The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic
This study investigates the characteristics of gravity and ocean tides using time series recorded with the spring gravimeter and tide gauge at Zhongshan station, CATS2008 regional ocean tide model, and Eot11a global ocean tide model. The results show that the ocean tidal amplitude of O1 wave reaches...
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ftdoajarticles:oai:doaj.org/article:970388c9d6464f4199148dbe9e09e0eb 2023-05-15T13:43:27+02:00 The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic LIU Qingchao SUN Heping WANG Zemin CHEN Xiaodong ZHANG Shengkai XU Jianqiao 2018-03-01T00:00:00Z https://doi.org/10.11947/j.AGCS.2018.20170123 https://doaj.org/article/970388c9d6464f4199148dbe9e09e0eb ZH chi Surveying and Mapping Press http://html.rhhz.net/CHXB/html/2018-3-316.htm https://doaj.org/toc/1001-1595 1001-1595 doi:10.11947/j.AGCS.2018.20170123 https://doaj.org/article/970388c9d6464f4199148dbe9e09e0eb Acta Geodaetica et Cartographica Sinica, Vol 47, Iss 3, Pp 316-323 (2018) Antarctic tidal gravity regional and global ocean tide model Mathematical geography. Cartography GA1-1776 article 2018 ftdoajarticles https://doi.org/10.11947/j.AGCS.2018.20170123 2023-01-08T01:32:09Z This study investigates the characteristics of gravity and ocean tides using time series recorded with the spring gravimeter and tide gauge at Zhongshan station, CATS2008 regional ocean tide model, and Eot11a global ocean tide model. The results show that the ocean tidal amplitude of O1 wave reaches 28 cm in the diurnal tidal bands. The sum of four tidals (Q1, O1, P1 and K1) difference between the global model and the tide gauge station is 4.2 cm, and that between the regional model and the tide gauge station is 4.4 cm. In contrast, the tidal amplitude of M2 wave reaches 20 cm in the semi-diurnal bands, and the sum of four tidals (N2, M2, S2 and K2) difference are 7.7 cm and 5.1 cm, respectively. This shows that correcting global ocean tide model using regional models is important. Subsequent to the correction of global oceanic loading using the regional model, the amplitudes of final residuals for the main gravity waves K1, M2, and S2 decreased by 9.84%, 56.14%, and 37.08%, respectively, which indicates that the regional ocean tide model can better reflect the true characteristics of ocean tides. Moreover, the validity of correcting global ocean tide model using the regional model is verified. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Zhongshan Station ENVELOPE(76.371,76.371,-69.373,-69.373) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Chinese |
topic |
Antarctic tidal gravity regional and global ocean tide model Mathematical geography. Cartography GA1-1776 |
spellingShingle |
Antarctic tidal gravity regional and global ocean tide model Mathematical geography. Cartography GA1-1776 LIU Qingchao SUN Heping WANG Zemin CHEN Xiaodong ZHANG Shengkai XU Jianqiao The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
topic_facet |
Antarctic tidal gravity regional and global ocean tide model Mathematical geography. Cartography GA1-1776 |
description |
This study investigates the characteristics of gravity and ocean tides using time series recorded with the spring gravimeter and tide gauge at Zhongshan station, CATS2008 regional ocean tide model, and Eot11a global ocean tide model. The results show that the ocean tidal amplitude of O1 wave reaches 28 cm in the diurnal tidal bands. The sum of four tidals (Q1, O1, P1 and K1) difference between the global model and the tide gauge station is 4.2 cm, and that between the regional model and the tide gauge station is 4.4 cm. In contrast, the tidal amplitude of M2 wave reaches 20 cm in the semi-diurnal bands, and the sum of four tidals (N2, M2, S2 and K2) difference are 7.7 cm and 5.1 cm, respectively. This shows that correcting global ocean tide model using regional models is important. Subsequent to the correction of global oceanic loading using the regional model, the amplitudes of final residuals for the main gravity waves K1, M2, and S2 decreased by 9.84%, 56.14%, and 37.08%, respectively, which indicates that the regional ocean tide model can better reflect the true characteristics of ocean tides. Moreover, the validity of correcting global ocean tide model using the regional model is verified. |
format |
Article in Journal/Newspaper |
author |
LIU Qingchao SUN Heping WANG Zemin CHEN Xiaodong ZHANG Shengkai XU Jianqiao |
author_facet |
LIU Qingchao SUN Heping WANG Zemin CHEN Xiaodong ZHANG Shengkai XU Jianqiao |
author_sort |
LIU Qingchao |
title |
The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
title_short |
The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
title_full |
The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
title_fullStr |
The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
title_full_unstemmed |
The Characteristics of Gravity and Regional Ocean Tides at Zhongshan Station in Antarctic |
title_sort |
characteristics of gravity and regional ocean tides at zhongshan station in antarctic |
publisher |
Surveying and Mapping Press |
publishDate |
2018 |
url |
https://doi.org/10.11947/j.AGCS.2018.20170123 https://doaj.org/article/970388c9d6464f4199148dbe9e09e0eb |
long_lat |
ENVELOPE(76.371,76.371,-69.373,-69.373) ENVELOPE(76.371,76.371,-69.373,-69.373) |
geographic |
Antarctic Zhongshan Zhongshan Station |
geographic_facet |
Antarctic Zhongshan Zhongshan Station |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Acta Geodaetica et Cartographica Sinica, Vol 47, Iss 3, Pp 316-323 (2018) |
op_relation |
http://html.rhhz.net/CHXB/html/2018-3-316.htm https://doaj.org/toc/1001-1595 1001-1595 doi:10.11947/j.AGCS.2018.20170123 https://doaj.org/article/970388c9d6464f4199148dbe9e09e0eb |
op_doi |
https://doi.org/10.11947/j.AGCS.2018.20170123 |
_version_ |
1766189175939268608 |