Multi-decade measurements of the long-term trends of atmospheric species by high-spectral-resolution infrared solar absorption spectroscopy

Solar absorption spectra were recorded for the first time in 5 years with the McMath Fourier transform spectrometer at the US National Solar Observatory on Kitt Peak in southern Arizona, USA (31.91°N latitude, 111.61°W longitude, 2.09 km altitude). The solar absorption spectra cover 750–1300 and 185...

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Veröffentlicht in:Journal of quantitative spectroscopy & radiative transfer 2010-02, Vol.111 (3), p.376-383
Hauptverfasser: Rinsland, Curtis P., Chiou, Linda, Goldman, Aaron, Hannigan, James W.
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Sprache:eng
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Zusammenfassung:Solar absorption spectra were recorded for the first time in 5 years with the McMath Fourier transform spectrometer at the US National Solar Observatory on Kitt Peak in southern Arizona, USA (31.91°N latitude, 111.61°W longitude, 2.09 km altitude). The solar absorption spectra cover 750–1300 and 1850–5000 cm −1 and were recorded on 20 days during March–June 2009. The measurements mark the continuation of a long-term record of atmospheric chemical composition measurements that have been used to quantify seasonal cycles and long-term trends of both tropospheric and stratospheric species from observations that began in 1977. Fits to the measured spectra have been performed, and they indicate the spectra obtained since return to operational status are nearly free of channeling and the instrument line shape function is well reproduced taking into account the measurement parameters. We report updated time series measurements of total columns for six atmospheric species and their analysis for seasonal cycles and long-term trends. As an example, the time series fit shows a decrease in the annual increase rate in Montreal-Protocol-regulated chlorofluorocarbon CCl 2F 2 from 1.51±0.38% yr −1 at the beginning of the time span to −1.54±1.28% yr −1 at the end of the time span, 1 sigma, and hence provides evidence for the impact of those regulations on the trend.
ISSN:0022-4073
1879-1352
DOI:10.1016/j.jqsrt.2009.09.012