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Sebastian D. Eastham

Sebastian D. Eastham

· Research Scientist, Laboratory for Aviation and the Environment, MIT Department of Aeronautics and Astronautics

Harvard University

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Research topics

  • Geology
  • Environmental science
  • Geography
  • Meteorology
  • Medicine
  • Agroforestry
  • Physical chemistry
  • Ecology
  • Environmental protection
  • Toxicology
  • Chemistry
  • Biology
  • Atmospheric sciences
  • Environmental health
  • Forestry
  • Socioeconomics
  • Organic chemistry
  • Nuclear physics
  • Physics
  • Climatology

Selected publications

  • Air quality impacts of crop residue burning in India and mitigation alternatives

    Nature Communications · 2022 · 189 citations

    • Environmental science
    • Toxicology
    • Environmental health

    Crop residue burning contributes to poor air quality and imposes a health burden on India. Despite government bans and other interventions, this practice remains widespread. Here we estimate the impact of changes in agricultural emissions on air quality across India and quantify the potential benefit of district-level actions using an adjoint modeling approach. From 2003 to 2019, we find that agricultural residue burning caused 44,000-98,000 particulate matter exposure-related premature deaths annually, of which Punjab, Haryana, and Uttar Pradesh contribute 67-90%. Due to a combination of relatively high downwind population density, agricultural output, and cultivation of residue-intensive crops, six districts in Punjab alone contribute to 40% of India-wide annual air quality impacts from residue burning. Burning two hours earlier in Punjab alone could avert premature deaths up to 9600 (95% CI: 8000-11,000) each year, valued at 3.2 (95% CI: 0.49-7.3) billion US dollars. Our findings support the use of targeted and potentially low-cost interventions to mitigate crop residue burning in India, pending further research regarding cost-effectiveness and feasibility.

  • Global tropospheric halogen (Cl, Br, I) chemistry and its impact on oxidants

    Atmospheric chemistry and physics · 2021 · 195 citations

    • Chemistry
    • Atmospheric sciences
    • Physical chemistry

    Abstract. We present an updated mechanism for tropospheric halogen (Cl + Br + I) chemistry in the GEOS-Chem global atmospheric chemical transport model and apply it to investigate halogen radical cycling and implications for tropospheric oxidants. Improved representation of HOBr heterogeneous chemistry and its pH dependence in our simulation leads to less efficient recycling and mobilization of bromine radicals and enables the model to include mechanistic sea salt aerosol debromination without generating excessive BrO. The resulting global mean tropospheric BrO mixing ratio is 0.19 ppt (parts per trillion), lower than previous versions of GEOS-Chem. Model BrO shows variable consistency and biases in comparison to surface and aircraft observations in marine air, which are often near or below the detection limit. The model underestimates the daytime measurements of Cl2 and BrCl from the ATom aircraft campaign over the Pacific and Atlantic, which if correct would imply a very large missing primary source of chlorine radicals. Model IO is highest in the marine boundary layer and uniform in the free troposphere, with a global mean tropospheric mixing ratio of 0.08 ppt, and shows consistency with surface and aircraft observations. The modeled global mean tropospheric concentration of Cl atoms is 630 cm−3, contributing 0.8 % of the global oxidation of methane, 14 % of ethane, 8 % of propane, and 7 % of higher alkanes. Halogen chemistry decreases the global tropospheric burden of ozone by 11 %, NOx by 6 %, and OH by 4 %. Most of the ozone decrease is driven by iodine-catalyzed loss. The resulting GEOS-Chem ozone simulation is unbiased in the Southern Hemisphere but too low in the Northern Hemisphere.

  • Air Quality and Climate Impacts of United States Nuclear Power Plant Closures

    AGU Fall Meeting Abstracts · 2020

    • Environmental science
    • Climatology
    • Meteorology

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