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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Bibliographic Details
Main Authors: Lindner, Klaus, Ritter, Bernhard
Format: Dataset
Language:English
Published: PANGAEA 1985
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.761578
https://doi.pangaea.de/10.1594/PANGAEA.761578
id ftdatacite:10.1594/pangaea.761578
record_format openpolar
spelling 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
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