Evidence for a missing carbon monoxide sink based on tropospheric measurements of ¹⁴CO

An important problem in atmospheric chemistry is the determination of the oxidative capacity of the troposphere, which provides an index of how quickly trace gas species are destroyed. Central to this question are the abundance and distribution of hydroxyl radical, which is responsible for the destruction of a large proportion of chemical compounds such as CH 4 , CO, and nonmethane hydrocarbons. 14 CO can be used as a chemical tracer to help constrain the OH concentration, as oxidation via OH is the major sink for all carbon monoxide. We present the first 14 CO observations in the free troposphere during different seasons from 90°S to 34°N. Model simulations suggest that a large increase in the carbon monoxide sink strength may be needed in order to accommodate the experimental results.