Zusammenfassung
Der gegenwärtige Fortschritt in der Quanten- und Lasermetrologie ermöglicht neue Messverfahren für die Bestimmung des Erdschwerefeldes und für das Monitoring der globalen und regionalen Massenumverteilung im Erdsystem. Die Laserinterferometrie erlaubt das Tracking von Testmassen im Orbit mit einer Präzision von Nanometern oder besser. Auf der Grundlage der Atominterferometrie werden mobile Quanten-Schweresensoren sowie stationäre Großexperimente für extrem empfindliche Schweremessungen entwickelt. Optische Atomuhren zusammen mit der Frequenzübertragung durch phasenstabilisierte Langstrecken-Faserverbindungen erlauben die Messung der relativistischen gravitativen Frequenzrotverschiebung. Auf diese Weise kann die Bestimmung von Höhen- und Potentialdifferenzen an atomare Standards geknüpft werden.
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Flury, J. (2017). Neue Sensorik für die Schwerefeldbestimmung und relativistische Geodäsie. In: Rummel, R. (eds) Erdmessung und Satellitengeodäsie. Springer Reference Naturwissenschaften . Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-47100-5_11
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