Please use this identifier to cite or link to this item: http://hdl.handle.net/10662/5571
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dc.contributor.authorBrugnara, Yuri-
dc.contributor.authorAuchmann, Renate-
dc.contributor.authorBrönnimann, S.-
dc.contributor.authorAllan, Robert J.-
dc.contributor.authorAuer, Ingeborg-
dc.contributor.authorBarriendos Vallve, Mariano-
dc.contributor.authorBergström, Hans-
dc.contributor.authorBhend, Jones-
dc.contributor.authorBrázdil, Rudolf-
dc.contributor.authorCompo, Gilbert P.-
dc.contributor.authorCornes, Richard C.-
dc.contributor.authorDomínguez Castro, Fernando-
dc.contributor.authorEngelen, A. F. V. van-
dc.contributor.authorFilipiak, Janusz-
dc.contributor.authorHolopainen, Jari-
dc.contributor.authorJourdain, Sylvie-
dc.contributor.authorKunz, Martin-
dc.contributor.authorLuterbacher, Jürg-
dc.contributor.authorMaugeri, Maurizio-
dc.contributor.authorMercalli, Luca-
dc.contributor.authorMoberg, Anders-
dc.contributor.authorMock, Cary J.-
dc.contributor.authorPichard, Georges-
dc.contributor.authorŘezníčková, Ladislava-
dc.contributor.authorSchrier, Gerard van der-
dc.contributor.authorSlonosky, Victoria C.-
dc.contributor.authorUstrnul, Zbigniew-
dc.contributor.authorValente, Maria Antónia-
dc.date.accessioned2017-04-04T12:01:21Z-
dc.date.available2017-04-04T12:01:21Z-
dc.date.issued2015-
dc.identifier.issn1814-9324-
dc.identifier.urihttp://hdl.handle.net/10662/5571-
dc.description.abstractLa erupción del Monte Tambora (Indonesia) en abril de 1815 es la mayor erupción volcánica documentada en la historia. Se asocia con un enfriamiento global durante el año siguiente, que se sintió especialmente en partes de Europa y América del Norte, donde el año 1816 pasó a ser conocido como "el año sin verano". Este estudio describe un esfuerzo por recoger las observaciones meteorológicas de superficie desde principios del período instrumental, enfocando a los años que siguieron a la erupción (1815-1817). Pese a la dificultad de la recolección de datos, en particular, la presión, temperatura…, éstos han sido recuperados. Algunas de las series ya habían sido descritas, pero una gran parte de los datos, han sido recientemente digitalizados a partir de datos sincrónicos originales sobre clima a partir de diarios y revistas y periódicos, que se presentan aquí por primera vez. La colección reúne más de 50 sub-series diarias desde observatorios terrestres en Europa y América del Norte y de los buques en los trópicos. Las observaciones sobre la presión han sido corregidas a partir de la temperatura y la gravedad y sobre el nivel medio del mar. Además, se aplicó una corrección estadística adicional para tener en cuenta el error posible en barómetros de mercurio. Para evaluar la fiabilidad de los datos corregidos, la variación en las observaciones de la presión se comparan con datos de climas actuales, y solo se utilizan observaciones sinópticas para análisis de tres estudios de caso en Europa. Todas las materias observadas se pondrán a disposición de la comunidad científica internacional en la base de datos sobre presión de superficie.es_ES
dc.description.abstractThe eruption of Mount Tambora (Indonesia) in April 1815 is the largest documented volcanic eruption in history. It is associated with a large global cooling during the following year, felt particularly in parts of Europe and North America, where the year 1816 became known as the “year without a summer”. This paper describes an effort made to collect surface meteorological observations from the early instrumental period, with a focus on the years of and immediately following the eruption (1815–1817). Although the collection aimed in particular at pressure observations, correspondent temperature observations were also recovered. Some of the series had already been described in the literature, but a large part of the data, recently digitised from original weather diaries and contemporary magazines and newspapers, is presented here for the first time. The collection puts together more than 50 sub-daily series from land observatories in Europe and North America and from ships in the tropics. The pressure observations have been corrected for temperature and gravity and reduced to mean sea level. Moreover, an additional statistical correction was applied to take into account common error sources in mercury barometers. To assess the reliability of the corrected data set, the variance in the pressure observations is compared with modern climatologies, and single observations are used for synoptic analyses of three case studies in Europe. All raw observations will be made available to the scientific community in the International Surface Pressure Databank.es_ES
