Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ...
The determination of the strain and velocity behaviour of the ice surface near the two German Antarctic Stations on Filchner/Ronne and Ekström ice shelves was performed by the use of various geodetic measuring techniques. The relative positions and heights of control points valid for reference data...
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1985
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Online Access: | https://dx.doi.org/10.1594/pangaea.761578 https://doi.pangaea.de/10.1594/PANGAEA.761578 |
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ftdatacite:10.1594/pangaea.761578 2024-09-09T19:11:29+00:00 Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... Lindner, Klaus Ritter, Bernhard 1985 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.761578 https://doi.pangaea.de/10.1594/PANGAEA.761578 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Sample code/label DATE/TIME Height Observation Research station FSE81 Neumayer_based Polarsirkel NEUMAYER III dataset Supplementary Dataset Dataset 1985 ftdatacite https://doi.org/10.1594/pangaea.761578 2024-08-01T10:50:55Z The determination of the strain and velocity behaviour of the ice surface near the two German Antarctic Stations on Filchner/Ronne and Ekström ice shelves was performed by the use of various geodetic measuring techniques. The relative positions and heights of control points valid for reference data were deduced from terrestrial observations (horizontal and vertical angle selectro optical distances). After a second sampling of data, these values served as the basis for the deformation analyses. Doppler-Satellite-observations (Navy Navigation Satellite System) made absolute positioning (latitude, longitude, height) of special points possible. These Doppler observations, supported by azimuth measurements (gyro-theodolite and sun observations) provided the datum of control networks (translations and orientation). After the repetition of these observations, the drift rates and azimuths of the control points as wenas the rotanon rates of the surface elements could be given. From vertical angles and horizontal ... : Supplement to: Lindner, Klaus; Ritter, Bernhard (1985): Geodätische Arbeiten auf den Filchner-Ronne- und Ekström-Schelfeisen 1979 bis 1982. Polarforschung, 55(1), 1-26 ... Dataset Antarc* Antarctic Ice Shelves Schelfeis* DataCite Antarctic Klaus ENVELOPE(24.117,24.117,65.717,65.717) Neumayer |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Sample code/label DATE/TIME Height Observation Research station FSE81 Neumayer_based Polarsirkel NEUMAYER III |
spellingShingle |
Event label Sample code/label DATE/TIME Height Observation Research station FSE81 Neumayer_based Polarsirkel NEUMAYER III Lindner, Klaus Ritter, Bernhard Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
topic_facet |
Event label Sample code/label DATE/TIME Height Observation Research station FSE81 Neumayer_based Polarsirkel NEUMAYER III |
description |
The determination of the strain and velocity behaviour of the ice surface near the two German Antarctic Stations on Filchner/Ronne and Ekström ice shelves was performed by the use of various geodetic measuring techniques. The relative positions and heights of control points valid for reference data were deduced from terrestrial observations (horizontal and vertical angle selectro optical distances). After a second sampling of data, these values served as the basis for the deformation analyses. Doppler-Satellite-observations (Navy Navigation Satellite System) made absolute positioning (latitude, longitude, height) of special points possible. These Doppler observations, supported by azimuth measurements (gyro-theodolite and sun observations) provided the datum of control networks (translations and orientation). After the repetition of these observations, the drift rates and azimuths of the control points as wenas the rotanon rates of the surface elements could be given. From vertical angles and horizontal ... : Supplement to: Lindner, Klaus; Ritter, Bernhard (1985): Geodätische Arbeiten auf den Filchner-Ronne- und Ekström-Schelfeisen 1979 bis 1982. Polarforschung, 55(1), 1-26 ... |
format |
Dataset |
author |
Lindner, Klaus Ritter, Bernhard |
author_facet |
Lindner, Klaus Ritter, Bernhard |
author_sort |
Lindner, Klaus |
title |
Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
title_short |
Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
title_full |
Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
title_fullStr |
Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
title_full_unstemmed |
Tab. 6+7: Altitudes and variations of altitudes in the area of the Filchner and Neumayer Stations ... |
title_sort |
tab. 6+7: altitudes and variations of altitudes in the area of the filchner and neumayer stations ... |
publisher |
PANGAEA |
publishDate |
1985 |
url |
https://dx.doi.org/10.1594/pangaea.761578 https://doi.pangaea.de/10.1594/PANGAEA.761578 |
long_lat |
ENVELOPE(24.117,24.117,65.717,65.717) |
geographic |
Antarctic Klaus Neumayer |
geographic_facet |
Antarctic Klaus Neumayer |
genre |
Antarc* Antarctic Ice Shelves Schelfeis* |
genre_facet |
Antarc* Antarctic Ice Shelves Schelfeis* |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.761578 |
_version_ |
1809751261064462336 |