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dc.contributor.authorMikhailenko, S. N.en
dc.contributor.authorKarlovets, E. V.en
dc.contributor.authorVasilchenko, S.en
dc.contributor.authorMondelain, D.en
dc.contributor.authorKassi, S.en
dc.contributor.authorCampargue, A.en
dc.date.accessioned2021-08-31T15:04:59Z-
dc.date.available2021-08-31T15:04:59Z-
dc.date.issued2019-
dc.identifier.citationNew transitions and energy levels of water vapor by high sensitivity CRDS near 1.73 and 1.54 µm / S. N. Mikhailenko, E. V. Karlovets, S. Vasilchenko, et al. — DOI 10.1016/j.jqsrt.2019.106574 // Journal of Quantitative Spectroscopy and Radiative Transfer. — 2019. — Vol. 236. — 106574.en
dc.identifier.issn224073-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Bronze3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85070739774&doi=10.1016%2fj.jqsrt.2019.106574&partnerID=40&md5=cc6e8cf201ef265af3eabff136914a2c
dc.identifier.urihttp://elar.urfu.ru/handle/10995/102702-
dc.description.abstractThis contribution is part of a long term project aiming at improving the water absorption spectroscopy by high sensitivity cavity ring down spectroscopy (CRDS) in the near infrared. Two new sources of CRDS spectra are considered: (i) The room temperature absorption spectrum of water vapor in natural isotopic abundance is recorded near 1.73 µm. A series of recordings was performed from 5693 to 5991 cm−1 with a pressure value of about 6 Torr. The noise equivalent absorption (αmin) of the spectra is better than 10− 10 cm−1. A total of 1453 lines were assigned to 1573 transitions of four water isotopologues (H2 16O, H2 17O, H2 18O and HD16O). Their intensities span more than five orders of magnitude from 3.0 × 10−30 to 4.7 × 10−25 cm/molecule at 296 K. The assignments were performed using known experimental energy levels as well as calculated line lists based on the results of Schwenke and Partridge. Two hundred fifty-one lines (assigned to 280 transitions) are observed for the first time and twelve energy levels are newly determined. The comparison of the obtained line parameters with those of the HITRAN database is discussed. Forty-six line positions are observed to significantly differ from their HITRAN values (δν = │νHITRAN – νCRDS│ > 0.02 cm−1). The derived set of energy levels is compared to those recommended by an IUPAC task group. (ii) The room temperature CRDS spectrum of water vapor highly enriched in 17O was recorded near 1.54 µm (6223–6672 cm−1) at a pressure of 12 Torr. Compared to a previous study, the higher pressure of the recordings allowed for extending the observations. Overall, twenty-six new levels were determined for both H2 17O and HD17O. All these observations together with other recent measurements will allow for an extension and an update of our empirical database in the 5693– 8340 cm−1 region. © 2019 Elsevier Ltden
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherElsevier Ltden
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceJ. Quant. Spectrosc. Radiat. Transf.2
dc.sourceJournal of Quantitative Spectroscopy and Radiative Transferen
dc.subjectCAVITY RING DOWN SPECTROSCOPYen
dc.subjectH2 17Oen
dc.subjectHD17Oen
dc.subjectHITRANen
dc.subjectISOTOPOLOGUEen
dc.subjectROVIBRATIONAL ASSIGNMENTSen
dc.subjectWATERen
dc.subjectBAND STRUCTUREen
dc.subjectINFRARED DEVICESen
dc.subjectLIGHT MEASUREMENTen
dc.subjectWATERen
dc.subjectWATER ABSORPTIONen
dc.subjectWATER VAPORen
dc.subjectCAVITY RING DOWN SPECTROSCOPIESen
dc.subjectH2^17Oen
dc.subjectHD^17Oen
dc.subjectHITRANen
dc.subjectISOTOPOLOGUESen
dc.subjectROVIBRATIONAL ASSIGNMENTen
dc.subjectABSORPTION SPECTROSCOPYen
dc.subjectATOMIC ABSORPTION SPECTROSCOPYen
dc.subjectDATABASEen
dc.subjectISOTOPIC ANALYSISen
dc.subjectSOFTWAREen
dc.subjectTEMPERATURE EFFECTen
dc.subjectWATER VAPORen
dc.titleNew transitions and energy levels of water vapor by high sensitivity CRDS near 1.73 and 1.54 µmen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1016/j.jqsrt.2019.106574-
dc.identifier.scopus85070739774-
local.contributor.employeeMikhailenko, S.N., V.E. Zuev Institute of Atmospheric Optics, SB, Russian Academy of Science, 1, Academician Zuev square, Tomsk, 634055, Russian Federation, Climate and Environmental Physics Laboratory, Ural Federal University, 19, Mira av, Yekaterinburg, 620002, Russian Federation
local.contributor.employeeKarlovets, E.V., Tomsk State University, Laboratory of Quantum Mechanics of Molecules and Radiative Processes, 36, Lenin Avenue, Tomsk, 634050, Russian Federation
local.contributor.employeeVasilchenko, S., V.E. Zuev Institute of Atmospheric Optics, SB, Russian Academy of Science, 1, Academician Zuev square, Tomsk, 634055, Russian Federation, Univ. Grenoble Alpes, CNRS, LIPhy, Grenoble, 38000, France
local.contributor.employeeMondelain, D., Univ. Grenoble Alpes, CNRS, LIPhy, Grenoble, 38000, France
local.contributor.employeeKassi, S., Univ. Grenoble Alpes, CNRS, LIPhy, Grenoble, 38000, France
local.contributor.employeeCampargue, A., Univ. Grenoble Alpes, CNRS, LIPhy, Grenoble, 38000, France
local.volume236-
local.contributor.departmentV.E. Zuev Institute of Atmospheric Optics, SB, Russian Academy of Science, 1, Academician Zuev square, Tomsk, 634055, Russian Federation
local.contributor.departmentClimate and Environmental Physics Laboratory, Ural Federal University, 19, Mira av, Yekaterinburg, 620002, Russian Federation
local.contributor.departmentTomsk State University, Laboratory of Quantum Mechanics of Molecules and Radiative Processes, 36, Lenin Avenue, Tomsk, 634050, Russian Federation
local.contributor.departmentUniv. Grenoble Alpes, CNRS, LIPhy, Grenoble, 38000, France
local.identifier.pure10474908-
local.identifier.puref485d46d-e592-4cf3-9665-37c66e041444uuid
local.description.order106574-
local.identifier.eid2-s2.0-85070739774-
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