High resolution absorption cross-sections and band oscillator strengths of the Schumann-Runge absorption bands of isotopic oxygen, 18O2, at 79 K

1988 ◽  
Vol 36 (11) ◽  
pp. 1201-1210 ◽  
Author(s):  
K. Yoshino ◽  
D.E. Freeman ◽  
J.R. Esmond ◽  
R.S. Friedman ◽  
W.H. Parkinson
Author(s):  
Brion Jean ◽  
A. Chakir ◽  
B. Coquart ◽  
D. Daumont ◽  
A. Jenouvrier ◽  
...  

1994 ◽  
Author(s):  
D. Malmasson ◽  
A. Vient ◽  
J. L. Lemaire ◽  
A. Le Floch ◽  
F. Rostas

1977 ◽  
Vol 50 (1) ◽  
pp. 101-106 ◽  
Author(s):  
P.H. Wine ◽  
A.R. Ravishankara ◽  
D.L. Philen ◽  
D.D. Davis ◽  
R.T. Watson

2005 ◽  
Vol 7 (1) ◽  
pp. 79 ◽  
Author(s):  
Francis D. Pope ◽  
Carina A. Smith ◽  
Michael N. R. Ashfold ◽  
Andrew J. Orr-Ewing

2015 ◽  
Vol 1 ◽  
pp. 20-25 ◽  
Author(s):  
Robert J. Hargreaves ◽  
Eric Buzan ◽  
Michael Dulick ◽  
Peter F. Bernath

2015 ◽  
Vol 8 (6) ◽  
pp. 5895-5936 ◽  
Author(s):  
J. Lampel ◽  
D. Pöhler ◽  
J. Tschritter ◽  
U. Frieß ◽  
U. Platt

Abstract. In recent updates of the HITRAN water vapour H2O spectroscopic compilation covering the blue spectral region (here: 394–480 nm) significant changes for the absorption bands at 416 and 426 nm were reported. In order to investigate the consistency of the different cross-sections calculated from these compilations, H2O vapour column density ratios for different spectral intervals were retrieved from Long-path and Multi-Axis – Differential Optical Absorption Spectroscopy (DOAS) measurements. We observed a significant improvement of the DOAS evaluation when using the updated HITRAN water vapour absorption cross-sections for the calculation of the reference spectra. In particular the magnitudes of the residual spectra as well as the fit errors were reduced. However we also found that the best match between measurement and model is reached when the absorption cross-section of groups of lines are scaled by factors ranging from 0.5 and 1.9, suggesting that the HITRAN water vapour absorption compilation still needs significant corrections. For this spectral region we present correction factors for HITRAN 2009, HITRAN 2012, HITEMP and BT2 derived from field measurements. Additionally, upper limits for water vapour absorption in the UV-A range from 330–390 nm are given.


2016 ◽  
Vol 9 (6) ◽  
pp. 2593-2601 ◽  
Author(s):  
Jeremy J. Harrison

Abstract. The most widely used hydrochlorofluorocarbon (HCFC) commercially since the 1930s has been chloro-difluoromethane, or HCFC-22, which has the undesirable effect of depleting stratospheric ozone. As this molecule is currently being phased out under the Montreal Protocol, monitoring its concentration profiles using infrared sounders crucially requires accurate laboratory spectroscopic data. This work describes new high-resolution infrared absorption cross sections of chlorodifluoromethane over the spectral range 730–1380 cm−1, determined from spectra recorded using a high-resolution Fourier transform spectrometer (Bruker IFS 125HR) and a 26 cm pathlength cell. Spectra of chlorodifluoromethane/dry synthetic air mixtures were recorded at resolutions between 0.01 and 0.03 cm−1 (calculated as 0.9/MOPD; MOPD denotes the maximum optical path difference) over a range of temperatures and pressures (7.5–762 Torr and 191–295 K) appropriate for atmospheric conditions. This new cross-section dataset improves upon the one currently available in the HITRAN (HIgh-resolution TRANsmission) and GEISA (Gestion et Etude des Informations Spectroscopiques Atmosphériques) databases; in particular it provides coverage over a wider range of pressures and temperatures, has more accurate wavenumber scales, more consistent integrated band intensities, improved signal-to-noise, is free of channel fringing, and additionally covers the ν2 and ν7 bands.


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