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Titlebook: IGFS 2014; Proceedings of the 3 Shuanggen Jin,Riccardo Barzaghi Conference proceedings 2016 Springer International Publishing Switzerland 2

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Evaluation of GOCE/GRACE GGMs Over Attica and Thessaloniki, Greece, and Wo Determination for Heightvaluation of the recent GOCE/GRACE Global Geopotential Models (GGMs) and the unification of the Greek Local Vertical Datum (LVD). To this extent all available satellite-only and combined GOCE/GRACE GGMs were evaluated to conclude on the possible improvement brought by GOCE in the determination of th
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Establishment of the Gravity Database AFRGDB_V1.0 for the African Geoid,in the frequency domain by 1-D FFT technique. The available gravity data set consists of land point gravity data as well as shipborne and altimetry derived gravity anomaly data. The available gravity data set has a lot of significant gaps allover the continent. The establishment of the gravity datab
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New Geoid of Greenland: A Case Study of Terrain and Ice Effects, GOCE and Use of Local Sea Level Da the ice free parts. Terrestrial gravity coverage has for the same reasons been relatively sparse, with an older airborne survey of the interior being the only gravity field data over the interior, and terrain and ice thickness models being insufficient both in terms of resolution and accuracy. This
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,Egyptian Geoid Using Best Estimated Response of the Earth’s Crust due to Topographic Loads,been proved that both the inverse isostasy approach and the direct isostasy approach (with Kelvin function .) give practically the same response of the earth’s crust due to topographic loads. The window remove-restore technique (Abd-Elmotaal and Kühtreiber, J Geod 77(1–2):77–85, 2003) has been used
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