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GeoWerkstatt Juli: Chronometrisches Nivellement zur Erstellung eines globalen Höhensystems

GeoWerkstatt July: Chronometric Levelling to Establish a Global Height System

© ife
Left: Classified Brazilian height system. The 10 LHSs: H1, H2, H3, H4, H5, H6, H7, H8, H9, and H10 are indicated in different colours. The reference tide gauge locations for each LHS are indicated by a black circle. Right: Configuration of clock distribution with master clocks (M) and local clocks (L) in each LHS. Local clock connections are established with optical fibre links within the LHS. Master clocks of each LHS can be connected via either optical fibres (black) or free-space links (green).

How high is Mount Everest actually? Nepal and China did not agree on this question for a long time - because they each used their own reference system for measuring altitude. An agreement was reached at the end of 2020. The reason: the two countries now used an international height reference system as the basis for their measurements. The reference value is no longer a specific sea level ("above sea level"), but a so-called global equipotential surface. This refers to the Earth's gravitational field: all points on the equipotential surface have the same gravitational potential. In order to measure the height of locations on the earth, one simply determines the respective deviation from this gravitational potential. The current Geowerkstatt project shows that optical atomic clocks are particularly suitable for these measurements.

Read the Geowerkstatt project of the month here:

GeoWerkstatt project July 2025
 


Info GeoWerkstatt - Insights into research

GeoWerkstatt is published monthly here on this website. Scientists take it in turns to report on their current research projects in the field of geodesy and geoinformatics. The Geodetic Institute (GIH), the Institute of Geodesy (IfE), the Institute of Cartography and Geoinformatics (IKG) and the Institute of Photogrammetry and GeoInformation (IPI) are involved.

All GeoWerkstatt articles are available in the archive: All GeoWerkstatt articles

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