Tab. 2+3: The results of the vertical component of tides ...

Part of the geophysical work at the German Georg von Neumayer Station is the recording of the tidal movement of the Ekström Ice Shelf. Measurements are performed with an earthtide gravity meter for the vertical component of the movement and two simple tiltmeters for the horizontal components. Gravit...

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Bibliographic Details
Main Authors: Kobarg, Wolfgang, Lippmann, Erich
Format: Dataset
Language:English
Published: PANGAEA 1986
Subjects:
Table
Wave
Frequency
Amplitude
Error
Ratio
delta
Monitoring station
Calculated
Neumayer_based
NEUMAYER III
Marine Geophysics @ AWI AWI_GeoPhy
Ekström Ice Shelf
Georg von Neumayer Station
Neumayer
Neumayer Station
Ice Shelf
Online Access:https://dx.doi.org/10.1594/pangaea.754606
https://doi.pangaea.de/10.1594/PANGAEA.754606
Description
Summary:Part of the geophysical work at the German Georg von Neumayer Station is the recording of the tidal movement of the Ekström Ice Shelf. Measurements are performed with an earthtide gravity meter for the vertical component of the movement and two simple tiltmeters for the horizontal components. Gravity measurements were done continuously during the 1984/85 winter season at the observatory of the Georg von Neumayer Station. Tilt measurements were carried out at the station and at three locations on an ice-rise at about 10 km distance from the station. Gravity measurements provide the tidal movements of the ice shelf, which amounts to about 1 m at spring tide. The most important result of the tiltmeter measurements lies in the fact that the amplitudes of tilt are substantially larger at the ice-rlse than at the observatory. Results of tide-correlated ice quake activities are also presented. ... : Time interval: 18 March 1984 00.00 UT - 9 February 1985 23.00 UT 7896 hours. ...

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