Thanks to the modern smartphone, we always know where we are. The built-in GPS function even calculates the user's exact location in remote mountain valleys, using microwave signals from satellites that send information on their position to earth. But how do the satellites know their own position? "Everyday positioning wouldn't be possible without a highly complex reference system that requires constant updating," responds Prof. Florian Seitz, Director of the German Geodetic Research Institute of the TUM. His team has just published the DTRF2014, a brand new realization of the International Terrestrial Reference System.
Constant updating is necessary because the earth is constantly changing. For example, each year Australia moves 6.9 centimeters to the northeast, while Hawaii drifts 7.1 centimeters to the northwest. Europe and America are moving away from one another; the Scandinavian countries, once weighed down by enormous sheets of ice, are now rising. "Measuring these movements exactly requires a highly precise reference system covering several decades. Here many dynamic processes have to be taken into account, for example the irregular rotational speed of the earth," Seitz explains.
With microwaves and lasers
But if everything is changing, how is it possible to establish a generally valid reference system? Geodesists have created a worldwide network of 1712 observing stations. One of the best equipped of these stations is the Geodetic Observatory Wettzell, operated in part by the TUM.
The observatory includes three radio telescopes for Very Long Baseline Interferometry (VLBI), which receive radio waves emitted by quasars. These measurements are required to detect changes in the position of our planet in space. In addition, two Satellite Laser Ranging (SLR) systems use powerful laser beams to observe the distance to satellites that reflect the laser light. This makes it possible to detect smallest movements of the ground station. In addition to these measurements several ground stations of the Global Navigation Satellite System (GNSS) receive data from GPS, Galileo and GLONASS. The three observation techniques VLBI, SLR and GNSS form the basis for the calculations of the DTRF2014. They are supplemented by the Doppler system DORIS (Doppler Orbitography and Radiopositioning Integrated by Satellite).
"By combining these various measurements we can calculate exactly the velocity at which a given location is moving," says TUM researcher Dr. Mathis Blossfeld. Wettzell is moving to the northeast at a rate of 25.4 millimeters per year. Together with his colleagues, engineer Blossfeld has also determined the movements of the other globally distributed measurement locations, using complex algorithms developed especially for the purpose. "However, the process can't be completely automated," Seitz explains: "Corrections have to be made for sudden changes in position, for example those resulting from the earthquakes in Chile in 2010 or Japan in 2011. Otherwise this would result in incorrect inferences regarding future movements."
Through careful analysis the TUM researchers could now, for the first time ever, include minute seasonal variations in the coordinates on the order of millimeters. These variations arise when persistent high-pressure areas exert pressure on the landmasses below them, or on the other hand when low-pressure areas relieve pressure on the land.
The future of the continents
The new realization of the International Terrestrial Reference System DTRF2014, created by the geodesists at the TUM on behalf of the International Earth Rotation and Reference Systems Service, is already eagerly awaited in the expert community. The data, recently published on PANGAEA, indicates the velocity and direction which the observing stations have moved in past years. Based on this information, the location of the points in several months or years can be calculated as well.
The results are of interest to geoscientists who can use the data to precisely model the movement of the earth's crust and to make inferences about the dynamics of the earth's interior. And the geodesists need the highly precise global coordinate system in order to measure the rising sea level – exactly down to the millimeter.
"More than anything the system creates a new basis for the positioning of satellites and thus improves the precision of all satellite-guided navigation systems," summarizes Seitz.
Reference to dataset: Seitz, Manuela; Bloßfeld, Mathis; Angermann, Detlef; Schmid, Ralf; Gerstl, Michael; Seitz, Florian (2016): The new DGFI-TUM realization of the ITRS: DTRF2014 (data). Deutsches Geodätisches Forschungsinstitut, Munich, Doi:10.1594/PANGAEA.864046.
Technical University of Munich
German Geodetic Research Institute and Chair of Geodetic Geodynamics
Prof. Florian Seitz
+40 (0)89 / 23031-1106