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A new meteorological record for Cadiz (Spain) 1806-1852: Implications for climatic reconstructions

dc.contributor.authorGallego, David
dc.contributor.authorGarcía Herrera, Ricardo Francisco
dc.contributor.authorCalvo Fernández, Natalia
dc.contributor.authorRibera, Pedro
dc.date.accessioned2023-06-20T10:43:14Z
dc.date.available2023-06-20T10:43:14Z
dc.date.issued2007-06-23
dc.description© 2007 by the American Geophysical Union. This work was supported by UNICAJA. The authors wish to thank M. J. Puertas for abstraction of the original reports; A. Gullón for helping in the historical interpretation; M. Barriendos, P. Jones, G. Können and D. Wheeler for the fruitful discussion about the interpretation of the results; the Spanish Meteorological Institute; and C. Camacho for useful information about the characteristics of the Tavira tower. Finally, the two anonymous reviewers are thanked for their helpful comments.
dc.description.abstractA new documentary source of data for wind, atmospheric pressure and air temperature for the city of Cadiz (southern Spain) has been abstracted, analyzed and compared with present-day data. Wind records cover the period 1806-1852 with three observations per day. Instrumental pressure and temperature cover the period 1825-1852. While the historical pressure series shows average values very close to that found for the period 1971-2000, temperature shows a large asymmetric seasonal warming, with increments in the order of 2 degrees C for the winter months and almost no change for summer. Wind measurements have been transformed into their numerical equivalents and then compared with present-day values. The analysis shows that the numerical estimation of ancient wind forces observed at Cadiz, while providing a robust climatic signal, has a strong bias to larger values than their instrumental equivalents. Despite the uncertainties involved in the interpretation of early wind series, this effect could be related to the recording of "average wind gusts" rather than average winds as measured by today's anemometers. In consequence, wind climatologies based on historical data, which recently are becoming available to the scientific community, should be used carefully.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipUNICAJA
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/25611
dc.identifier.doi10.1029/2007JD008517
dc.identifier.issn0148-0227
dc.identifier.officialurlhttp://dx.doi.org/10.1029/2007JD008517
dc.identifier.relatedurlhttp://onlinelibrary.wiley.com/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/51073
dc.issue.numberD12
dc.journal.titleJournal of geophysical research-atmospheres
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.rights.accessRightsopen access
dc.subject.cdu52
dc.subject.keywordInstrumental pressure observations
dc.subject.keywordNorth-Atlantic oscillation
dc.subject.keywordWeather terms
dc.subject.keywordWind force
dc.subject.keywordSeries
dc.subject.keywordDirection
dc.subject.keywordIceland
dc.subject.keywordPeriod
dc.subject.keywordCliwoc
dc.subject.keywordIndex
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.subject.ucmFísica atmosférica
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleA new meteorological record for Cadiz (Spain) 1806-1852: Implications for climatic reconstructions
dc.typejournal article
dc.volume.number112
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