{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282681481756672.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj.2014-a13"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"025797983"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/025797983"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I025797983"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmsj/92A/0/92A_2014-A13/_pdf"}},{"identifier":{"@type":"NAID","@value":"40020204470"}},{"identifier":{"@type":"NAID","@value":"130004704190"}}],"dc:title":[{"@language":"en","@value":"Column Water Vapor Retrievals from Sky Radiometer (POM-02) 940 nm Data"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Sky radiometer data are used to retrieve aerosol optical properties and to estimate the effect of aerosols on solar irradiance at the Earth’s surface. The Prede POM-02 is equipped with a 940-nm channel corresponding to a primary water vapor absorption band in the near infrared region, but 940-nm data have been underutilized. Atmospheric water vapor is an important factor in determining the surface radiation budget. To retrieve the columnar precipitable water vapor amount from sun-sky radiometers, the 940-nm channel was calibrated using the Langley method, which accounts for gas absorption. The relation between column water vapor and atmospheric transmittance at 940 nm was determined using simulation data, and the results were used to retrieve column water vapor. This method was applied to data collected at Tsukuba, Japan, in 2011 and compared with global positioning system receiver (GPS), microwave radiometer, and radiosonde water vapor retrievals. The highest correlations were found between GPS and radiosonde observations. A comparison of POM-02 and GPS results showed a bias error of 0.09 g cm<sup>-2</sup>; the root mean square error was 0.179 g cm<sup>-2</sup>; and <i>r</i> = 0.996. The transmittance of the 940-nm channel was theoretically determined in this study. Therefore, the accuracy of column water vapor retrieval depends on the accuracy of transmittance calculation model."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658806288896","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50354460"},{"@type":"NRID","@value":"1000050354460"},{"@type":"NRID","@value":"9000002717503"},{"@type":"NRID","@value":"9000363501953"},{"@type":"NRID","@value":"9000363405735"},{"@type":"NRID","@value":"9000249866671"},{"@type":"NRID","@value":"9000363406249"},{"@type":"NRID","@value":"9000387906207"},{"@type":"NRID","@value":"9000392819386"},{"@type":"NRID","@value":"9000363481438"},{"@type":"NRID","@value":"9000370746725"},{"@type":"NRID","@value":"9000363405883"},{"@type":"NRID","@value":"9000272990631"},{"@type":"NRID","@value":"9000257767980"},{"@type":"NRID","@value":"9000257767263"},{"@type":"NRID","@value":"9000264268235"},{"@type":"NRID","@value":"9000363250898"},{"@type":"NRID","@value":"9000290819250"},{"@type":"NRID","@value":"9000272990613"},{"@type":"NRID","@value":"9000363480178"},{"@type":"NRID","@value":"9000363495689"},{"@type":"NRID","@value":"9000392819466"},{"@type":"NRID","@value":"9000363408415"},{"@type":"NRID","@value":"9000367417673"},{"@type":"NRID","@value":"9000363480581"},{"@type":"NRID","@value":"9000392816692"},{"@type":"NRID","@value":"9000257828073"},{"@type":"NRID","@value":"9000363407246"},{"@type":"NRID","@value":"9000363407248"},{"@type":"NRID","@value":"9000363407461"},{"@type":"NRID","@value":"9000363409152"},{"@type":"NRID","@value":"9000363408386"},{"@type":"NRID","@value":"9000363481101"},{"@type":"NRID","@value":"9000008181012"},{"@type":"NRID","@value":"9000363410752"},{"@type":"NRID","@value":"9000363411196"},{"@type":"NRID","@value":"9000363404174"},{"@type":"NRID","@value":"9000363405079"},{"@type":"NRID","@value":"9000363409014"},{"@type":"NRID","@value":"9000363406478"},{"@type":"NRID","@value":"9000272990607"},{"@type":"NRID","@value":"9000360551822"},{"@type":"NRID","@value":"9000392816595"},{"@type":"NRID","@value":"9000363405538"},{"@type":"NRID","@value":"9000253481510"},{"@type":"NRID","@value":"9000392819392"},{"@type":"NRID","@value":"9000272990637"},{"@type":"NRID","@value":"9000363411384"},{"@type":"NRID","@value":"9000363408413"},{"@type":"NRID","@value":"9000363410748"},{"@type":"NRID","@value":"9000363405253"},{"@type":"NRID","@value":"9000363408378"},{"@type":"NRID","@value":"9000363407862"},{"@type":"NRID","@value":"9000363406252"},{"@type":"NRID","@value":"9000363408384"},{"@type":"NRID","@value":"9000363408322"},{"@type":"NRID","@value":"9000363480095"},{"@type":"NRID","@value":"9000240064507"},{"@type":"NRID","@value":"9000283593457"},{"@type":"NRID","@value":"9000363405809"},{"@type":"NRID","@value":"9000363403155"},{"@type":"NRID","@value":"9000363483044"},{"@type":"NRID","@value":"9000363402832"},{"@type":"NRID","@value":"9000363489408"},{"@type":"NRID","@value":"9000363400588"},{"@type":"NRID","@value":"9000363402301"},{"@type":"NRID","@value":"9000363498607"},{"@type":"NRID","@value":"9000363403180"},{"@type":"NRID","@value":"9000363403463"},{"@type":"NRID","@value":"9000363498593"},{"@type":"NRID","@value":"9000363402594"},{"@type":"NRID","@value":"9000363404669"},{"@type":"NRID","@value":"9000363401865"},{"@type":"NRID","@value":"9000363402090"},{"@type":"NRID","@value":"9000363402592"},{"@type":"NRID","@value":"9000363400584"},{"@type":"NRID","@value":"9000363401463"},{"@type":"NRID","@value":"9000363400572"},{"@type":"NRID","@value":"9000363402584"},{"@type":"NRID","@value":"9000363404670"},{"@type":"NRID","@value":"9000363403471"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0005613"}],"foaf:name":[{"@language":"en","@value":"UCHIYAMA Akihiro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801208135936","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40278106"},{"@type":"NRID","@value":"1000040278106"},{"@type":"NRID","@value":"9000002316395"},{"@type":"NRID","@value":"9000387906209"},{"@type":"NRID","@value":"9000253480964"},{"@type":"NRID","@value":"9000363501944"},{"@type":"NRID","@value":"9000272990632"},{"@type":"NRID","@value":"9000257767981"},{"@type":"NRID","@value":"9000264268236"},{"@type":"NRID","@value":"9000272990612"},{"@type":"NRID","@value":"9000367417674"},{"@type":"NRID","@value":"9000253480972"},{"@type":"NRID","@value":"9000257828072"},{"@type":"NRID","@value":"9000264268261"},{"@type":"NRID","@value":"9000253480959"},{"@type":"NRID","@value":"9000272990608"},{"@type":"NRID","@value":"9000283593270"},{"@type":"NRID","@value":"9000253480638"},{"@type":"NRID","@value":"9000283593447"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/aymri"}],"foaf:name":[{"@language":"en","@value":"YAMAZAKI