{"@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/1363670320704193920.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2013gl058181"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058181"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058181"}}],"dc:title":[{"@value":"Hydrogen and oxygen isotopic compositions of water vapor over the Bay of Bengal during monsoon"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p><jats:italic>δ</jats:italic>D<jats:sub>v</jats:sub> and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O<jats:sub>v</jats:sub> of ~70 water vapor samples collected at 6 and 25 m above sea level over the Bay of Bengal (BoB) during July–August 2012 are reported. This helps characterize the isotopic signature of monsoon vapor. No significant vertical variation is observed in <jats:italic>δ</jats:italic>D<jats:sub>v</jats:sub>, <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O<jats:sub>v</jats:sub>, or deuterium excess (defined as <jats:italic>δ</jats:italic>D–8<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O); <jats:italic>δ</jats:italic>D<jats:sub>v</jats:sub> and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O<jats:sub>v</jats:sub> are significantly correlated (<jats:italic>r</jats:italic> = 0.92) at each height; the deuterium excess values do not, because the variation of <jats:italic>δ</jats:italic>D<jats:sub>v</jats:sub> and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O<jats:sub>v</jats:sub> relative to their uncertainties is much larger than that of the latter. The temporal variations of <jats:italic>δ</jats:italic>D<jats:sub>v</jats:sub> and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O<jats:sub>v</jats:sub> correlate well with air temperature rather than sea surface temperature. The control of normalized humidity on deuterium excess is less prominent. While the distribution of water vapor isotopologues over the BoB is primarily determined by the ocean surface conditions, they are significantly altered by laterally advected vapor from rain en route during the monsoon.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233486076672","@type":"Researcher","foaf:name":[{"@value":"M. Midhun"}],"jpcoar:affiliationName":[{"@value":"Geosciences Division Physical Research Laboratory  Ahmedabad Gujarat India"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320704193920","@type":"Researcher","foaf:name":[{"@value":"P. R. Lekshmy"}],"jpcoar:affiliationName":[{"@value":"Geosciences Division Physical Research Laboratory  Ahmedabad Gujarat India"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320704193792","@type":"Researcher","foaf:name":[{"@value":"R. Ramesh"}],"jpcoar:affiliationName":[{"@value":"Geosciences Division Physical Research Laboratory  Ahmedabad Gujarat India"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2013-12-12","prism:volume":"40","prism:number":"23","prism:startingPage":"6324","prism:endingPage":"6328"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058181"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058181"}],"createdAt":"2013-11-13","modifiedAt":"2023-08-19","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004229806770944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Controlling factors of rainwater and water vapor isotopes at Bangalore, India: Constraints from observations in 2013 Indian monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233486076672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stable isotopes in water vapor and rainwater over Indian sector of Southern Ocean and estimation of fraction of recycled moisture"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658221239296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Effect of Monsoon Circulation on the Stable Isotopic Composition of Rainfall"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367065767168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal variation in isotopic composition and the origin of precipitation over Bangladesh"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2013gl058181"},{"@type":"CROSSREF","@value":"10.1002/2016jd025352_references_DOI_H33J1cxulmluTY99hg5G5mkKy5S"},{"@type":"CROSSREF","@value":"10.1038/s41598-018-25522-5_references_DOI_H33J1cxulmluTY99hg5G5mkKy5S"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0231-4_references_DOI_H33J1cxulmluTY99hg5G5mkKy5S"},{"@type":"CROSSREF","@value":"10.1029/2017jd027427_references_DOI_H33J1cxulmluTY99hg5G5mkKy5S"}]}