07.01.2013 Views

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

SHOW MORE
SHOW LESS

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.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!