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dc.rights.licenseopenen_US
hal.structure.identifierInstitut de Physique du Globe de Paris [IPGP (UMR_7154)]
dc.contributor.authorPERRIER, Frédéric
dc.contributor.authorBOURGES, François
hal.structure.identifierInstitut de Physique du Globe de Paris [IPGP (UMR_7154)]
dc.contributor.authorGIRAULT, Frédéric
hal.structure.identifierInstitut de Physique du Globe de Paris [IPGP (UMR_7154)]
dc.contributor.authorMOUËL, Jean-Louis Le
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGENTY, Dominique
hal.structure.identifierGéosciences Environnement Toulouse [GET]
dc.contributor.authorLARTIGES, Bruno
hal.structure.identifierInstitut de Physique du Globe de Paris [IPGP (UMR_7154)]
dc.contributor.authorLOSNO, Rémi
hal.structure.identifierGéosciences Environnement Toulouse [GET]
dc.contributor.authorBONNET, Stéphane
dc.date.accessioned2024-02-05T12:26:02Z
dc.date.available2024-02-05T12:26:02Z
dc.date.issued2023-05
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187811
dc.description.abstractEnIn underground cavities, temperature variations of the order of 10-3 °C are permanently induced by the variations of atmospheric pressure, even at great depths, with couplings of the order of 0.2 to 20 × 10-3 °C/hPa depending on frequency. In the first part of this study, we established the atmospheric pressure to temperature transfer function (TF) as a function of frequency from 8 × 10-7 to 8 × 10-4 Hz. Here, we use this TF to calculate the expected PIT variations, which, after being subtracted from the observed time-series, provide residual temperature time-series. We calculated such temperature residuals in four natural caves in France: Esparros, Aven d'Orgnac, Pech Merle and Chauvet-Pont d'Arc Caves, the last two containing unique prehistoric wall paintings. Temperature signals, as small as a few 10-3 °C, due to human presence, are then conspicuous, with evidence of relaxation longer than several days and long-term cumulative effects. In addition, we observe temperature signals suggesting non-stationary states characterized by several processes which are not necessarily easy to separate, such as transient air currents, due to barometric winds or locally semi-confined convection cells, transient infiltration, or energy dissipation by evaporation-condensation at the rock surface. This background thermal agitation displays a scale-free amplitude spectrum, from 2 × 10-5 to 4 × 10-4 Hz, of the form f-α, with α varying from 0.1 to 0.6 depending on the site. Furthermore, at the Chauvet Cave, a weak but unambiguous peak emerges during some months at a period of about 82.2 ± 0.8 minutes, suggesting a Helmholtz-type resonance. Small but significant temperature signals are therefore detected in underground cavities once the effect of atmospheric pressure variations is corrected for. These signals reveal subtle coupled processes whose knowledge is essential to evaluate preservation strategies and to establish conditions for resilience of underground systems under artificial or natural influence including climate change.
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/
dc.subject.enAtmospheric pressure
dc.subject.enCaves
dc.subject.enNatural ventilation
dc.subject.enPreservation
dc.subject.enBarometric pumping
dc.subject.enCritical Zone
dc.subject.enHelmholtz resonance
dc.subject.enEarth Science
dc.title.enTemperature variations in caves induced by atmospheric pressure variations-Part 2: Unveiling hidden thermal signals
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.geogeo.2022.100146en_US
dc.subject.halPlanète et Univers [physics]en_US
bordeaux.journalGeosystems and Geoenvironmenten_US
bordeaux.volume2en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierinsu-04155721
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccCC BY-NC-NDen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geosystems%20and%20Geoenvironment&rft.date=2023-05&rft.volume=2&rft.au=PERRIER,%20Fr%C3%A9d%C3%A9ric&BOURGES,%20Fran%C3%A7ois&GIRAULT,%20Fr%C3%A9d%C3%A9ric&MOU%C3%8BL,%20Jean-Louis%20Le&GENTY,%20Dominique&rft.genre=article


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