Supplementary material in electronic form for the paper WATER SPECTRA IN THE 4200-6250 cm-1 REGION: EXTENDED ANALYSIS OF n1+n2, n2+n3, AND 3n2 BANDS AND CONFIRMATION OF HIGHLY EXCITED STATES FROM FLAME SPECTRA AND FROM ATMOSPHERIC LONG-PATH OBSERVATIONS by (1) S.N. MIKHAILENKO, (2) VL.G. TYUTEREV, (1) V.I. STARIKOV, (3) K.K. ALBERT, (3,#) B.P. WINNEWISSER, (3,#) M. WINNEWISSER, (3) G. MELLAU, (4) C. CAMY-PEYRET, (4) R. LANQUETIN, (5) J.-M. FLAUD and (6) J.W. BRAULT (1) Institute of Atmospheric Optics, Russian Academy of Sciences, 1, av.Akademicheskii, 634055 Tomsk, Russia (2) Groupe de Spectrometrie Moleculaire et Atmospherique, UMR CNRS 6089, Universite de Reims, Faculte des Sciences, Moulin de la Housse, BP 1039, 51687 Reims Cedex 2, France (3) Justus-Liebig-Universitaet Giessen, Heinrich-Buff-Ring 58, D-35392 Giessen, Germany (4)Laboratoire de Physique Moleculaire et Applications, Universite Pierre et Marie Curie, Tour 13, Bte 76, 4 place Jussieu, 75252 Paris Cedex 05, France (5)Laboratoire de Photophysique Moleculaire, Universite Paris-Sud, Bat. 350, 91405 Orsay, France (6)Laboratory for Atmospheric and Space Physics, Campus Box 590, Univ. of Colorado, Boulder, CO 80309-0590 (#) Present address: Department of Physics, The Ohio State University, Columbus, Ohio USA 43210 submitted to Journal of Molecular Spectroscopy. ----------------------------------------------------------------- Appendix 5. H2_17O and H2_18O lines observed in laboratory room temperature spectra in the transparency window 4200-5000 cm-1 Observed line positions [in cm-1]. Line intensities in cm-1 / molecule cm-2 at T=296K. Intensity is taken from HITRAN-2000 database. (*) means that a line is absent from HITRAN, in this case the intensity calculated from ab initio dipole moment surface by Partridge and Schwenke PS(24) is given. ---------------------------------------------------------------------- A auxiliary peaklist provided "as is" without profile fits and intensity measurements, just to give information for atmospheric applications that these lines should be there at natural abundance. The accuracy of line positions in this file is ~ 2-3*10-3 cm-1. ---------------------------------------------------------------------- Observed line positions Observed line calculated position intensities iso v1v2v3 J Ka Kc v1v2v3 J Ka Kc P HITRAN/PS(*) upper lower sam 4200.9802 4.67E-26 H2O18 001 10 6 4 000 9 4 5 p 4201.0227 3.09E-26 H2O18 001 10 5 6 000 9 3 7 p 4206.6933 1.56E-26 H2O17 001 9 6 4 000 8 4 5 p 4208.6621 3.98E-26 H2O18 001 10 4 7 000 9 2 8 p 4209.8076 3.34E-26 H2O18 001 8 7 1 000 7 5 2 p 4220.8885 1.45E-26 H2O18 001 10 6 5 000 9 4 6 q 4229.2539 1.38E-26 H2O18 001 12 4 8 000 11 2 9 q 4232.0537 2.56E-26 H2O18 001 9 7 3 000 8 5 4 p 4235.4706 8.53E-26 H2O18 001 10 2 8 000 9 0 9 p 4235.6960 3.58E-26 H2O18 001 11 5 7 000 10 3 8 p 4236.4242 1.48E-26 H2O18 001 11 3 8 000 10 1 9 p 4242.7246 1.73E-26 H2O17 001 10 2 8 000 9 0 9 p 4243.5290 7.47E-27 * H2O17 001 11 5 7 000 10 3 8 q 4245.6789 1.90E-26 H2O18 001 11 6 6 000 10 4 7 p 4254.2079 4.27E-26 H2O18 001 11 4 8 000 10 2 9 p 4288.4940 