Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5523
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dc.contributor.authorallBaldi, P.; Dipartimento di Fisica - Settore Geofisica - Università di Bolognaen
dc.contributor.authorallCasula, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallCenni, N.; Dipartimento di Fisica - Settore Geofisica - Università di Bolognaen
dc.contributor.authorallLoddo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallPesci, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.date.accessioned2010-01-11T13:17:43Zen
dc.date.available2010-01-11T13:17:43Zen
dc.date.issued2009-10-04en
dc.identifier.urihttp://hdl.handle.net/2122/5523en
dc.description.abstractWe use regional and local networks of continuously-operating GPS stations (CGPS) distributed in the northern–central part of the Italian peninsula to investigate the subsidence phenomenon of the Po plain sedimentary basin and vertical movements of the surrounding areas. The observations of 146 scientific and commercial stations are analyzed and compared, adopting analytical techniques widely used to study GPS coordinate time series. The use of simple antenna supports in commercial installations, instead of a more rigorous geodetic monument, does not seem to induce significant differences in the noise characteristics and in the amplitudes of annual and semi-annual periodic signals. The vertical velocity field deduced from 129 sites with observation time spans greater than one year, located in the Central–Northern Italian Peninsula, indicates the presence of two mainly subsidence areas: the Po Plain and the Arno Plain, while the sites located in the Alps and Apennine domains show relatively low uplift. The areas of the Po Plain monitored by GPS seem to indicate that the subsidence rate is constant or, in some cases, decreasing with respect to the values obtained from the last measurements, performed up to 2006 by means of both SAR and levelling techniques. Only the central part of the eastern Po Plain close to the Apennine border (Modena city area) is characterized by a peak in subsidence consisting in a velocity of about 15 mm/yr.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Ltd.en
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.relation.ispartofseries1-2/288 (2009)en
dc.subjectSubsidenceen
dc.subjectPo Plainen
dc.subjectGPSen
dc.subjectNoise Modelen
dc.titleGPS-based monitoring of land subsidence in the Po Plain (Northern Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber204-212en
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoringen
dc.identifier.doi10.1016/j.epsl.2009.09.023en
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dc.description.obiettivoSpecifico1.9. Rete GPS nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBaldi, P.en
dc.contributor.authorCasula, G.en
dc.contributor.authorCenni, N.en
dc.contributor.authorLoddo, F.en
dc.contributor.authorPesci, A.en
dc.contributor.departmentDipartimento di Fisica - Settore Geofisica - Università di Bolognaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentDipartimento di Fisica - Settore Geofisica - Università di Bolognaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità di Bologna, Dipartimento di Fisica, Settore Geofisica.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptDipartimento di Fisica - Settore Geofisica - Univ. di bologna-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0001-7934-2019-
crisitem.author.orcid0000-0002-1153-1021-
crisitem.author.orcid0000-0003-1863-3132-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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