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dc.contributor.authorKostelecký, Jan
dc.contributor.authorBezděk, Aleš
dc.contributor.authorKlokočník, Jaroslav
dc.date.accessioned2013-11-28T11:15:26Z
dc.date.available2013-11-28T11:15:26Z
dc.date.issued2013
dc.identifier.citationActa Geodynamica et Geomaterialia. 2013, vol. 10, no. 3, p. 285-291.cs
dc.identifier.issn1214-9705
dc.identifier.urihttp://hdl.handle.net/10084/101294
dc.description.abstractSince 2002, the US-German GRACE (Gravity Recovery and Climate Experiment) mission has been providing a precise survey of the Earth's time-variable gravity field, with unprecedented temporal and spatial sampling. GRACE time-variable gravity fields provide a means of measuring the temporal and spatial variations of mass redistribution within the Earth system. The GRACE mission has started a new era in studying a series of geophysical problems ranging from deep Earth structure to tracking mass redistribution on and near the surface of the Earth. Time variability of the gravity field presented here is based on the transformation of “monthly gravity field models” to the geoid. We show the changes caused by the global water cycle and land hydrology.cs
dc.format.extent916286 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoencs
dc.publisherAkademie věd České republiky, Ústav struktury a mechaniky hornincs
dc.relation.ispartofseriesActa Geodynamica et Geomaterialiacs
dc.relation.urihttp://dx.doi.org/10.13168/AGG.2013.0028cs
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/deed.en
dc.subjectGRACE missioncs
dc.subjectseasonal variationscs
dc.subjectgeoidcs
dc.titleGlobal and regional seasonal variations of the geoid detected by gracecs
dc.typearticlecs
dc.identifier.doi10.13168/AGG.2013.0028
dc.rights.accessopenAccess
dc.type.versionpublishedVersioncs
dc.type.statusPeer-reviewedcs
dc.description.sourceWeb of Sciencecs
dc.description.volume10cs
dc.description.issue3cs
dc.description.lastpage291cs
dc.description.firstpage285cs
dc.identifier.wos000325747800002


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