GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER
P(論文) Gravity change observations with a superconducting gravimeter started in March 22,1993 at Syowa Station, Antarctica. The observations have been continuing almost four years until now. In this paper, the first three years of data are investigated for the purpose of obtaining detailed tidal cons...
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Language: | English |
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National Institute of Polar Research
1997
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Online Access: | https://nipr.repo.nii.ac.jp/record/2838/files/KJ00002368111.pdf https://doi.org/10.15094/00002838 https://nipr.repo.nii.ac.jp/records/2838 |
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author | タムラ, ヨシアキ アオヤマ, ユウイチ ナワ, カズナリ TAMURA, Yoshiaki AOYAMA, Yuichi NAWA, Kazunari |
author_facet | タムラ, ヨシアキ アオヤマ, ユウイチ ナワ, カズナリ TAMURA, Yoshiaki AOYAMA, Yuichi NAWA, Kazunari |
author_sort | タムラ, ヨシアキ |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Gravity change observations with a superconducting gravimeter started in March 22,1993 at Syowa Station, Antarctica. The observations have been continuing almost four years until now. In this paper, the first three years of data are investigated for the purpose of obtaining detailed tidal constants for diurnal, semidiurnal and terdiurnal waves. The observed tidal constants show rather large δ factors of 1.2 and of 1.5 for diurnal and semidiurnal tides, respectively. Those apparent large δ factors could be explained by large ocean tide loading. After applying several corrections to the observed tidal parameters, the ocean-tide corrected tidal factors were compared with theoretical ones by an elastic, ellipsoidal, rotating Earth model. Finally, the obtained tidal factors are consistent with theoretical ones within the discrepancy of 1% for principal constituents. More detailed discussion, for example, to see the latitude dependency of tidal factors, awaits accurate calibration of the scale constant of the gravimeter. departmental bulletin paper |
genre | Antarc* Antarctica |
genre_facet | Antarc* Antarctica |
geographic | Syowa Station |
geographic_facet | Syowa Station |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002838 |
institution | Open Polar |
language | English |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002838 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 10 1 AA1072335X https://nipr.repo.nii.ac.jp/record/2838/files/KJ00002368111.pdf https://doi.org/10.15094/00002838 https://nipr.repo.nii.ac.jp/records/2838 |
publishDate | 1997 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002838 2025-04-13T14:10:29+00:00 GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER タムラ, ヨシアキ アオヤマ, ユウイチ ナワ, カズナリ TAMURA, Yoshiaki AOYAMA, Yuichi NAWA, Kazunari 1997-09 application/pdf https://nipr.repo.nii.ac.jp/record/2838/files/KJ00002368111.pdf https://doi.org/10.15094/00002838 https://nipr.repo.nii.ac.jp/records/2838 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 10 1 AA1072335X https://nipr.repo.nii.ac.jp/record/2838/files/KJ00002368111.pdf https://doi.org/10.15094/00002838 https://nipr.repo.nii.ac.jp/records/2838 earth tide gravity superconducting gravimeter ocean tide loading 1997 ftnipr https://doi.org/10.15094/00002838 2025-03-19T10:19:57Z P(論文) Gravity change observations with a superconducting gravimeter started in March 22,1993 at Syowa Station, Antarctica. The observations have been continuing almost four years until now. In this paper, the first three years of data are investigated for the purpose of obtaining detailed tidal constants for diurnal, semidiurnal and terdiurnal waves. The observed tidal constants show rather large δ factors of 1.2 and of 1.5 for diurnal and semidiurnal tides, respectively. Those apparent large δ factors could be explained by large ocean tide loading. After applying several corrections to the observed tidal parameters, the ocean-tide corrected tidal factors were compared with theoretical ones by an elastic, ellipsoidal, rotating Earth model. Finally, the obtained tidal factors are consistent with theoretical ones within the discrepancy of 1% for principal constituents. More detailed discussion, for example, to see the latitude dependency of tidal factors, awaits accurate calibration of the scale constant of the gravimeter. departmental bulletin paper Other/Unknown Material Antarc* Antarctica National Institute of Polar Research Repository, Japan Syowa Station |
spellingShingle | earth tide gravity superconducting gravimeter ocean tide loading タムラ, ヨシアキ アオヤマ, ユウイチ ナワ, カズナリ TAMURA, Yoshiaki AOYAMA, Yuichi NAWA, Kazunari GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title | GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title_full | GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title_fullStr | GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title_full_unstemmed | GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title_short | GRAVIMETRIC TIDAL FACTORS AT SYOWA STATION OBTAINED FROM THREE-YEAR OBSERVATIONS WITH A SUPERCONDUCTING GRAVIMETER |
title_sort | gravimetric tidal factors at syowa station obtained from three-year observations with a superconducting gravimeter |
topic | earth tide gravity superconducting gravimeter ocean tide loading |
topic_facet | earth tide gravity superconducting gravimeter ocean tide loading |
url | https://nipr.repo.nii.ac.jp/record/2838/files/KJ00002368111.pdf https://doi.org/10.15094/00002838 https://nipr.repo.nii.ac.jp/records/2838 |