Akihiro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751135226368","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00414508"},{"@type":"NRID","@value":"1000000414508"},{"@type":"NRID","@value":"9000016708455"},{"@type":"NRID","@value":"9000387906211"},{"@type":"NRID","@value":"9000412058347"},{"@type":"NRID","@value":"9000345308587"},{"@type":"NRID","@value":"9000272990633"},{"@type":"NRID","@value":"9000257767982"},{"@type":"NRID","@value":"9000264268237"},{"@type":"NRID","@value":"9000406043090"},{"@type":"NRID","@value":"9000006902503"},{"@type":"NRID","@value":"9000412058316"},{"@type":"NRID","@value":"9000404513082"},{"@type":"NRID","@value":"9000398955929"},{"@type":"NRID","@value":"9000272990609"},{"@type":"NRID","@value":"9000415087770"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/reikudo"}],"foaf:name":[{"@language":"en","@value":"KUDO Rei"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261165"},{"@type":"LISSN","@value":"00261165"},{"@type":"EISSN","@value":"21869057"},{"@type":"NDL_BIB_ID","@value":"000000388871"},{"@type":"ISSN","@value":"00261165"},{"@type":"NCID","@value":"AA00702524"}],"prism:publicationName":[{"@language":"ja","@value":"気象集誌. 第2輯"},{"@value":"気象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan. Ser. II"},{"@language":"ja","@value":"気象集誌"},{"@language":"ja","@value":"氣象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan"},{"@language":"en","@value":"JMSJ"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2014","prism:volume":"92A","prism:number":"0","prism:startingPage":"195","prism:endingPage":"203"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/025797983"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I025797983"},{"@id":"https://www.jstage.jst.go.jp/article/jmsj/92A/0/92A_2014-A13/_pdf"}],"availableAt":"2014","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=column%20water%20vapor","dc:title":"column water vapor"},{"@id":"https://cir.nii.ac.jp/all?q=precipitable%20water%20vapor","dc:title":"precipitable water vapor"},{"@id":"https://cir.nii.ac.jp/all?q=sky%20radiometer","dc:title":"sky radiometer"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282814083921664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cloud optical thickness and effective particle radius derived from transmitted solar radiation measurements : Comparison with cloud radar observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142930013312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"AERONET—A Federated Instrument Network and Data Archive for Aerosol Characterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146076565632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of the atmospheric-water-vapor content in the 940-nm absorption band by use of moderate spectral-resolution measurements of direct solar irradiance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022305566005120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Optimal use of Prede POM sky radiometer for aerosol, water vapor,\nand ozone retrievals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022307172422912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nocturnal aerosol optical depth measurements  with  modified  skyradiometer POM-02 using the moon as a light source"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617598966656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An overview of and issues with sky radiometer technology and SKYNET"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617906723840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"THE HITRAN MOLECULAR SPECTROSCOPIC DATABASE AND HAWKS (HITRAN ATMOSPHERIC WORKSTATION): 1996 EDITION"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619244491136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Water Vapor Spectrum in the Region 8600–15 000 cm−1: Experimental and Theoretical Studies for a New Spectral Line Database"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621146927488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Optical Depth Measurements of Aerosol Cloud, and Water Vapor Using Sun Photometers during FIRE Cirrus IFO II"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567190140890880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The instrument constant of sky radiometers (POM-02) – Part 1: Calibration constant"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567190141943424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Retrieval of characteristic parameters for water vapour transmittance in the development of ground-based sun–sky radiometric measurements of columnar water vapour"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568694966741760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of on-site self-calibration and retrieval methods for sky-radiometer observations of precipitable water vapor"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891972608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The HITRAN 2004 molecular spectroscopic database"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094628511872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Spectroscopic Determination of Aqueous Vapor"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095825507072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Visible and near-infrared O line intensity corrections for HITRAN-96"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569240578560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water vapor: spectral transmission at wavelengths between 07 μm and 1 μm"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570628233472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of columnar water-vapor