybean yields. Solid lines in (b) and (c) indicate the mean estimate across 100 bootstrap estimates that account for uncertainty in yield sensitivities to pollutants as well as pollution gradients near power plants, which are used to estimate NO2 effects. Shaded areas indicate 5%–95% confidence intervals.
Cleaner air has contributed one-fifth of U.S. maize and soybean yield gains since 1999

July 2021

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74 Reads

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31 Citations

Crop productivity is potentially affected by several air pollutants, although these are usually studied in isolation. A significant challenge to understanding the effects of multiple pollutants in many regions is the dearth of air quality data near agricultural fields. Here we empirically estimate the effect of four key pollutants (ozone (O3), particulate matter (PM), sulfur dioxide (SO2), and nitrogen dioxide (NO2)) on maize and soybean yields in the United States using a combination of administrative data and satellite-derived yield estimates. We identify clear negative effects of exposure to O3, PM, and SO2 in both crops, using yields measured in the vicinity of monitoring stations. We also show that while stations measuring NO2 are too sparse to reliably estimate a yield effect, the strong gradient of NO2 concentrations near power plants allows us to more precisely estimate NO2 effects using satellite measured yield gradients. The presence of some powerplants that turn on and others that shut down during the study period are particularly useful for attributing yield gradients to pollution. We estimate that total yield losses from these pollutants averaged roughly 5% for both maize and soybean over the past two decades. While all four pollutants have statistically significant effects, PM and NO2 appear more damaging to crops at current levels than O3 and SO2. Finally, we find that the significant improvement in air quality since 1999 has halved the impact of poor air quality on major crops and contributed to yield increases that represent roughly 20% of overall yield gains over that period.


(A) Map of urban surface temperature anomalies (ΔT). Shown is the average of all urban pixels in each grid cell (aggregated to a 2∘ grid to show basic distribution). (Full 1 km resolution data are available at https://sabenz.users.earthengine.app/view/surface-delta-t). Grid cells not included in a city defined by the Urban Center Database (Florczyk et al 2019) are left blank. (See figure S1 for all seasons and annual mean). (B) Summer daytime ΔT and winter nighttime ΔT for selected locations. Shown are urban and non-urban ΔT, outlines of cities are shown in black.
(A) Heat map of daytime and nighttime urban surface temperature anomalies (ΔT) averaged over the whole year, and broken out by season (see figure S2 for spring and fall). Black markings indicate the mean point and 90% confidence ellipse. The total area and population represented in each quadrant is shown. (B) Distributions of average summer daytime (left) and average winter nighttime (right) surface temperatures that populations in cities are exposed to, compared to all other areas. In red the distribution based on average city surface temperatures. The light blue line shows the surface temperatures at the homes of the urban population in a scenario without urban heat (LST—ΔT). C: Heat map of the standard deviation (Std) of ΔT of each city within the Urban Center Database of the Global Human Settlement Layer (Florczyk et al 2019).
(A) Bivariate relationships between urban surface temperature anomalies (ΔT) and observable satellite measures impacting the surface energy balance. The inner 90 percentile of each parameter is fit with a simple linear regression, shown in red, 90% confidence interval are dashed in black (see table S2 for coefficients and goodness of fit; figure S5 for results of seasonal (summer and winter) ΔT). (B) Predicted changes in urban ΔT for each satellite measure, based on a multiple regression model including all four parameters. Shown is the predicted change in ΔT for a change in the predictor variable over the entire analyzed range (5th to 95th percentile). Uncertainties are constructed by conducting 1000 versions of the regression using sub-samples of data (see supplement S2.3); median regression is shown as a dot, outliers (following the box-plot convention defined as outside ±2.7σ) are displayed as circles.
(A) Expected changes in urban surface temperature anomalies (ΔT) for a change in population density following all urbanization scenarios. (B) Average change from current annual mean ΔT for different scenarios, years, and SSPs. The 90% confidence ellipse displaying spatial variability is given in lighter colors, the uncertainty for the mean point following the regression is given as a colored-in square. Changes during Summer and Winter are shown in figure S14. (C) Changes from current ΔT based on scenarios Business-as-Usual and Best Case. Average of all inner-city pixels in each 2∘ grid cells is shown.
(A) Distribution of urban population and surface temperatures they are exposed to. Distributions of present population are compared to hypothetical scenarios without ΔT and our optimized scenario Mitigation. Comparisons also include the future scenarios Business-as-Usual, which preserves present urban relationships into the future, and Best Case, which optimizes vegetation and albedo. Future population distributions are derived from SSP 2 for the year 2100. (B) The number of urban individuals living in areas with extremely hot summer days ( $\gt$ 35 ∘C), extremely hot summer nights ( $\gt$ 20 ∘C), winter heating degree days (HDD: 18 ∘C minus average temperature), and summer cooling degree days (CDD: average temperature minus 18 ∘C). These thresholds are typically applied to air temperature or a heat index not LST and can only be used here to compare scenarios. Percentages shown are relative to current.
Drivers and projections of global surface temperature anomalies at the local scale

