First results from the Fennoscandian GPS networks
Temporal correlations were measured of data obtained by the Swedish Permanent GPS Network for Positioning (SWEPOS). The model for correlations, r(Delta t) = exp(-(absolute value of (Delta t))/tau), can be used to predict precision of averaged values for different values of tau. Results indicate that...
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1993
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| Online Access: | http://hdl.handle.net/2060/19940020722 |
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ftnasantrs:oai:casi.ntrs.nasa.gov:19940020722 |
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ftnasantrs:oai:casi.ntrs.nasa.gov:19940020722 2023-05-15T16:12:53+02:00 First results from the Fennoscandian GPS networks Johansson, J. M. Jaldehag, R. T. K. Unclassified, Unlimited, Publicly available Dec 1, 1993 application/pdf http://hdl.handle.net/2060/19940020722 unknown Document ID: 19940020722 Accession ID: 94N25204 http://hdl.handle.net/2060/19940020722 No Copyright CASI GEOPHYSICS Smithsonian Astrophysical Observatory, Measurement and Interpretation of Crustal Deformation Rates Associated with Postglacial Rebound; 12 p|AGU Fall Meeting; 1993; Onsala; Sweden 1993 ftnasantrs 2019-07-21T03:36:16Z Temporal correlations were measured of data obtained by the Swedish Permanent GPS Network for Positioning (SWEPOS). The model for correlations, r(Delta t) = exp(-(absolute value of (Delta t))/tau), can be used to predict precision of averaged values for different values of tau. Results indicate that tau is approximately equal to 1 day (r less than 1% after 5 days). The results show that the network can be used in geophysical applications such as the DOSE investigation on postglacial rebound. Other/Unknown Material Fennoscandian NASA Technical Reports Server (NTRS) |
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Open Polar |
| collection |
NASA Technical Reports Server (NTRS) |
| op_collection_id |
ftnasantrs |
| language |
unknown |
| topic |
GEOPHYSICS |
| spellingShingle |
GEOPHYSICS Johansson, J. M. Jaldehag, R. T. K. First results from the Fennoscandian GPS networks |
| topic_facet |
GEOPHYSICS |
| description |
Temporal correlations were measured of data obtained by the Swedish Permanent GPS Network for Positioning (SWEPOS). The model for correlations, r(Delta t) = exp(-(absolute value of (Delta t))/tau), can be used to predict precision of averaged values for different values of tau. Results indicate that tau is approximately equal to 1 day (r less than 1% after 5 days). The results show that the network can be used in geophysical applications such as the DOSE investigation on postglacial rebound. |
| format |
Other/Unknown Material |
| author |
Johansson, J. M. Jaldehag, R. T. K. |
| author_facet |
Johansson, J. M. Jaldehag, R. T. K. |
| author_sort |
Johansson, J. M. |
| title |
First results from the Fennoscandian GPS networks |
| title_short |
First results from the Fennoscandian GPS networks |
| title_full |
First results from the Fennoscandian GPS networks |
| title_fullStr |
First results from the Fennoscandian GPS networks |
| title_full_unstemmed |
First results from the Fennoscandian GPS networks |
| title_sort |
first results from the fennoscandian gps networks |
| publishDate |
1993 |
| url |
http://hdl.handle.net/2060/19940020722 |
| op_coverage |
Unclassified, Unlimited, Publicly available |
| genre |
Fennoscandian |
| genre_facet |
Fennoscandian |
| op_source |
CASI |
| op_relation |
Document ID: 19940020722 Accession ID: 94N25204 http://hdl.handle.net/2060/19940020722 |
| op_rights |
No Copyright |
| _version_ |
1765998490122452992 |