dc.description.sponsorshipThis work was supported by the Atmospheric Circulation Reconstructions over the Earth (ACRE) initiative (www.met-acre.org), the Swiss National Science Foundation (SNF) Sinergia project FUPSOL-II (Grant CRSII2-147659) and the EU Horizon 2020 EUSTACE project (Grant Agreement no. 640171). Renate Auchmann was supported by the SNF project TWIST (200021_146599/1), Rob Allan by the EU FP7 ERA-CLIM2 (European Reanalysis of Global Climate Observations 2) project and the Met Office Hadley Centre Climate Program (HCCP), Rudolf Brázdil by the Grant Agency of the Czech Republic for the project no. P209/11/0956, Ladislava Rˇ eznícˇková by the Ministry of Education, Youth and Sports of the Czech Republic within the National Sustainability Program I (NPU I, grant no. L01415), Janusz Filipiak by the Polish National Science Centre (grant no. 2012/07/B/ST10/04214) and Fernando Domínguez-Castro by the Prometeo Project, Secretariat of Higher Learning, Science, Technology and Innovation. Support for the Twentieth Century Reanalysis Project data set is provided by the US Department of Energy, Office of Science Innovative and Novel Computational Impact on Theory and Experiment (DOE INCITE) program, and Office of Biological and Environmental Research (BER), and by the National Oceanic and Atmospheric Administration Climate Program Office.es_ES
dc.format.extent21 p.es_ES
dc.format.mimetypeapplication/pdfen_US
dc.language.isoenges_ES
dc.publisherCopernicus Publicationses_ES
dc.rightsAtribución-NoComercial-CompartirIgual 3.0 España*
dc.rightsAtribución-NoComercial-CompartirIgual 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/es/*
dc.subjectMonte Tambora (Indonesia)es_ES
dc.subjectVolcaneses_ES
dc.subjectEnfriamiento globales_ES
dc.subjectMeteorologíaes_ES
dc.subject1815es_ES
dc.subjectEuropaes_ES
dc.subjectAmérica del Nortees_ES
dc.subjectMount Tambora (Indonesia)es_ES
dc.subjectVolcanoeses_ES
dc.subjectGlobal coolinges_ES
dc.subjectMeteorologyes_ES
dc.subjectEuropees_ES
dc.subjectNorth Americaes_ES
dc.titleA collection of sub-daily pressure and temperature observations for the early instrumental period with a focus on the “year without a summer” 1816es_ES
dc.typearticlees_ES
dc.description.versionpeerReviewedes_ES
europeana.typeTEXTen_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/607029es_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/640171/EU/EUSTACEes_ES
dc.rights.accessRightsopenAccesses_ES
dc.subject.unesco2502.05 Paleoclimatologíaes_ES
dc.subject.unesco2502.06 Climatología Físicaes_ES
europeana.dataProviderUniversidad de Extremadura. Españaes_ES
dc.identifier.bibliographicCitationBrugnara, Y.; Auchmann, R.; Brönnimann, S.; Allan, R. J.; Auer, I.; Barriendos Vallve, M. y Bergström, H. et al. (2015). A collection of sub-daily pressure and temperature observations for the early instrumental period with a focus on the “year without a summer” 1816. Climate of the past, 11, 8, 1027-1047. ESSN 1814-9332es_ES
dc.type.versionpublishedVersiones_ES
dc.contributor.affiliationUniversity of Bern. Switzerlanden_US
dc.contributor.affiliationUniversidad de Barcelona-
dc.contributor.affiliationUppsala University. Sweden-
dc.contributor.affiliationMasaryk University. Czech Republic-
dc.contributor.affiliationAcademy of Sciences of the Czech Republic-
dc.contributor.affiliationUniversity of Colorado. USA-
dc.contributor.affiliationUniversity of East Anglia. Norwich-
dc.contributor.affiliationUniversidad de Extremadura. Departamento de Física-
dc.contributor.affiliationUniversity of Gdansk. Poland-
dc.contributor.affiliationUniversity of Helsinki. Finland-
dc.contributor.affiliationUniversity of Giessen. Germany-
dc.contributor.affiliationUniversità degli Studi di Milano. Italia-
dc.contributor.affiliationStockholm University. Sweden-
dc.contributor.affiliationUniversity of South Carolina. USA-
dc.contributor.affiliationUniversité d’Aix-Marseille. France-
dc.contributor.affiliationMcGill University. Canada-
dc.contributor.affiliationJagiellonian University. Poland-
dc.contributor.affiliationUniversidade de Lisboa. Portugal-
dc.relation.publisherversionhttp://www.clim-past.net/11/1027/2015/cp-11-1027-2015.pdfes_ES
dc.identifier.doi10.5194/cp-11-1027-2015-
dc.identifier.publicationtitleClimate of the pastes_ES
dc.identifier.publicationissue8es_ES
dc.identifier.publicationfirstpage1027es_ES
dc.identifier.publicationlastpage1047es_ES
dc.identifier.publicationvolume11es_ES
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