I. INTRODUCTIONPeroxy species are key intermediates in chemical reactions in both combustion 1, 2 and the troposphere 3,4 , which is the layer of the atmosphere extending from the Earth's surface to roughly 15 km in altitude, where temperature stops decreasing with altitude 5 . As is true for the study of reactive intermediates in general, advances in the understanding of peroxides have come from a dialog between theory-both electronic structure and statistical rate theory calculations-and experiment. This chapter focuses on the insights that electronic structure calculations, particularly those involving composite methods and density functional theory (DFT), have brought to peroxide chemistry. As much as possible, experimental results will be cited to validate or challenge the predictions of electronic structure theory. (While a direct comparison between electronic structure predictions and experimental data sometimes requires applications of statistical rate theory and other 1