Our Research

  • New article in Science: "UV Dosage Levels in Summer: Increased Risk of Ozone Loss from Convectively Injected Water Vapor"
  • Overview of the StratoCruiser Concept for Long Duration Observations in and from the Stratosphere over the U.S. in Summer
  • While past climates have had high water vapor concentrations in the stratosphere, the Earth system has never simultaneously had high water vapor concentrations and high halogen loading.
  • The quantitative determination of methane and carbon dioxide isotopic fluxes from the most important source and sink regions constitutes a first order imperative in the union of energy, climate, and public policy.
  • The need for irrefutable observations to define the current state of the atmosphere is becoming increasingly critical. CO2.
  • A critical component of global change research is the integrity of the laboratory observations used in chemistry, radiation and climate.
  • The foundation for trusted quantitative forecasts of risk from the rapidly escalating, irreversible changes to the Earth’s climate structure driven by accelerating fossil fuel use, depends directly on fundamental advances in the quantitative determination of the physical, chemical and biological mechanisms controlling each of the major climate sub-systems. The manifold of risks to society from the continued use of fossil fuels requires quantitative forecasts of: (1) the increasing rate of sea level rise; (2) the rapid increases in the frequency, intensity and geographic extent of wild fires, (3) intensifying freshwater shortages, (4) severe storms with associated losses of life and property, (5) agricultural drought, (6) deadly heat waves; (7) glacial loss from regions that constitute the major water sources across multiple continents; as well as (9) forecasts of intensifying global refugee flow.

Research Area Overview

The Anderson group is engaged in a coupled array of research projects designed to establish the quantitative coupling between (1) the forcing of climate by increasing carbon dioxide and methane and other infrared active molecules, and (2) the feedbacks within the climate structure that set the time scale for global scale change. These research areas include:

  • The coupling between climate forcing and changes in the free radical catalytic chemistry that controls ultraviolet dosage at the Earth’s surface resulting from changes in stratospheric ozone
  • Mechanisms responsible for the increased flux of carbon isotopes into the atmosphere from melt zones in the Arctic, hydraulic fracturing of shale in the extraction of natural gas from shale, and the quantitative mapping of the nation’s carbon source/sink fluxes
  • Development of very high accuracy interferometers capable of observing the spectrally resolved infrared radiance emitted from Earth to Space from low Earth orbit that is capable of establishing a benchmark data set for the testing of climate forecast models
  • Observations of feedbacks that are triggered by the rapid loss of the permanent ice cover of the Arctic Ocean such as changes in the Greenland glacial structure and the flow of heat into other reservoirs of the climate system
  • Laboratory studies of the photochemistry and kinetics of free radicals and reactive intermediates involved in the chemistry of the troposphere and stratosphere.
  • Geoengineering directly involves a number of the feedbacks in the climate system that are addressed by the research group. The possibility that geoengineering would be considered on a global scale brings an imperative to quantitatively understand those feedbacks and how they couple.