Sea level variation in seismic normal mode band observed with on-ice GPS and on-land SG at Syowa Station, Antarctica

Author:

Nawa Kazunari1,Suda Naoki2,Aoki Shigeru3,Shibuya Kazuo3,Sato Tadahiro4,Fukao Yoshio56

Affiliation:

1. Geological Survey of Japan; National Institute of Advanced Industrial Science and Technology; Tsukuba Japan

2. Graduate School of Science; Hiroshima University; Higashi-Hiroshima Japan

3. National Institute of Polar Research; Tokyo Japan

4. National Astronomical Observatory; Mizusawa Japan

5. Earthquake Research Institute; University of Tokyo; Tokyo Japan

6. Institute for Frontier Research on Earth Evolution; Japan Marine Science and Technology Center; Yokosuka Japan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference19 articles.

1. Vertical seismic noise at very low frequencies;Agnew;J. Geophys. Res.,1978

2. GPS observation of the sea level variation in Lützow-Holm Bay, Antarctica;Aoki;Geophys. Res. Lett.,2000

3. Ashtech Ashtech Precise Differential GPS Navigation and Surveying (PNAV) software user's guide Doc. 630112, Rev. A Sunnyvale, Calif. 1994

4. The effects of the atmospheric pressure changes on seismic signals or how to improve the quality of a station;Beauduin;Bull. Seismol. Soc. Am.,1996

5. Effective barometric admittance and gravity residuals;Crossley;Phys. Earth Planet. Inter.,1995

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1. Ambient seismic wave field;Proceedings of the Japan Academy, Series B;2017

2. Earth's Background Free Oscillations;Annual Review of Earth and Planetary Sciences;2013-05-30

3. Earth^|^rsquo;s Background Free Oscillations;Zisin (Journal of the Seismological Society of Japan. 2nd ser.);2009

4. Loading and Gravitational Effects of the 2004 Indian Ocean Tsunami at Syowa Station, Antarctica;Bulletin of the Seismological Society of America;2007-01-01

5. Sea level and gravity variations after the 2004 Sumatra Earthquake observed at Syowa Station, Antarctica;Dynamic Planet

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