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dc.contributor.authorPrieto, Juan Franciscoes_ES
dc.contributor.authorFernández Torres, Josées_ES
dc.contributor.authorPalano, Mimmoes_ES
dc.contributor.authorAbajo, Tamaraes_ES
dc.contributor.authorPérez, Enriquees_ES
dc.contributor.authorEscayo, Joaquines_ES
dc.contributor.authorVelasco, Jesuses_ES
dc.contributor.authorHerrero, Tomases_ES
dc.contributor.authorCamacho, Antonio G.es_ES
dc.contributor.authorBru, Guadalupees_ES
dc.contributor.authorMolina, Iñigoes_ES
dc.contributor.authorLópez, J. C.es_ES
dc.contributor.authorRodríguez Velasco, Gemaes_ES
dc.contributor.authorGómez, Israeles_ES
dc.date.accessioned2019-08-19T09:03:23Z-
dc.date.available2019-08-19T09:03:23Z-
dc.date.issued2016-12-12-
dc.identifier.citationAGU Fall Meeting (2016)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/188427-
dc.descriptionTrabajo presentado en el AGU (American Geophysical Union) Fall Meeting: Advancing Earth and Space Science, celebrado en San Francisco (Estados Unidos), del 12 al 16 de diciembre de 2016es_ES
dc.description.abstractLand subsidence associated to the overexploitation of aquifers represents a common hazard impacting extensive areas worldwide. Recently, González and Fernández (20101) revealed that the Alto Guadalentín Basin, located in southern Spain, is affected by the highest subsidence rates measured in Europe (about 10 cm/yr) as a direct consequence of long-term aquifer exploitation. They used ERS and ENVISAT radar data spanning the 1992¿2007 period. They identify a delayed transient nonlinear compaction of the Alto Guadalentín aquifer due to the 1990¿1995 drought period. Bonì et al. (2015) extend the previous studies using advanced DInSAR techniques to process ALOS PALSAR (2007¿2010) and COSMO-SkyMed (2011¿2012) radar images. The combination of multi-sensor SAR images with different resolutions allows for a wider monitoring time span of 20 years (1992¿2012) over the Alto Guadalentín Basin. All regional studies of the area to date are based on satellite radar interferometry using just ascending or descending acquisitions, without any combination among them to obtain vertical and horizontal (E-W) components. It is important to obtain the 3D motion field in order to perform a correct interpretation of the observations, as well as an advanced model of the aquifer evolution, to be consider for sustainable management plans of groundwater resources and hazard assessments. With this objective, a GNSS network has been defined and two surveys have been carried out in November 2015 and July 2016. Despite the limited time interval covered by the surveys, the results allow us to obtain, for the first time, the regional 3D displacement field associated to the exploitation of the aquifer. These results, although in a preliminary form, confirm previous observations and suggest that the ad-hoc establishment of small GNSS networks represent a valuable technique for the spatio-temporal monitoring of the 3D displacement field of areas subjected to extensive groundwater extraction.es_ES
dc.language.isoenges_ES
dc.rightsclosedAccesses_ES
dc.titleGNSS 3D displacement field determination in Lorca (Murcia, Spain) subsidence areaes_ES
dc.typepóster de congresoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.type.coarhttp://purl.org/coar/resource_type/c_6670es_ES
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
item.openairetypepóster de congreso-
item.fulltextNo Fulltext-
item.languageiso639-1en-
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