June 2021

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521 Reads

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26 Citations

More than half of the world’s population now lives in urban areas, and trends in rural-to-urban migration are expected to continue through the end of the century. Although cities create efficiencies that drive innovation and economic growth, they also alter the local surface energy balance, resulting in urban temperatures that can differ dramatically from surrounding areas. Here we introduce a global 1 km resolution data set of seasonal and diurnal anomalies in urban surface temperatures relative to their rural surroundings. We then use satellite-observable parameters in a simple model informed by the surface energy balance to understand the dominant drivers of present urban heating, the heat-related impacts of projected future urbanization, and the potential for policies to mitigate those damages. At present, urban populations live in areas with daytime surface summer temperatures that are 3.21 ∘C (−3.97, 9.24, 5th–95th percentiles) warmer than surrounding rural areas. If the structure of cities remains largely unchanged, city growth is projected to result in additional daytime summer surface temperature heat anomalies of 0.19 ∘C (−0.01, 0.47) in 2100—in addition to warming due to climate change. This is projected to raise the urban population living under extreme surface temperatures by approximately 20% compared to current distributions. However we also find a significant potential for mitigation: 82% of all urban areas have below average vegetation and/or surface albedo. Optimizing these would reduce urban daytime summer surface temperatures for the affected populations by an average of −0.81 ∘C (−2.55, −0.05).


Oaxaca-Blinder decomposition for farm income and subjective wellbeing indicators
Average values of outcome variables (standard deviation between parentheses)
Average values of explanatory variables (standard deviation between parentheses)
Estimates for the impacts of the MAIS (standard deviation between parentheses)
Improving production and quality of life for smallholder farmers through a climate resilience program: An experience in the Brazilian Sertão

May 2021

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76 Reads

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17 Citations

We use a combination of economic and wellbeing metrics to evaluate the impacts of a climate resilience program designed for family farmers in the semiarid region of Brazil. Most family farmers in the region are on the verge of income and food insufficiency, both of which are exacerbated in prolonged periods of droughts. The program assisted farmers in their milk and sheepmeat production, implementing a set of climate-smart production practices and locally-adapted technologies. We find that the program under evaluation had substantive and significant impacts on production practices, land management, and quality of life in general, using several different quasi-experimental strategies to estimate the average treatment effect on the treated farmers. We highlight the strengths and limitations of each evaluation strategy and how the set of analyses and outcome indicators complement each other. The evaluation provides valuable insights into the economic and environmental sustainability of family farming in semiarid regions, which are under growing pressure from climate change and environmental degradation worldwide.


Citations (22)


... Leveraging GEOS-Chem model and geographically weighted regression, van Donkelaar et al. (2021) attempted to produce a global monthly mean near-surface PM 2.5 concentration dataset from 1998 to 2021 with a spatial resolution of 0.1 • . As a representative dataset, it has been widely used for health-related haze exposure assessments globally (Ge et al., 2022;Hammer et al., 2020;Li et al., 2023;Polonik et al., 2023;Rentschler and Leonova, 2023). Additionally, several regional PM 2.5 concentration datasets have also been produced using versatile big data analytics approaches, such as CHAP , TAP (Geng et al., 2021), and LGHAP in China (Bai et al., 2022b), as well as daily and annual mean PM 2.5 concentrations for the contiguous United States (Di et al., 2019). ...

Reference:

SCAGAT: A scene-aware ensemble graph attention network for global PM 2.5 pollution mapping via land-atmosphere interactions
Air quality equity in US climate policy

Proceedings of the National Academy of Sciences

... Studies evaluating the impact of climate change on water deficiency and crop yield have shown that these effects may vary between regions, with potentially positive local impacts (Mohammadi et al., 2023;Zhang and Cai, 2013;Zhu et al., 2022). Moreover, inter-annual variability in crop production is expected to increase under climate change (Challinor et al., 2014), thereby heightening uncertainty for farmers regarding future yields. ...

