Section 1.2 | Global Geomonitoring and Gravity Field

Research Topics

Trend of global Terrestrail Water Storage within 2002 and 2021

GRACE-FO Science Data System and Mission Operation

To observe mass distribution and mass transport in System Earth, which are closely linked to climate-relevant changes on our planet, we develop, operate and analyse together with German industry and space agencies DLR, NASA or ESA specially designed gravity field satellite missions such as GRACE or GRACE-FO.

The picture shows satellites orbiting the earth.

Realization of Future Gravity Missions

In order to extend the existing time series of mass distribution and mass transport in the Earth system beyond GRACE-FO and to significantly increase the accuracy as well as the temporal and spatial resolution of the monthly gravity field models, we are currently realising the GRACE-C (Continuity) mission with DLR and NASA and have been commissioned by ESA to develop key elements of the data processing segment of a future Next Generation Gravity Mission.

The photo shows the GFZ observatory equipped with the superconducting gravimeter at Zugspitze in winter.

Terrestrial Gravimetry

Temporal variations of the gravity acceleration are induced by mass redistributions and deformations in the entire system Earth, the Earth's rotation and the masses of the Sun and Moon. We use superconducting gravimeters to observe the gravity acceleration with highest precision. This enables us to quantify a wide range of geophysical and hydrological processes.

The picture shows the laser station in night mode.

Satellite Laser Ranging

Satellite Laser Ranging (SLR) is one of the four space geodetic techniques. We operate a SLR ground station in Potsdam within the worldwide network of the International Laser Ranging Service (ILRS) and are one of the official SLR analysis centers of the ILRS.

The spatial distribution of the sea level trend is shown on a world map. Regionally, the trend is between -2 and 6 mm per year. Sea levels are rising almost everywhere.

From the ocean to the Coast

Our main focus is on the observation and analysis of sea level changes in the ocean and in coastal regions. We cover very fast processes, such as tsunamis, as well as very slow ones, such as sea level rise. We use various geodetic methods to analyse these complex phenomena, such as radar altimetry, tide gauges , buoys or GNSS measurements.

The picture shows a buoy with a GNSS antenna in the centre, which is being pulled across the lake behind a ship with a rope. The snow-covered mountains of Tian Shan can be seen in the background.

Water in Central Asia

A focus of our research in Central Asia is the monitoring and understanding of water resources and their changes. We use radar altimetry to observe the inland water cycle. Here we also use our network of climate stations and our Observatory at Lake Issyk Kul in Kyrgyzstan.

 

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