Measurements and modeling of contemporary radiocarbon in the stratosphere
Measurements of the 14 C content of carbon dioxide in air collected by high-altitude balloon flights in 2003–2005 reveal the contemporary radiocarbon distribution in the northern midlatitude stratosphere, four decades after the Limited Test Ban Treaty restricted atmospheric testing of nuclear weapons. Comparisons with results from a 3-D chemical-transport model show that the 14 CO 2 distribution is now largely governed by the altitude/latitude dependence of the natural cosmogenic production rate, stratospheric transport, and propagation into the stratosphere of the decreasing radiocarbon trend in tropospheric CO 2 due to fossil fuel combustion. From the observed correlation of 14 CO 2 with N 2 O mixing ratios, an annual global mean net flux of 14 CO 2 to the troposphere of 1.6(±0.4) × 10 17 ‰ mol CO 2 yr –1 and a global production rate of 2.2(±0.6) × 10 26 atoms 14 C yr –1 are empirically derived. Furthermore, the results also indicate that contemporary 14 CO 2 observations provide highly sensitive diagnostics for stratospheric transport and residence times in models.