Tidal gravity variations revisited at Vostok Station, Antarctica
In 1969, prior to the discovery of the subglacial Lake Vostok, an Askania Gs-11 gravimeter was operated at Vostok Station (78.466S, 106.832E; 3478 m asl) to observe tidal gravity variations. To gain a better understanding of the lake's tidal dynamics, we reanalyzed these data using a Bayesian T...
Published in: | Polar Science |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
x
2009
|
Subjects: | |
Online Access: | https://doi.org/10.1016/j.polar.2008.11.001 http://ecite.utas.edu.au/81992 |
id |
ftunivtasecite:oai:ecite.utas.edu.au:81992 |
---|---|
record_format |
openpolar |
spelling |
ftunivtasecite:oai:ecite.utas.edu.au:81992 2023-05-15T14:02:31+02:00 Tidal gravity variations revisited at Vostok Station, Antarctica Doi, K Shibuya, K Wendt, A Dietrich, R King, MA 2009 https://doi.org/10.1016/j.polar.2008.11.001 http://ecite.utas.edu.au/81992 en eng x http://dx.doi.org/10.1016/j.polar.2008.11.001 Doi, K and Shibuya, K and Wendt, A and Dietrich, R and King, MA, Tidal gravity variations revisited at Vostok Station, Antarctica, Polar Science, 3, (1) pp. 1-12. ISSN 1873-9652 (2009) [Refereed Article] http://ecite.utas.edu.au/81992 Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified Refereed Article PeerReviewed 2009 ftunivtasecite https://doi.org/10.1016/j.polar.2008.11.001 2019-12-13T21:46:56Z In 1969, prior to the discovery of the subglacial Lake Vostok, an Askania Gs-11 gravimeter was operated at Vostok Station (78.466S, 106.832E; 3478 m asl) to observe tidal gravity variations. To gain a better understanding of the lake's tidal dynamics, we reanalyzed these data using a Bayesian Tidal Analysis Program Grouping method (BAYTAP-G and -L programs). The obtained phase leads for the semidiurnal waves M2 (6.6 2.1) and S2 (10.1 4.2) are more pronounced than those of the diurnal waves, among which the largest phase lead (for K1) was 5.0 0.5. The obtained factor for M2 was 0.890 0.032, significantly less than the theoretical value of 1.16. For three global ocean tide models (NAO99b, FES2004, and TPXO6.2), the estimated load tides on waves Q1, O1, P1, K1, M2, and S2 range from 0.1-0.2 Gal (Q1 and S2) to 0.6-0.7 Gal (K1). The difference in amplitude among the three models is less than 0.14 Gal (M2), and the difference in phase is generally less than 10. In calculating the residual tide vectors using the ocean models, the TPXO6.2 model generally gave the smallest residual amplitudes. Our result for the K1 wave was anomalously large (1.36 0.25 Gal), while that for the M2 wave was sufficiently small (0.37 0.17 Gal). The associated uncertainty is half that reported in previous studies. It is interesting that the residual K1 tide is approximately 90 phase-leaded, while the M2 tide is approximately 180 phase-leaded (delayed). Importantly, a similar reanalysis of data collected at Asuka Station (71.5S, 24.1E) gave residual tides within 0.2-0.3 Gal for all major diurnal and semidiurnal waves, including the K1 wave. Therefore, the anomalous K1 residual tide observed at Vostok Station must be linked to the existence of the subglacial lake and the nature of solid-ice-water dynamics in the region. 2009 Elsevier B.V. and NIPR. Article in Journal/Newspaper Antarc* Antarctica Polar Science Polar Science eCite UTAS (University of Tasmania) Lake Vostok ENVELOPE(106.000,106.000,-77.500,-77.500) Vostok Station ENVELOPE(106.837,106.837,-78.464,-78.464) Polar Science 3 1 1 12 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified Doi, K Shibuya, K Wendt, A Dietrich, R King, MA Tidal gravity variations revisited at Vostok Station, Antarctica |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified |
