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Authordc.contributor.authorSepúlveda, Edgardo
Authordc.contributor.authorCordero, Raúl R.
Authordc.contributor.authorDamiani, Alessandro
Authordc.contributor.authorFeron, Sarah
Authordc.contributor.authorPizarro, Jaime
Authordc.contributor.authorZamorano, Félix
Authordc.contributor.authorKivi, Rigel
Authordc.contributor.authorSánchez, Ricardo
Authordc.contributor.authorYela, Margarita
Authordc.contributor.authorJumelet, Julien
Authordc.contributor.authorGodoy, Alejandro
Authordc.contributor.authorCarrasco, Jorge
Authordc.contributor.authorCrespo, Juan S.
Authordc.contributor.authorSeckmeyer, Gunther
Authordc.contributor.authorJorquera, José A.
Authordc.contributor.authorCarrera, Juan M.
Authordc.contributor.authorValdevenito, Braulio
Authordc.contributor.authorCabrera Silva, Sergio Hugo
Authordc.contributor.authorRedondas, Alberto
Authordc.contributor.authorRowe, Penny M.
Admission datedc.date.accessioned2022-01-11T20:59:04Z
Available datedc.date.available2022-01-11T20:59:04Z
Publication datedc.date.issued2021
Cita de ítemdc.identifier.citationScientific Reports (2021) 11:4288es_ES
Identifierdc.identifier.other10.1038/s41598-021-81954-6
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/183680
Abstractdc.description.abstractPredicting radiative forcing due to Antarctic stratospheric ozone recovery requires detecting changes in the ozone vertical distribution. In this endeavor, the Limb Profiler of the Ozone Mapping and Profiler Suite (OMPS-LP), aboard the Suomi NPP satellite, has played a key role providing ozone profiles over Antarctica since 2011. Here, we compare ozone profiles derived from OMPS-LP data (version 2.5 algorithm) with balloon-borne ozonesondes launched from 8 Antarctic stations over the period 2012-2020. Comparisons focus on the layer from 12.5 to 27.5 km and include ozone profiles retrieved during the Sudden Stratospheric Warming (SSW) event registered in Spring 2019. We found that, over the period December-January-February-March, the root mean square error (RMSE) tends to be larger (about 20%) in the lower stratosphere (12.5-17.5 km) and smaller (about 10%) within higher layers (17.5-27.5 km). During the ozone hole season (September-October-November), RMSE values rise up to 40% within the layer from 12.5 to 22 km. Nevertheless, relative to balloon-borne measurements, the mean bias error of OMPS-derived Antarctic ozone profiles is generally lower than 0.3 ppmv, regardless of the season.es_ES
Patrocinadordc.description.sponsorshipChilean Antarctic Institute (INACH) Preis RT_32-15 RT_70-18 Consejo Nacional de Ciencia y Tecnologia (CONACyT) Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) Preis FONDECYT 1191932 REDES180158 Corporacion Fomento de la Produccion Preis CORFO 19BP-117358 18BPE-93920 18BPCR-89100 Finnish Antarctic research program (FINNARP) Consejo Nacional de Ciencia y Tecnologia CONICYT (CONICYT-DFG-SouthTrac)es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherNature Research, Germanyes_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
Sourcedc.sourceScientific Reportses_ES
Títulodc.titleEvaluation of antarctic ozone profiles derived from omps‑lp by using balloon‑borne ozonesondeses_ES
Document typedc.typeArtículo de revistaes_ES
dc.description.versiondc.description.versionVersión publicada - versión final del editores_ES
dcterms.accessRightsdcterms.accessRightsAcceso abiertoes_ES
Catalogueruchile.catalogadorcfres_ES
Indexationuchile.indexArtículo de publícación WoSes_ES


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Attribution-NonCommercial-NoDerivs 3.0 United States
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States