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dc.contributor.authorJoodaki, Gholamreza
dc.contributor.authorNahavandchi, Hossein
dc.date.accessioned2022-05-03T11:48:59Z
dc.date.available2022-05-03T11:48:59Z
dc.date.created2013-05-29T10:24:05Z
dc.date.issued2010
dc.identifier.citationESA SP. 2010, (686), .en_US
dc.identifier.issn0379-6566
dc.identifier.urihttps://hdl.handle.net/11250/2993904
dc.description.abstractThe Gravity Recovery and Climate Experiment (GRACE) data is used to estimate the secular trend and periodic variations of ice mass variability over Greenland. To do this, we use 92 monthly GRACE level 2 Release-04 (RL04) data from the Center for Space Research at the University of Texas (UTCSR) during the period April 2002 to February 2010. The high frequency noise of data has been filtered out with three smoothing cap radius. For separation of leakage effects, the appropriate reduction model is used. Taking the average over all smoothing radius after the leakage effects correction, the annual ice-mass loss becomes -155±3 Gt/year. Note that these values are free of any GIA correction.en_US
dc.language.isoengen_US
dc.publisherESA Publication Divisionen_US
dc.titleGreenland mass balance estimation from satellite gravity measurementsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber3en_US
dc.source.journalESA SPen_US
dc.source.issue686en_US
dc.identifier.cristin1031134
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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