NATIONAL REPORT OF THE FEDERAL REPUBLIC OF ... - IAG Office
NATIONAL REPORT OF THE FEDERAL REPUBLIC OF ... - IAG Office
NATIONAL REPORT OF THE FEDERAL REPUBLIC OF ... - IAG Office
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
Information System contains 281,000 gravity points covering<br />
entire Germany and border-zone areas to neighbouring<br />
countries. 157,000 data points belong to companies from<br />
the German hydrocarbon industry. The system is open to<br />
the public via the internet.<br />
4. Projects and Results<br />
Within the framework of the “European Gravity and Geoid<br />
Project (EGGP)”, a project within Commission 2 of the<br />
International Association of Geodesy (<strong>IAG</strong>), several new<br />
European geoid and quasigeoid models were derived and<br />
a final version shall be presented at the IUGG General<br />
Assembly 2007 in Perugia. The project (also known as<br />
CP2.1) is chaired by H. DENKER, IfE, Hannover. Progress<br />
reports were given anually at scientific meetings in Porto<br />
2004 (DENKER et al. 2005, DENKER 2005b), Austin 2005<br />
(DENKER 2005d), and Istanbul 2006 (DENKER et al. 2007).<br />
Further informations related to the EGGP can be found in<br />
DENKER et al. (2003a and 2004) and DENKER (2004, 2006a,<br />
2006b). Due to the confidentiality of many data sets, only<br />
one data and computing center was set up at IfE in<br />
Hannover. The presently available results indicate an<br />
accuracy potential of the gravimetric (quasi)geoid models<br />
in the order of 3 – 5 cm at continental scales and 1 – 2 cm<br />
over shorter distances up to a few 100 km, provided that<br />
high quality and resolution input data are available. This<br />
is a very significant improvement compared to the last<br />
published (quasi)geoid model EGG97, the key elements<br />
being improved terrestrial and satellite gravity field data<br />
from the CHAMP and GRACE missions (e.g., DENKER<br />
2005b and 2005c).<br />
In connection with the EGGP, a consistent marine gravity<br />
data set was derived (DENKER and ROLAND 2005, ROLAND<br />
2005), the merging of ship and altimetric data was studied<br />
(ROLAND and DENKER 2005c), and contributions were made<br />
to the cross-validation of terrestrial and satellite gravity data<br />
(ROLAND and DENKER 2003 and 2005a). In addition, the<br />
collected terrestrial data sets were utilized for the computation<br />
of gravity gradients at satellite altitude with regard to<br />
the coming GOCE satellite mission (DENKER 2003A,<br />
MÜLLER et al. 2004b, WOLF et al. 2003, WOLF and DENKER<br />
2005, WOLF 2007). Linked to the EGGP are also the<br />
activities within the EUVN-DA project, an initiative to<br />
collect a dense network of GPS and levelling control points<br />
in Europe (KENYERES et al. 2006 and 2007).<br />
A corresponding geoid project was established for Antarctica<br />
within <strong>IAG</strong> Commission 2. The project “Antarctic<br />
Geoid (AntGP)” (CP2.4), chaired by M. SCHEINERT, TU<br />
Dresden, is aiming at the improvement of the terrestrial<br />
gravity coverage and geoid in Antarctica. Intensive activities<br />
took place in order to get access to already existing data<br />
sets as well as to link the AntGP goals to planned surveys,<br />
especially within the framework of the International Polar<br />
Year 2007/2008. A close relation was maintained to the<br />
project “Physical Geodesy” (chaired by M. SCHEINERT and<br />
A. CAPRA, Italy) within the SCAR GIANT program.<br />
Reports were given regularly to the <strong>IAG</strong> and on dedicated<br />
conferences (e.g. SCHEINERT 2005). A case study for<br />
regional geoid determination in Antarctica was presented<br />
H. Denker: Regional Gravity Field Modelling 59<br />
for the region of the Prince Charles Mountains and Lambert<br />
Glacier, East Antarctica (SCHEINERT et al. 2007).<br />
Since 2003, absolute gravity measurements were performed<br />
in Scandinavia at about 30 stations co-located with permanent<br />
GPS sites. The observations were carried out by four<br />
groups including IfE in Hannover (TIMMEN et al. 2005 and<br />
2006, PETTERSEN et al. 2005a and 2005b). The aim of the<br />
project is to study glacial isostasy effects and to provide<br />
ground truth data for the GRACE satellite gravity mission<br />
(MÜLLER et al. 2003a, 2003c, 2004c, 2005a, 2005b, 2006a,<br />
2007).<br />
Several investigations were carried out with respect to the<br />
upcoming GOCE satellite gradiometer mission (see also<br />
other sections of the present report); the activities concern<br />
the GOCE processing algorithms (KOOP and MÜLLER<br />
2004), error studies (e.g., WOLF 2007, WOLF and MÜLLER<br />
2004, WOLF 2006), calibration and validation topics<br />
(BOUMAN et al. 2005, DENKER et al. 2003c and 2003d,<br />
MÜLLER et al. 2003b and 2006b, TOTH et al. 2005, WOLF<br />
2004), temporal variations in the GOCE data (JARECKI et<br />
al. 2005), quality assessment procedures (JARECKI et al.<br />
2006), and a regional combination and validation experiment<br />
in Germany with heterogeneous data (LUX et al. 2006,<br />
VOIGT et al. 2006).<br />
In a joint effort, the Bundesamt für Kartographie und<br />
Geodäsie (BKG), Frankfurt am Main, and IfE, Hannover,<br />
developed a new model for the height reference surface<br />
(quasigeoid) in Germany, which now serves as a standard<br />
for the conversion between GPS ellipsoidal heights and<br />
normal heights. BKG and IfE did independent computations<br />
based on two different methods, both relying on the<br />
remove-restore technique. The input data were point gravity<br />
observations with a spacing of a few km, a digital terrain<br />
model with a block size of 50 m, a global geopotential<br />
model as well as GPS and levelling control points. Due to<br />
insignificant differences between the two independent<br />
solutions, both results were simply averaged, yielding the<br />
final GCG05 model. The evaluation of this model with<br />
independent GPS and levelling points suggests an accuracy<br />
of about 1 to 2 cm. For details see DENKER et al. (2003B),<br />
IHDE et al. (2006a and 2006b), LIEBSCH et al. (2006),<br />
SCHIRMER ET AL. (2006), and IHDE et al. (2007).<br />
Moreover, German scientists contributed to geoid studies<br />
in Iran (ARDALAN and GRAFAREND 2004) and Turkey<br />
(ÜSTÜN et al. 2005, EROL et al. 2007a and 2007b). Finally,<br />
the previous national report on regional and local gravity<br />
field modelling activities can be found in DENKER (2003b).<br />
References<br />
ARDALAN A.A., GRAFAREND E.: High-resolution regional geoid<br />
computation without applying Stokes’s formula: a case study<br />
of the Iranian geoid. Journal of Geodesy 78, 138-156, 2004.<br />
BOUMAN J., KOOP R., HAAGMANS R., MÜLLER J., SNEEUW N.,<br />
TSCHERNING C.C., VISSER P.: Calibration and Validation<br />
of GOCE Gravity Gradients. In: F. Sanso (ed.): A Window<br />
on the Future of Geodesy – Sapporo, Japan, June 30 - July<br />
11, 2003, <strong>IAG</strong> Symp., Vol. 128, 265-270, Springer Verlag,<br />
Berlin, Heidelberg, New York, 2005.