My research group studies how aerosol formation and the oxidative capacity of the atmosphere change in response to both climate change and anthropogenic activities. We aim to answer two fundamental questions in atmospheric chemistry:
1.How do the formation pathways of sulfate and nitrate aerosols vary over space and time, and what are the implications for atmospheric chemistry and climate?
2.How has the oxidation capacity of the atmosphere changed in response to both anthropogenic and climate forcing, and what are the implications for climate feedback processes via the impact on the concentration of reduced trace gases (e.g. CH4) that affect the distribution of energy in the climate system?
The main approaches that we use to answer the above questions are:
1.Measuring the isotopic composition of sulfate and nitrate from aerosol, water, snow, and ice core samples (see our laboratory facilities).
2.Modeling using global three-dimensional models of atmospheric chemistry and climate (mostly GEOS-Chem).
