Infrared solar spectra recorded at the International Scientific Station of the Jungfraujoch (3580 m altitude), Switzerland, in 1950–1951 and from 1984 to 1992 have been analyzed to determine vertical column abundances of nitrous oxide (N2O) above the station. The best fit to the relatively dense set of measurements made between 1984 and 1992 indicates a mean exponential rate of increase equal to 0.36 ± 0.06% yr−1 (1 σ) and a seasonal modulation of 7.2% peak to peak, the minimum occurring at the end of the winter and the maximum in early September. The column abundances for April of the years 1951, 1984, and 1992 were found equal to 3.49 × 1018, 3.76 × 1018, and 3.87 × 1018 molecules cm−2, respectively; they translate into N2O concentrations at the altitude of the Jungfraujoch equal to 275, 296, and 305 parts per billion by volume. These results indicate that the exponential rate of increase for 1951–1984 was equal to 0.23 ± 0.04% yr−1 (1σ), thus substantially lower than for the 1984–1992 time interval and that the so‐called preindustrial levels of N2O pertained until 1951 with most of the increase in atmospheric N2O occurring thereafter
