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dc.contributor.authorVasilchenko, S.en
dc.contributor.authorMikhailenko, S. N.en
dc.contributor.authorCampargue, A.en
dc.date.accessioned2024-04-22T15:53:37Z-
dc.date.available2024-04-22T15:53:37Z-
dc.date.issued2022-
dc.identifier.citationVasilchenko, S, Mikhailenko, SN & Campargue, A 2022, 'Cavity ring down spectroscopy of water vapour near 750 nm: a test of the HITRAN2020 and W2020 line lists', Molecular Physics, Том. 120, № 15-16, e2051762. https://doi.org/10.1080/00268976.2022.2051762harvard_pure
dc.identifier.citationVasilchenko, S., Mikhailenko, S. N., & Campargue, A. (2022). Cavity ring down spectroscopy of water vapour near 750 nm: a test of the HITRAN2020 and W2020 line lists. Molecular Physics, 120(15-16), [e2051762]. https://doi.org/10.1080/00268976.2022.2051762apa_pure
dc.identifier.issn0026-8976
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access; Green Open Access3
dc.identifier.otherhttps://hal.science/hal-03865608/file/revised%203rd%20March.pdf1
dc.identifier.otherhttps://hal.science/hal-03865608/file/revised%203rd%20March.pdfpdf
dc.identifier.urihttp://elar.urfu.ru/handle/10995/132467-
dc.description.abstractCavity ring down spectroscopy (CRDS) is used to measure with unprecedented sensitivity and accuracy the weak water vapour spectrum in the 13,171–13,417 cm−1 region. A total of more than 1400 water lines are rovibrationally assigned to four isotopologues in natural isotopic abundance (H216O, H218O, H217O and HD16O), leading to the determination of 151 new levels and correction of 160 levels. The review of previous experimental works in the region is discussed. The comparison to the recent HITRAN2020 spectroscopic databases and to the W2020 line lists [Furtenbacher et al. J. Phys. Chem. Ref. Data 49 (2020) 043103; doi:10.1063/5.0030680] shows important discrepancies both for line positions and line intensities. A significant fraction of the W2020 line positions is inaccurate and shows deviations compared to measurements largely exceeding their claimed error bars. Line intensities are poorly predicted by available ab initio calculations in the considered region. A recommended line list mostly based on the present CRDS measurements is proposed. © 2022 Informa UK Limited, trading as Taylor & Francis Group.en
dc.description.sponsorshipIAO-Tomsken
dc.description.sponsorshipCentre National de la Recherche Scientifique, CNRS, (IRP SAMIA)en
dc.description.sponsorshipMinistry of Science and Higher Education of the Russian Federationen
dc.description.sponsorshipFunding text 1: The support of the CNRS (France) in the frame of International Research Project SAMIA is acknowledged. CRDS measurements and spectrum analysis were performed at IAO-Tomsk and funded by Ministry of Science and High Education of the Russian Federation.en
dc.description.sponsorshipFunding text 2: This work was supported by Centre National de la Recherche Scientifique [grant number IRP SAMIA]. The support of the CNRS (France) in the frame of International Research Project SAMIA is acknowledged. CRDS measurements and spectrum analysis were performed at IAO-Tomsk and funded by Ministry of Science and High Education of the Russian Federation.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherTaylor and Francis Ltd.en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.rightscc-byother
dc.sourceMolecular Physics2
dc.sourceMolecular Physicsen
dc.subjectABSORPTION SPECTROSCOPYen
dc.subjectH<SUB>2</SUB>Oen
dc.subjectHITRANen
dc.subjectROVIBRATIONAL ENERGY LEVELen
dc.subjectWATER VAPOURen
dc.subjectCALCULATIONSen
dc.subjectLIGHT MEASUREMENTen
dc.subjectWATER ABSORPTIONen
dc.subjectWATER PIPING SYSTEMSen
dc.subjectWATER VAPORen
dc.subjectCAVITY RING DOWN SPECTROSCOPIESen
dc.subjectH2Oen
dc.subjectHITRANen
dc.subjectLINE INTENSITIESen
dc.subjectLINE LISTSen
dc.subjectLINE POSITIONSen
dc.subjectRO-VIBRATIONAL ENERGIESen
dc.subjectROVIBRATIONAL ENERGY LEVELen
dc.subjectVAPOR SPECTRAen
dc.subjectWATER VAPOURen
dc.subjectABSORPTION SPECTROSCOPYen
dc.titleCavity ring down spectroscopy of water vapour near 750 nm: a test of the HITRAN2020 and W2020 line listsen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/submittedVersionen
dc.conference.name10 July 2021 through 11 July 2021en
dc.conference.date2021 International Scientific Forum on Sustainable Development and Innovation, WFSDI 2021
dc.identifier.doi10.1080/00268976.2022.2051762-
dc.identifier.scopus85126815687-
local.contributor.employeeVasilchenko S., V.E. Zuev Institute of Atmospheric Optics, Russian Academy of Science, SB, Tomsk, Russian Federationen
local.contributor.employeeMikhailenko S.N., V.E. Zuev Institute of Atmospheric Optics, Russian Academy of Science, SB, Tomsk, Russian Federation, Climate and Environmental Physics Laboratory, Ural Federal University, Yekaterinburg, Russian Federationen
local.contributor.employeeCampargue A., Univ. Grenoble Alpes, CNRS, LIPhy, Grenoble, Franceen
local.issue15-16
local.volume120
dc.identifier.wos000770276500001-
local.contributor.departmentV.E. Zuev Institute of Atmospheric Optics, Russian Academy of Science, SB, Tomsk, Russian Federationen
local.contributor.departmentClimate and Environmental Physics Laboratory, Ural Federal University, Yekaterinburg, Russian Federationen
local.contributor.departmentUniv. Grenoble Alpes, CNRS, LIPhy, Grenoble, Franceen
local.identifier.pure674dd195-ffe1-4f8c-a7a0-4d39f1046c2duuid
local.identifier.pure31781606-
local.description.ordere2051762
local.identifier.eid2-s2.0-85126815687-
local.identifier.wosWOS:000770276500001-
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