description |
In 1969, prior to the discovery of the subglacial Lake Vostok, an Askania Gs-11 gravimeter was operated at Vostok Station (78.466S, 106.832E; 3478 m asl) to observe tidal gravity variations. To gain a better understanding of the lake's tidal dynamics, we reanalyzed these data using a Bayesian Tidal Analysis Program Grouping method (BAYTAP-G and -L programs). The obtained phase leads for the semidiurnal waves M2 (6.6 2.1) and S2 (10.1 4.2) are more pronounced than those of the diurnal waves, among which the largest phase lead (for K1) was 5.0 0.5. The obtained factor for M2 was 0.890 0.032, significantly less than the theoretical value of 1.16. For three global ocean tide models (NAO99b, FES2004, and TPXO6.2), the estimated load tides on waves Q1, O1, P1, K1, M2, and S2 range from 0.1-0.2 Gal (Q1 and S2) to 0.6-0.7 Gal (K1). The difference in amplitude among the three models is less than 0.14 Gal (M2), and the difference in phase is generally less than 10. In calculating the residual tide vectors using the ocean models, the TPXO6.2 model generally gave the smallest residual amplitudes. Our result for the K1 wave was anomalously large (1.36 0.25 Gal), while that for the M2 wave was sufficiently small (0.37 0.17 Gal). The associated uncertainty is half that reported in previous studies. It is interesting that the residual K1 tide is approximately 90 phase-leaded, while the M2 tide is approximately 180 phase-leaded (delayed). Importantly, a similar reanalysis of data collected at Asuka Station (71.5S, 24.1E) gave residual tides within 0.2-0.3 Gal for all major diurnal and semidiurnal waves, including the K1 wave. Therefore, the anomalous K1 residual tide observed at Vostok Station must be linked to the existence of the subglacial lake and the nature of solid-ice-water dynamics in the region. 2009 Elsevier B.V. and NIPR. |
format |
Article in Journal/Newspaper |
author |
Doi, K Shibuya, K Wendt, A Dietrich, R King, MA |
author_facet |
Doi, K Shibuya, K Wendt, A Dietrich, R King, MA |
author_sort |
Doi, K |
title |
Tidal gravity variations revisited at Vostok Station, Antarctica |
title_short |
Tidal gravity variations revisited at Vostok Station, Antarctica |
title_full |
Tidal gravity variations revisited at Vostok Station, Antarctica |
title_fullStr |
Tidal gravity variations revisited at Vostok Station, Antarctica |
title_full_unstemmed |
Tidal gravity variations revisited at Vostok Station, Antarctica |
title_sort |
tidal gravity variations revisited at vostok station, antarctica |
publisher |
x |
publishDate |
2009 |
url |
https://doi.org/10.1016/j.polar.2008.11.001 http://ecite.utas.edu.au/81992 |
long_lat |
ENVELOPE(106.000,106.000,-77.500,-77.500) ENVELOPE(106.837,106.837,-78.464,-78.464) |
geographic |
Lake Vostok Vostok Station |
geographic_facet |
Lake Vostok Vostok Station |
genre |
Antarc* Antarctica Polar Science Polar Science |
genre_facet |
Antarc* Antarctica Polar Science Polar Science |
op_relation |
http://dx.doi.org/10.1016/j.polar.2008.11.001 Doi, K and Shibuya, K and Wendt, A and Dietrich, R and King, MA, Tidal gravity variations revisited at Vostok Station, Antarctica, Polar Science, 3, (1) pp. 1-12. ISSN 1873-9652 (2009) [Refereed Article] http://ecite.utas.edu.au/81992 |
op_doi |
https://doi.org/10.1016/j.polar.2008.11.001 |
container_title |
Polar Science |
container_volume |
3 |
container_issue |
1 |
container_start_page |
1 |
op_container_end_page |
12 |
_version_ |
1766272816302260224 |