Warming reduces global agricultural production by decreasing cropping frequency and yields

Nature Climate Change

... Excess N losses from rice production not only jeopardize water bodies, public health and economies but also worsen climate change 4,5 . The adverse impacts of climate change and pollution on rice production have been observed 6,7 , indicating that the global rice production system is both a victim of and a contributor to climate change and environmental pollution. Advisable agricultural management is needed to trade off rice production, GHG emissions and pollution and to prevent irreversible harm to food security, climate mitigation and environmental health, which are defined as the three sustainable indicators of agroecosystems in this study (Extended Data Fig. 1). ...

Globally ubiquitous negative effects of nitrogen dioxide on crop growth

Science Advances

... An indeterminate share of the high emissions recorded in non-industrialized countries could be seen as environmental leakage from richer nations. Studies of more recent periods highlight that the transfer of land-based emissions is particularly significant today (Hong et al., 2022;Pendrill et al., 2019). Given that deforestation and agricultural expansion were even more pronounced in the mid-20th century than they are now (Houghton et al., 1991;Meyfroidt and Lambin, 2011;Williams, 2003), it is plausible that land-based emissions transfers from the Global South to the Global North were considerable. ...

Land-use emissions embodied in international trade
  • Citing Article
  • May 2022

Science

... In addition, the pollution burden of a vibrant in-person economy (shopping/restaurants/ entertainment) can be disproportionately placed on low-income and racially minorized communities. Specifically, a study during the COVID-19 pandemic lockdowns in California observed reductions in pollution for Asian and Hispanic communities AMERICAN THORACIC SOCIETY DOCUMENTS near in-person economy hubs, whereas predominantly Black communities did not experience a reduction in pollution exposure, because their sources (e.g., power plants) were not shut down (154). Given community-specific exposures, an exemplary policy action that empowers communities to self-monitor is California Assembly Bill 617 (AB617). ...

Disparate air pollution reductions during California’s COVID-19 economic shutdown

Nature Sustainability

... However, it is important to note that excessive or inefficient irrigation practices can lead to water wastage, increased soil salinity, and environmental degradation [50]. Moreover, the sustainability of irrigation practices is a concern, particularly in the face of climate change and increasing water scarcity [51,52]. ...

Untangling irrigation effects on maize water and heat stress alleviation using satellite data

... Excessive urban heat can severely affect public health, increasing the risk of heat-related illnesses and mortality 17,18 , especially among vulnerable populations, such as older adults 19,20 , economically disadvantaged groups 21 , marginalized communities 22 , and outdoor workers 23,24 . Beyond health impacts, extreme heat also disrupts transportation system 25 , infrastructure vulnerability 26 , reduces economic productivity 27 , and deepens socioeconomic disparity 28,29 . ...

Widespread Race and Class Disparities in Surface Urban Heat Extremes Across the United States

... For instance, rising temperatures can increase non-methane volatile organic compound emissions from vegetation (Murray et al., 2024), and reduce dry deposition on plants (Lin et al., 2020), exacerbating ozone concentrations. Unfortunately, this crucial correlation is usually overlooked in the statistical crop models, thus plausibly leading to biased estimations of the temperature's influence on crop yield due to ozone omission (Carter et al., 2018;David B. ;Lobell & Burney, 2021). However, recent advancements in surface ozone retrieval techniques using machine learning algorithms and remote sensing data would have provided new insights into studying the elaborate interactions between ozone and crop yield (X. Liu et al., 2022;Montes et al., 2021). ...

Cleaner air has contributed one-fifth of U.S. maize and soybean yield gains since 1999

... Due to the extension to other thermal parameters we refer to them as urban-rural intensity differences. Based on the methodology developed by Benz et al (2021) for each pixel with a local temperature value T(u, v) the median comparable rural background temperaturē ( ) T u v r , , rural is subtracted (equation (2)). Comparable meaning within a 100 km radius r of the local pixel (therefore including pixel outside of Hesse when available) and with elevation differences of up to 100 m and similar slope aspects (north or south-facing). ...

Drivers and projections of global surface temperature anomalies at the local scale

... Es así como las TIC pueden ofrecer nuevos escenarios con múltiples propósitos que favorecen la producción del conocimiento rural a través de redes de aprendizaje y comunicaciones en tiempo real. Así, se podría mejorar la calidad de vida de las comunidades rurales mediante la revitalización del campo [4]. Para esto, la utilización de las TIC es de vital importancia, aplicando un concepto de territorio inteligente que permita el empoderamiento económico y social de las comunidades rurales. ...

Improving production and quality of life for smallholder farmers through a climate resilience program: An experience in the Brazilian Sertão