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N2O Temporal Variability from the Middle Troposphere to the Middle Stratosphere Based on Airborne and Balloon-Borne Observations during the Period 1987–2018
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dc.contributor.authorKrysztofiak, Gisèlees_ES
dc.contributor.authorCatoire, Valéryes_ES
dc.contributor.authorDudok de Wit, Thierryes_ES
dc.contributor.authorKinnison, Douglas E.es_ES
dc.contributor.authorRavishankara, A. R.es_ES
dc.contributor.authorBrocchi, Vanessaes_ES
dc.contributor.authorAtlas, Elliotes_ES
dc.contributor.authorBozem, Heikoes_ES
dc.contributor.authorCommane, Roisines_ES
dc.contributor.authorD’Amato, Francescoes_ES
dc.contributor.authorDaube, Bruce C.es_ES
dc.contributor.authorDiskin, Glenn S.es_ES
dc.contributor.authorEngel, Andreases_ES
dc.contributor.authorFriedl-Vallon, Felixes_ES
dc.contributor.authorHintsa, Eric J.es_ES
dc.contributor.authorHurst, Dale F.es_ES
dc.contributor.authorHoor, Peteres_ES
dc.contributor.authorJegou, Fabricees_ES
dc.contributor.authorJucks, Kenneth W.es_ES
dc.contributor.authorKleinböhl, Armines_ES
dc.contributor.authorKüllmann, Harryes_ES
dc.contributor.authorKort, Eric A.es_ES
dc.contributor.authorMcKain, Kathrynes_ES
dc.contributor.authorMoore, Fred L.es_ES
dc.contributor.authorObersteiner, Florianes_ES
dc.contributor.authorGonzález Ramos, Yennyes_ES
dc.contributor.authorSchuck, Tanjaes_ES
dc.contributor.authorToon, Geoffrey C.es_ES
dc.contributor.authorViciani, Silviaes_ES
dc.contributor.authorWetzel, Geraldes_ES
dc.contributor.authorWilliams, Jonathanes_ES
dc.contributor.authorWofsy, Steven C.es_ES
dc.date.accessioned2023-06-27T10:40:12Z-
dc.date.available2023-06-27T10:40:12Z-
dc.date.issued2023-
dc.identifier.citationAtmosphere. 2023, 14(3), 585es_ES
dc.identifier.issn2073-4433-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/14632-
dc.description.abstractNitrous oxide (N2O) is the fourth most important greenhouse gas in the atmosphere and is considered the most important current source gas emission for global stratospheric ozone depletion (O3 ). It has natural and anthropogenic sources, mainly as an unintended by-product of food production activities. This work examines the identification and quantification of trends in the N2O concentration from the middle troposphere to the middle stratosphere (MTMS) by in situ and remote sensing observations. The temporal variability of N2O is addressed using a comprehensive dataset of in situ and remote sensing N2O concentrations based on aircraft and balloon measurements in the MTMS from 1987 to 2018. We determine N2O trends in the MTMS, based on observations. This consistent dataset was also used to study the N2O seasonal cycle to investigate the relationship between abundances and its emission sources through zonal means. The results show a longterm increase in global N2O concentration in the MTMS with an average of 0.89 ± 0.07 ppb/yr in the troposphere and 0.96 ± 0.15 ppb/yr in the stratosphere, consistent with 0.80 ppb/yr derived from ground-based measurements and 0.799 ± 0.024 ppb/yr ACE-FTS (Atmospheric Chemistry Experiment Fourier Transform Spectrometer) satellite measurements.es_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.rightsLicencia CC: Reconocimiento CC BYes_ES
dc.subjectN2O variabilityes_ES
dc.subjectUpper tropospherees_ES
dc.subjectStratospherees_ES
dc.subjectBalloon dataes_ES
dc.subjectIn situ measurementses_ES
dc.subjectAircraft dataes_ES
dc.titleN2O Temporal Variability from the Middle Troposphere to the Middle Stratosphere Based on Airborne and Balloon-Borne Observations during the Period 1987–2018es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://doi.org/10.3390/atmos14030585es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Colecciones: Artículos científicos 2023-2026


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