{"@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/1361699995471263232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/92jd01050"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F92JD01050"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/92JD01050"}}],"dc:title":[{"@value":"Water vapor column abundance retrievals during FIFE"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>A variation of the modified Langley plot algorithm is reported here and applied to the retrieval of atmospheric water column abundance from a filtered sunphotometer. In this new methodology an absorption data base (LOWTRAN 7) is used to compute a water abundance versus transmittance curve of growth, rather than the square‐root dependence previously assumed. Validation of the technique is provided from an uncertainty analysis, and plans to further validate using Fourier transform spectrometers are detailed. The new sunphotometer technique is used to report total column water vapor during the First ISLSCP Field Experiment (FIFE), and comparisons are made with abundances retrieved via FIFE radiosonde observations. The sunphotometer data can best be utilized, however, to in turn validate data from airborne or in‐orbit measurements of water vapor. With these flight sensors, horizontal and topographic variability within the scene can be viewed. An example of the airborne data set is given using an image from the airborne visible infrared imaging spectrometer (AVIRIS), as acquired on August 31, 1990.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995471263235","@type":"Researcher","foaf:name":[{"@value":"Carol J. Bruegge"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995471263234","@type":"Researcher","foaf:name":[{"@value":"James E. Conel"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995471263237","@type":"Researcher","foaf:name":[{"@value":"Robert O. Green"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995471263233","@type":"Researcher","foaf:name":[{"@value":"Jack S. Margolis"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995471263232","@type":"Researcher","foaf:name":[{"@value":"Ronald G. Holm"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995471263236","@type":"Researcher","foaf:name":[{"@value":"Geoff Toon"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Atmospheres"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1992-11-30","prism:volume":"97","prism:number":"D17","prism:startingPage":"18759","prism:endingPage":"18768"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F92JD01050"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/92JD01050"}],"createdAt":"2012-02-03","modifiedAt":"2025-03-19","relatedProduct":[{"@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/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":["isReferencedBy"],"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/1390282681481756672","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Column Water Vapor Retrievals from Sky Radiometer (POM-02) 940 nm Data"}]},{"@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":"CROSSREF","@value":"10.1029/92jd01050"},{"@type":"CROSSREF","@value":"10.5194/amt-11-5363-2018_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.5194/amt-7-1075-2014_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.5194/amt-12-6465-2019_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2014-a13_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00467-6_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.5194/amt-14-3395-2021_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.5194/amtd-6-8071-2013_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"},{"@type":"CROSSREF","@value":"10.5194/amt-13-2635-2020_references_DOI_TmQsZXXYhbfWxcXjbM1x1ULbvdk"}]}