
Paul Shepson
· Distinguished ProfessorStony Brook University · Sustainability Studies
Active 1981–2026
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About
Paul Shepson is a professor at Stony Brook University in the School of Marine and Atmospheric Sciences (SoMAS), where he conducts research on atmospheric chemistry and composition, interactions between the atmosphere and the surface, and the impacts of climate change on the physics, biology, and chemistry at the surface and in the atmosphere. His research group focuses on developing methods for quantifying greenhouse gas emission rates, particularly CO2 and CH4, from urban environments using aircraft-based measurements, tower observations, emissions models, and chemical transport models. This work connects to efforts at local, national, and international levels to mitigate climate change, and involves collaboration with organizations such as the National Institute for Standards and Technology (NIST). Shepson's research also includes studies of halogen chemistry in the Arctic Ocean environment, examining ocean-sea ice-snowpack-aerosol interactions that are changing due to climate change. His group has been involved in long-term Arctic research, including field projects in Alaska and campaigns like CHACHA, aimed at understanding atmospheric chemistry in the rapidly changing Arctic atmosphere. With a PhD from Pennsylvania State University obtained in 1982, Shepson has contributed extensively to the field through research on atmospheric chemistry, climate change, and related topics, with numerous publications and active involvement in grants and projects.
Research topics
- Statistics
- Atmospheric sciences
- Environmental chemistry
- Meteorology
- Organic chemistry
- Engineering
- Mathematics
- Geography
- Climatology
- Chemistry
Selected publications
Environmental Science & Technology Letters · 2020 · 81 citations
Organic aerosol (OA) is a complex mixture of compounds with diverse elemental and structural features, and its composition affects its health and environmental impacts. A detailed speciation of the functional group distribution in OA is important for constraining atmospheric reaction pathways and products, evaluating chemical mechanisms and models, and understanding OA impacts. We used high-resolution tandem mass spectrometry to perform a nontargeted analysis of OA functional groups from three d…
Environmental Science & Technology · 2020 · 72 citations
, and 13% for CO). Analysis of hourly reported emissions from power plants and traffic counts shows that 97% of the daily variability in posterior emissions estimates is explained by accounting for the sampling in time and space of sources that have large hourly variability and, thus, caution must be taken in properly interpreting variability that is caused by irregular spatiotemporal sampling conditions.
Atmospheric chemistry and physics · 2023-09-15 · 44 citations
articleOpen accessCorrespondingAbstract. The hydroxyl (OH), hydroperoxy (HO2), and organic peroxy (RO2) radicals play important roles in atmospheric chemistry. In the presence of nitrogen oxides (NOx), reactions between OH and volatile organic compounds (VOCs) can initiate a radical propagation cycle that leads to the production of ozone and secondary organic aerosols. Previous measurements of these radicals under low-NOx conditions in forested environments characterized by emissions of biogenic VOCs, including isoprene and m…
Underestimation of Thermogenic Methane Emissions in New York City
Environmental Science & Technology · 2024-05-14 · 14 citations
articleOpen accessSenior authorRecent studies have shown that methane emissions are underestimated by inventories in many US urban areas. This has important implications for climate change mitigation policy at the city, state, and national levels. Uncertainty in both the spatial distribution and sectoral allocation of urban emissions can limit the ability of policy makers to develop appropriately focused emission reduction strategies. Top-down emission estimates based on atmospheric greenhouse gas measurements can help to imp…
Tropospheric bromine monoxide vertical profiles retrieved across the Alaskan Arctic in springtime
Atmospheric chemistry and physics · 2024-01-03 · 9 citations
articleOpen accessAbstract. Reactive halogen chemistry in the springtime Arctic causes ozone depletion events and alters the rate of pollution processing. There are still many uncertainties regarding this chemistry, including the multiphase recycling of halogens and how sea ice impacts the source strength of reactive bromine. Adding to these uncertainties are the impacts of a rapidly warming Arctic. We present observations from the CHACHA (CHemistry in the Arctic: Clouds, Halogens, and Aerosols) field campaign ba…
Recent grants
A Multiphase Study of the Nature, Sources, and Fate of Atmospheric Organic Nitrogen
NSF · $751k · 2006–2013
NSF · $508k · 2007–2011
Studies of the Production of Molecular Halogens in Arctic Snowpacks and on Sea Ice Surfaces
NSF · $527k · 2011–2014
Frequent coauthors
- 124 shared
Brian H. Stirm
Purdue University West Lafayette
- 104 shared
A. Karion
National Institute of Standards and Technology
- 98 shared
Kerri A. Pratt
- 91 shared
Colm Sweeney
National Oceanic and Atmospheric Administration
- 77 shared
J. W. Bottenheim
Environment and Climate Change Canada
- 73 shared
J. C. Turnbull
University of Colorado Boulder
- 68 shared
K. R. Gurney
Northern Arizona University
- 66 shared
W. R. Simpson
University of Alaska Fairbanks
Education
- 1981
Ph.D., Atmospheric Chemistry
University of California, Los Angeles
- 1978
M.S., Atmospheric Chemistry
University of California, Los Angeles
- 1976
B.S., Chemistry
University of California, Los Angeles
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