1.06E-26 H2O18 001 11 2 9 000 10 0 10 q 4290.7066 3.18E-26 H2O18 001 11 3 9 000 10 1 10 p 4290.8139 1.37E-26 H2O18 001 12 3 9 000 11 1 10 p 4298.2365 7.23E-27 * H2O17 001 11 3 9 000 10 1 10 q 4340.1498 1.11E-26 H2O18 001 12 2 10 000 11 0 11 q 4391.2355 4.31E-27 * H2O18 001 13 3 11 000 12 1 12 q 4476.4346 7.80E-27 * H2O18 030 8 1 8 000 9 0 9 q 4497.9896 3.62E-27 * H2O18 030 5 2 3 000 6 3 4 q 4513.9496 7.08E-27 * H2O18 030 6 0 6 000 7 1 7 q 4517.5321 2.19E-26 * H2O18 030 6 1 6 000 7 0 7 q 4531.3377 7.86E-27 * H2O18 030 3 2 1 000 4 3 2 q 4531.4420 2.88E-26 * H2O18 030 5 0 5 000 6 1 6 p 4539.2287 1.20E-26 * H2O18 030 3 1 2 000 4 2 3 q 4547.4892 1.12E-26 * H2O18 030 4 0 4 000 5 1 5 q 4558.5896 3.64E-26 * H2O18 030 4 1 4 000 5 0 5 p 4562.4069 3.34E-26 * H2O18 030 3 0 3 000 4 1 4 p 4603.6359 2.85E-26 * H2O18 030 2 1 2 000 3 0 3 p 4721.2263 5.41E-27 * H2O18 030 4 1 3 000 4 0 4 t 4755.6696 1.55E-26 * H2O18 030 2 2 1 000 2 1 2 t 4809.5199 7.70E-27 * H2O18 030 6 2 5 000 6 1 6 t 4817.9959 9.05E-27 * H2O18 030 5 3 2 000 5 2 3 t 4831.4364 1.22E-26 * H2O18 030 3 3 0 000 3 2 1 t 4840.6495 1.45E-26 * H2O18 030 4 3 2 000 4 2 3 t 4878.2049 5.57E-27 H2O18 110 6 1 6 000 7 2 5 t 4878.8084 4.44E-27 H2O18 011 6 4 2 000 7 6 1 t 4883.0659 8.98E-27 H2O18 011 7 1 7 000 8 3 6 t 4885.6762 8.52E-27 H2O18 011 7 3 5 000 8 5 4 t 4888.5704 6.85E-27 H2O18 110 8 4 5 000 9 5 4 t 4903.4009 4.50E-27 H2O18 011 5 4 2 000 6 6 1 t 4908.7579 2.62E-26 * H2O18 030 3 3 0 000 2 2 1 t 4910.1584 4.88E-27 H2O18 011 7 3 4 000 8 5 3 t 4926.4679 7.07E-27 H2O18 110 7 4 3 000 8 5 4 t 4927.6831 1.99E-26 H2O18 011 6 3 3 000 7 5 2 t 4936.3659 7.94E-27 H2O18 011 6 1 6 000 7 3 5 t 4939.9079 1.31E-26 H2O18 011 8 2 6 000 9 4 5 t 4940.8539 1.07E-26 H2O18 011 6 2 5 000 7 4 4 t 4940.9549 7.49E-27 H2O18 110 6 6 1 000 7 7 0 t 4943.5564 1.34E-26 H2O18 110 6 5 2 000 7 6 1 t 4943.5819 4.46E-27 H2O18 110 6 5 1 000 7 6 2 t 4947.3973 7.97E-27 H2O18 011 5 3 2 000 6 5 1 t 4950.5789 1.51E-26 H2O18 110 6 4 3 000 7 5 2 s 4954.0659 9.31E-27 H2O18 110 7 3 4 000 8 4 5 t 4954.3417 3.47E-26 H2O18 110 6 3 4 000 7 4 3 s 4964.3679 1.19E-26 H2O18 011 7 1 6 000 8 3 5 t 4968.0727 3.63E-26 H2O18 011 6 0 6 000 7 2 5 s 4968.5918 6.62E-27 H2O18 011 4 3 2 000 5 5 1 t 4969.9950 2.96E-26 H2O18 110 5 5 0 000 6 6 1 s 4970.9579 7.05E-27 H2O18 110 6 3 3 000 7 4 4 t 4975.4146 5.62E-27 * H2O17 110 5 5 0 000 6 6 1 t 4976.2677 6.11E-27 H2O18 110 3 0 3 000 4 3 2 t 4976.4753 6.80E-26 H2O18 011 5 2 4 000 6 4 3 s 4976.8509 1.37E-26 H2O18 110 5 4 2 000 6 5 1 t 4977.0144 4.24E-26 H2O18 110 5 4 1 000 6 5 2 s 4981.2279 1.76E-26 H2O18 110 5 2 4 000 6 3 3 t 4981.2779 5.59E-27 * H2O18 011 14 0 14 000 15 0 15 t 4984.9874 2.67E-26 H2O18 110 5 3 3 000 6 4 2 s 4986.0761 5.55E-26 H2O18 011 5 1 5 000 6 3 4 s 4990.6173 6.16E-27 * H2O17 110 5 3 3 000 6 4 2 t 4991.1300 4.61E-26 H2O18 011 6 2 4 000 7 4 3 s 4991.9694 3.83E-26 H2O18 110 5 3 2 000 6 4 3 s 4994.7859 1.59E-26 * H2O17 011 5 1 5 000 6 3 4 t 4997.4396 3.81E-26 H2O18 110 4 1 4 000 5 2 3 s 4999.1254 1.27E-26 * H2O17 011 6 2 4 000 7 4 3 t ----------------------------------------------------------------------