The GeoForschungsZentrum Potsdam/Groupe de Recherche de Geodesie Spatiale satellite-only and combined gravity field models:: EIGEN-GL04S1 and EIGEN-GL04C

被引:178
作者
Foerste, Christoph [1 ]
Schmidt, Roland [1 ]
Stubenvoll, Richard [1 ]
Flechtner, Frank [2 ]
Meyer, Ulrich
Koenig, Rolf [2 ]
Neumayer, Hans [2 ]
Biancale, Richard [3 ]
Lemoine, Jean-Michel [3 ]
Bruinsma, Sean [3 ]
Loyer, Sylvain [3 ,4 ]
Barthelmes, Franz [1 ]
Esselborn, Saskia [1 ]
机构
[1] Geoforschungszentrum Potsdam, Dept Geodesy & Remote Sensing 1, D-14473 Potsdam, Germany
[2] Geoforschungszentrum Potsdam, Dept Geodesy & Remote Sensing 1, D-82234 Wessling, Germany
[3] GRGS, F-31401 Toulouse, France
[4] Collecte Localisat Satellites, F-31520 Ramonville St Agne, France
关键词
earth gravity field model; global gravity field recovery; GRACE; LAGEOS; surface gravity data;
D O I
10.1007/s00190-007-0183-8
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The recent improvements in the Gravity Recovery And Climate Experiment (GRACE) tracking data processing at GeoForschungsZentrum Potsdam (GFZ) and Groupe de Recherche de Geodesie Spatiale (GRGS) Toulouse, the availability of newer surface gravity data sets in the Arctic, Antarctica and North-America, and the availability of a new mean sea surface height model from altimetry processing at GFZ gave rise to the generation of two new global gravity field models. The first, EIGEN-GL04S1, a satellite-only model complete to degree and order 150 in terms of spherical harmonics, was derived by combination of the latest GFZ Potsdam GRACE-only (EIGEN-GRACE04S) and GRGS Toulouse GRACE/LAGEO (EIGEN-GL04S) mean field solutions. The second, EIGEN-GL04S I was combined with surface gravity data from altimetry over the oceans and gravimetry over the continents to derive a new high-resolution global gravity field model called EIGEN-GL04C. This model is complete to degree and order 360 and thus resolves geoid and gravity anomalies at half-wavelengths of 55 km at the equator. A degree-dependent combination method has been applied in order to preserve the high accuracy from the GRACE satellite data in the lower frequency band of the geopotential and to form a smooth transition to the high-frequency information coming from the surface data. Compared to pre-CHAMP global high-resolution models, the accuracy was improved at a spatial resolution of 200 km (half-wavelength) by one order of magnitude to 3 cm in terms of geoid heights. The accuracy of this model (i.e. the commission error) at its full spatial resolution is estimated to be 15 cm. The model shows a reduced artificial meridional striping and an increased correlation of EIGEN-GL04C-derived geostrophic meridional currents with World Ocean Atlas 2001 (WOA01) data. These improvements have led to select EIGEN-GL04C for JASON-1 satellite altimeter data reprocessing.
引用
收藏
页码:331 / 346
页数:16
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