By Erik R. Ivins, Eric Rignot, Xiaoping Wu, Thomas S. James, Gino Casassa (auth.), Prof. Dr. Dr. Christoph Reigber, Prof. Dr. Hermann Lühr, Dr. Peter Schwintzer, Dr. Jens Wickert (eds.)
In the summer season of 2000 the German geo-research satellite tv for pc CHAMP was once embarked on orbit. Its cutting edge payload association and the low preliminary orbit enable CHAMP to at the same time gather and virtually regularly examine specified facts on the subject of gravity and magnetic fields at low altitude. additionally, CHAMP additionally measures the impartial surroundings and ionosphere utilizing GPS options. 3 years after release, greater than 2 hundred CHAMP investigators and co-investigators from around the globe met on the GeoForschungsZentrum in Potsdam to provide and talk about the implications derived from the broad facts units of the venture. the most final result of this professional assembly is summarized during this quantity. The booklet deals a complete perception into the current prestige of the exploitation of CHAMP info for Earth approach learn and sensible purposes in geodesy, geophysics and meteorology.
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Extra info for Earth Observation with CHAMP: Results from Three Years in Orbit
McCarthy DD (2000) IERS conventions 2000, International Earth Rotation Service. Neumeyer J, Barthelmes F, Wolf D (1999) Estimates of environmental effects in Superconducting Gravimeter data. Marees Terrestres d'Informations, Bruxelles 131: 10,15310,159. Reigber Ch, Schwintzer P, Neumayer K-H, Barthelmes F, König R, Förste Ch, Balmino G, Biancale R, Lemoine J-M, Loyer S, Bruinsma S, Perosanz F, Fayard T (2003) The CHAMP-only Earth Gravity Field Model EIGEN-2. Adv Space Res 31(8): 1883-1888. Torge W (1989) Gravimetry.
Blaisdale Press, Waltham, Mass. Milly PCD, Shmakin AB (2002) Global modeling of land water and energy balances. Part I: The land dynamics (LaD) model. Journal of Hydrometeorology 3(3): 283-299. Reigber Ch, Schwintzer P, Neumayer K-H, Barthelmes F, König R, Förste Ch, Balmino G, Biancale R, Lemoine J-M, Loyer S, Bruinsma S, Perosanz F, Fayard T (2003a) The CHAMP-only Earth Gravity Field Model EIGEN-2. Adv Space Res 31(8): 1883-1888. Reigber Ch, Schmidt R, Flechtner F, König R, Meyer U, Neumayer K-H, Schwintzer P, Zhu SY (2003b) First GFZ GRACE gravity field model EIGEN-GRACE01S.
Then the filtered ARC-GP is subtracted from the ArcGP itself to get residuals which then are added the back to the low pass-filtered GRACE. Fig. 7. (a) GRACE GGM01S 120x120 geoid (left), and (b) a hybrid geoid combining GRACE and ARC-GP models (right, see text). 44 David McAdoo et al. Fig. 8. (a) Left: ERS-1, four-year mean sea surface (MSS), (b) Right: ERS MSS minus hybrid geoid (Fig. 7b); Note the windshield-shaped test region F extending from 150E to 230E (see text). As a preliminary demonstration of the utility of such a "Hybrid” Arctic geoid we have subtracted it from a mean sea surface (Fig.