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Global Atmospheric OCS Trend Analysis From 22 NDACC Stations
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dc.contributor.authorHannigan, James W.es_ES
dc.contributor.authorOrtega, Ivanes_ES
dc.contributor.authorShams, Shima Bahramvashes_ES
dc.contributor.authorBlumenstock, Thomases_ES
dc.contributor.authorCampbell, John Elliotes_ES
dc.contributor.authorConway, Stephaniees_ES
dc.contributor.authorFlood, Victoriaes_ES
dc.contributor.authorGarcía Rodríguez, Omaira Elenaes_ES
dc.contributor.authorGriffith, David W. T.es_ES
dc.contributor.authorGrutter, Micheles_ES
dc.contributor.authorHase, Frankes_ES
dc.contributor.authorJeseck, Pascales_ES
dc.contributor.authorJones, Nicholases_ES
dc.contributor.authorMahieu, Emmanueles_ES
dc.contributor.authorMakarova, Mariaes_ES
dc.contributor.authorMazière, Martine dees_ES
dc.contributor.authorMorino, Isamues_ES
dc.contributor.authorMurata, Isaoes_ES
dc.contributor.authorNagahama, Tomooes_ES
dc.contributor.authorNakijima, Hideakies_ES
dc.contributor.authorNotholt, Justuses_ES
dc.contributor.authorPalm, Mathiases_ES
dc.contributor.authorPoberovskii, Anatolyes_ES
dc.contributor.authorRettinger, Markuses_ES
dc.contributor.authorRobinson, Johnes_ES
dc.contributor.authorRöhling, Amelie N.es_ES
dc.contributor.authorSchneider, Matthiases_ES
dc.contributor.authorServais, Christianes_ES
dc.contributor.authorSmale, Danes_ES
dc.contributor.authorStremme, Wolfganges_ES
dc.contributor.authorStrong, Kimberlyes_ES
dc.contributor.authorSussmann, Ralfes_ES
dc.contributor.authorTe, Yaoes_ES
dc.contributor.authorVigouroux, Corinnees_ES
dc.contributor.authorWizenberg, Tyleres_ES
dc.identifier.citationJournal of Geophysical Research: Atmospheres. 2022, 127(4), p. 1-28es_ES
dc.description.abstractCarbonyl sulfide (OCS) is a non-hygroscopic trace species in the free troposphere and a large sulfur reservoir maintained by both direct oceanic, geologic, biogenic, and anthropogenic emissions and the oxidation of other sulfur-containing source species. It is the largest source of sulfur transported to the stratosphere during volcanically quiescent periods. Data from 22 ground-based globally dispersed stations are used to derive trends in total and partial column OCS. Middle infrared spectral data are recorded by solar-viewing Fourier transform interferometers that are operated as part of the Network for the Detection of Atmospheric Composition Change between 1986 and 2020. Vertical information in the retrieved profiles provides analysis of discreet altitudinal regions. Trends are found to have well-defined inflection points.es_ES
dc.description.sponsorshipNASA | Science Mission Directorate (SMD). Grant Numbers: NNX17AE38 G S003, 80NSSC21K0891. Natural Sciences and Engineering Research Council of Canada (NSERC); the Canadian Space Agency (CSA); Environment and Climate Change Canada (ECCC); Sorbonne Université; French Research Center CNRS; French Space Agency CNES. F.R.S.-FNRS. Grant Numbers: J.0147.18, J.0126.21. CONACYT. Grant Number: 290589. PAPIIT. Grant Number: IN111521. NIWA; New Zealand’s Ministry of Business, Innovation and Employment Strategic Science Investment Fund German research foundation. Grant Number: 268020496 German Bundesministerium für Wirtschaft und Energie (BMWi). Grant Numbers: 50EE1711A, 50EE1711D. Helmholtz Society Australian Research Council. Université de La Réunion. Grant Numbers: LACy-UMR8105, UMS3365.es_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.rightsLicencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-NDes_ES
dc.subjectCarbonyl sulfidees_ES
dc.subjectRemote sensinges_ES
dc.subjectLong term trendses_ES
dc.titleGlobal Atmospheric OCS Trend Analysis From 22 NDACC Stationses_ES
Appears in Collections:Artículos científicos 2019-2022

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