measurements from solar transmittance methods"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045416148864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A description of the correlated <i>k</i> distribution method for modeling nongray gaseous absorption, thermal emission, and multiple scattering in vertically inhomogeneous atmospheres"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518614934400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Comparison of Columnar Water Vapor Retrievals Obtained with Near-IR Solar Radiometer and Microwave Radiometer Measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518883250048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sun photometric measurements of atmospheric water vapor column abundance in the 940‐nm band"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519555085056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Columnar water vapor retrievals from multifilter rotating shadowband radiometer data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995471263232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water vapor column abundance retrievals during FIFE"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996182818816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Line-by-line computation of the atmospheric absorption spectrum using the decomposed Voigt line shape"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468640771200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New studies of the visible and near‐infrared absorption by water vapour and some problems with the HITRAN database"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468894441216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Infrared Transmission of the Atmosphere to Solar Radiation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468985408128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimating the Atmospheric Water Vapor Content from Sun Photometer Measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471206329088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-channel solar radiometer for the determination of atmospheric columnar water vapor"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944956342784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A comparison of Sun photometer derivations of total column water vapor and ozone to standard measures of same at the Southern Great Plains Atmospheric Radiation Measurement site"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945031176064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A differential technique to retrieve column water vapor using sun radiometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946217636992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimating the atmospheric water vapor content from multi-filter rotating shadow-band radiometry at São Paulo, Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419111105920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of modeled and empirical approaches for retrieving columnar water vapor from solar transmittance measurements in the 0.94‐μm region"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419232100864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of Precipitable Water from Solar Transmission"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420054408192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Water Vapor Spectrum in the Region 8600–15 000 cm−1: Experimental and Theoretical Studies for a New Spectral Line Database"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893293368960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeled and empirical approaches for retrieving columnar water vapor from solar transmittance measurements in the 0.72, 0.82, and 0.94 μm absorption bands"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893991224960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Transparency of Aqueous Vapor"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370921421440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temporal Variations in Atmospheric Water Vapor and Aerosol Optical Depth Determined by Remote Sensing"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794331010944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A robust retrieval of water vapor column in dry Arctic conditions using the rotating shadowband spectroradiometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269450584704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Optical Properties of the Atmosphere (Revised)"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270318968960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extrapolation of Earth-Based Solar Irradiance Measurements to Exoatmospheric Levels for Broad-Band and Selected Absorption-Band Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270630821888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Column water vapor from diffuse irradiance"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842060383232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid, accurate computation of narrow-band sky radiance in the 940 nm gas absorption region using the correlated k-distribution method for sun-photometer observations"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:1004113609"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I025797983"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2014-a13"},{"@type":"CIA","@value":"40020204470"},{"@type":"CIA","@value":"130004704190"},{"@type":"OPENAIRE","@value":"doi_dedup___::c8f676feabb563366a98c7912ae34866"},{"@type":"CROSSREF","@value":"10.5194/amt-13-4195-2020_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"},{"@type":"CROSSREF","@value":"10.5194/amt-11-5363-2018_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"},{"@type":"CROSSREF","@value":"10.5194/amt-12-6465-2019_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00467-6_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"},{"@type":"CROSSREF","@value":"10.5194/amt-14-3395-2021_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"},{"@type":"CROSSREF","@value":"10.5194/amt-13-2635-2020_references_DOI_FIgmchQvThGb3O2w0dgd5NJFtQX"}]}