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GOCE TRF (terrestrial reference frame) vertical anomalous gradients (Tzz) from two periods have been used to determine gravity anomalies changes in mid-west Greenland, where a large mass-loss has been detected using GRACE (Fig. 1). As additional data were used the GOCE DIR-3 model and ground gravity at the coast on solid rock, where no mass loss is expected. The methods of Least-Squares Collocation (LSC) and the Reduced Point Mass (RPM) methods have been used, however only LSC included the ground data.
Original languageEnglish
Publication date2014
Number of pages1
StatePublished - 2014
EventEuropean Geosciences Union General Assembly 2014 - Vienna, Austria

Conference

ConferenceEuropean Geosciences Union General Assembly 2014
CountryAustria
CityVienna
Period27/04/201402/05/2014
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