The first twenty years (1994–2014) of ozone soundings from Rapa Nui (27°S, 109°W, 51 m a.s.l.)

dc.contributor.authorGallardo, Laura
dc.contributor.authorHenrÍquez, Adolfo
dc.contributor.authorThompson, Anne M.
dc.contributor.authorRondanelli, Roberto
dc.contributor.authorCarrasco, Jorge
dc.contributor.authorOrfanoz-Cheuquelaf, Andrea
dc.contributor.authorVelásquez, Patricio
dc.date.accessioned2024-06-20T17:32:05Z
dc.date.available2024-06-20T17:32:05Z
dc.date.issued2016-11-04
dc.description.abstractOzone (O₃) soundings have been performed on Easter Island or Rapa Nui (27 °S, 109 °W, 51 m a.s.l.) since 1994 as part of the Global Atmospheric Watch Programme of the World Meteorological Organization. In this work, we analyse 260 soundings compiled over the period 1994–2014, and make the data available for the international community. We characterise O₃ profiles over this remote area of the Pacific by means of statistical analyses that consider, on the one hand, a traditional climatology that describes the data in terms of seasonal cycles based on monthly averages and, on the other hand, a process-oriented analysis based on self-organising maps. Our analyses show the influence of both tropical and subtropical/mid-latitude air masses at Rapa Nui. The former occurs in summer and fall when convective conditions prevail, and the latter in late winter and spring when subsiding conditions are recurrent. The occurrence of stratospheric intrusions in late winter and spring in connection with deep troughs and the presence of the subtropical jet stream is also apparent in the data set. The tropospheric ozone column is in good agreement with the corresponding data derived from satellites but with a systematic overestimate of summer and fall values. There is evidence of an upward trend in ozone near the surface, which suggests the impact of local pollution. We look forward to an enhancement of the Rapa Nui observing site, given its location that offers a privileged position to observe climate change over the sparsely sampled and vast South Pacific Ocean.
dc.description.sponsorshipInitially this work was supported by grant FONDECYT1030809 and finished under FONDAP 15110009. We aregrateful for the provision of ozone profiles by the ChileanWeather Office, and the ancillary data collected fromvarious sources. CO data were obtained from WMO/WDCGG data base and collected by NOAA/ESRL.We are also grateful for 7Be provided by the ChileanCommission on Nuclear Energy. A. M. Thompson’s parti-cipation is courtesy of SHADOZ (NASA Upper AirResearch Program) and was initially sponsored through aGrant to the Pennsylvania State University: NNX09AJ23G.
dc.description.urihttps://www.tandfonline.com/doi/full/10.3402/tellusb.v68.29484
dc.format.extent17 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2g02u-qv68
dc.identifier.citationGallardo, Laura, Adolfo HenrÍquez, Anne M. Thompson, Roberto Rondanelli, Jorge Carrasco, Andrea Orfanoz-Cheuquelaf, and Patricio Velásquez. “The First Twenty Years (1994–2014) of Ozone Soundings from Rapa Nui (27°S, 109°W, 51 m a.s.l.).” Tellus B: Chemical and Physical Meteorology 68, no. 1 (December 1, 2016): 29484. https://doi.org/10.3402/tellusb.v68.29484.
dc.identifier.urihttps://doi.org/10.3402/tellusb.v68.29484
dc.identifier.urihttp://hdl.handle.net/11603/34736
dc.language.isoen_US
dc.publisherTaylor & Francis
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.subjectclimatology
dc.subjectGlobal Atmospheric Watch
dc.subjectOzone sondes
dc.subjectRapa Nui
dc.subjectself-organizing maps
dc.titleThe first twenty years (1994–2014) of ozone soundings from Rapa Nui (27°S, 109°W, 51 m a.s.l.)
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-7829-0920

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