Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11078
DC FieldValueLanguage
dc.date.accessioned2018-03-07T12:22:07Zen
dc.date.available2018-03-07T12:22:07Zen
dc.date.issued2018en
dc.identifier.urihttp://hdl.handle.net/2122/11078en
dc.description.abstractCO2 is the second most abundant volatile species of degassing magma. CO2 fluxes carry information of incredible value, such as periods of volcanic unrest. Ground-based laser remote sensing is a powerful technique to measure CO2 fluxes in a spatially integrated manner, quickly and from a safe distance, but it needs accurate knowledge of the plume speed. The latter is often difficult to estimate, particularly for complex topographies. So, a supplementary or even alternative way of retrieving fluxes would be beneficial. Here, we assess Bayesian inversion as a potential technique for the case of the volcanic crater of Solfatara (Italy), a complex terrain hosting two major CO2 degassing fumarolic vents close to a steep slope. Direct integration of remotely sensed CO2 concentrations of these vents using plume speed derived from optical flow analysis yielded a flux of 717 121 t day􀀀1, in agreement with independent measurements. The flux from Bayesian inversion based on a simple Gaussian plume model was in excellent agreement under certain conditions. In conclusion, Bayesian inversion is a promising retrieval tool for CO2 fluxes, especially in situations where plume speed estimation methods fail, e.g., optical flow for transparent plumes. The results have implications beyond volcanology, including ground-based remote sensing of greenhouse gases and verification of satellite soundings.en
dc.language.isoEnglishen
dc.relation.ispartofRemote Sensingen
dc.relation.ispartofseries/10 (2018)en
dc.titleGround-Based Remote Sensing of Volcanic CO2 Fluxes at Solfatara (Italy)—Direct Versus Inverse Bayesian Retrievalen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber125en
dc.identifier.doi10.3390/rs10010125en
dc.description.obiettivoSpecifico4V. Processi pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.contributor.authorQueißer, Manuelen
dc.contributor.authorBurton, Mikeen
dc.contributor.authorGranieri, Domenicoen
dc.contributor.authorVarnam, Matthewen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0002-2988-428X-
crisitem.author.orcid0000-0003-2831-723X-
crisitem.author.orcid0000-0002-3794-5302-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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