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dc.contributor.authorMikhailenko, S. N.en
dc.contributor.authorKassi, S.en
dc.contributor.authorMondelain, D.en
dc.contributor.authorCampargue, A.en
dc.date.accessioned2021-08-31T15:01:18Z-
dc.date.available2021-08-31T15:01:18Z-
dc.date.issued2020-
dc.identifier.citationWater vapor absorption between 5690 and 8340 cm−1: Accurate empirical line centers and validation tests of calculated line intensities / S. N. Mikhailenko, S. Kassi, D. Mondelain, et al. — DOI 10.1016/j.jqsrt.2020.106840 // Journal of Quantitative Spectroscopy and Radiative Transfer. — 2020. — Vol. 245. — 106840.en
dc.identifier.issn224073-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Bronze, Green3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85079165230&doi=10.1016%2fj.jqsrt.2020.106840&partnerID=40&md5=6755e7ba92de4f010b0c11d520fdffd8
dc.identifier.urihttp://elar.urfu.ru/handle/10995/102017-
dc.description.abstractAn accurate empirical list of 57,995 transitions is constructed for natural water in the 5690–8340 cm−1 near infrared region (1.76–1.20 µm). The new list represents an updated version of the list reported in Mikhailenko et al. (2016). The spectral range is extended to lower energy and the transition frequencies benefited from a series of recent measurements by comb-assisted cavity ring down spectroscopy (CA-CRDS). The line list construction uses as starting point the variational line lists computed on the basis of the results of Schwenke and Partridge for the six most abundant water isotopologues (H2 16O, H2 18O, H2 17O, HD16O, HD18O, HD17O). Variational line positions are replaced by position values calculated from empirical rotation-vibration energy levels. The set of required empirical energy levels is improved in accuracy and enlarged, in particular for the minor isotopologues. A large number of energy levels and thus transition frequencies, relying on spectra recorded by CA-CRDS, have accuracy on the order of 10−4 cm−1. All the transitions are provided with unique vibrational labeling supported by effective Hamiltonian calculations in case of ambiguity. A detailed comparison is presented with the list of natural water included in the HITRAN2016 database and with the very recent H2 16O and H2 18O lists reported in Conway et al. (2020). The advantage of our list in terms of line position accuracy is demonstrated and illustrated by direct comparison with CRDS recordings at disposal. Intensity comparison shows a general agreement but a number of weaknesses of the most recent intensity calculations are evidenced. All the considered theoretical line lists include a few bands (e.g. 4ν2, 5ν2, ν1+2ν2 and ν1+3ν2) with intensities deviating significantly from the observations. © 2020 Elsevier Ltden
dc.description.sponsorshipE.K. Conway (Center for Astrophysics, Cambridge and University College London) is acknowledged for providing us the submitted version of Ref. [44] together with the corresponding H216O and H218O lists, prior publication. The support of the University Grenoble Alpes and CNRS (France) in the frame of International Research Project SAMIA is acknowledged. SNM activity was also partly supported in the frame of the Russian Science Foundation, grant no. 18-11-00024.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherElsevier Ltden
dc.relationinfo:eu-repo/grantAgreement/RSF//18-11-00024en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceJ. Quant. Spectrosc. Radiat. Transf.2
dc.sourceJournal of Quantitative Spectroscopy and Radiative Transferen
dc.subjectABSORPTION SPECTROSCOPYen
dc.subjectCAVITY RING DOWN SPECTROSCOPYen
dc.subjectGEISAen
dc.subjectH2Oen
dc.subjectHITRANen
dc.subjectSPECTROSCOPIC DATABASEen
dc.subjectWATER VAPORen
dc.subjectBAND STRUCTUREen
dc.subjectINFRARED DEVICESen
dc.subjectLIGHT MEASUREMENTen
dc.subjectWATER ABSORPTIONen
dc.subjectWATER VAPORen
dc.subjectCAVITY RING DOWN SPECTROSCOPIESen
dc.subjectEFFECTIVE HAMILTONIANen
dc.subjectGEISAen
dc.subjectHITRANen
dc.subjectNEAR INFRARED REGIONen
dc.subjectSPECTROSCOPIC DATABASEen
dc.subjectTRANSITION FREQUENCIESen
dc.subjectWATER-VAPOR ABSORPTIONen
dc.subjectABSORPTION SPECTROSCOPYen
dc.subjectABSORPTIONen
dc.subjectACCURACY ASSESSMENTen
dc.subjectCOMPARATIVE STUDYen
dc.subjectEXPERIMENTAL STUDYen
dc.subjectMODEL VALIDATIONen
dc.subjectWATER VAPORen
dc.titleWater vapor absorption between 5690 and 8340 cm−1: Accurate empirical line centers and validation tests of calculated line intensitiesen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1016/j.jqsrt.2020.106840-
dc.identifier.scopus85079165230-
local.contributor.employeeMikhailenko, S.N., Laboratory of Theoretical Spectroscopy, 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.employeeKassi, S., CNRS, LIPhy, Université Grenoble Alpes, Grenoble, 38000, France
local.contributor.employeeMondelain, D., CNRS, LIPhy, Université Grenoble Alpes, Grenoble, 38000, France
local.contributor.employeeCampargue, A., CNRS, LIPhy, Université Grenoble Alpes, Grenoble, 38000, France
local.volume245-
dc.identifier.wos000534641000003-
local.contributor.departmentLaboratory of Theoretical Spectroscopy, V.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.departmentCNRS, LIPhy, Université Grenoble Alpes, Grenoble, 38000, France
local.identifier.pure0bf60ef6-bf48-49aa-8b83-a50cf7eca410uuid
local.identifier.pure12246643-
local.description.order106840-
local.identifier.eid2-s2.0-85079165230-
local.fund.rsf18-11-00024-
local.identifier.wosWOS:000534641000003-
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