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- Nawa Kazunari
- Department of Earth and Planetary Sciences, Nagoya University
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- Suda Naoki
- Department of Earth and Planetary Sciences, Nagoya University
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- Fukao Yoshio
- Earthquake Research Institute, University of Tokyo
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- Sato Tadahiro
- National Astronomical Observatory
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- Aoyama Yuichi
- The Graduate University for Advanced Studies
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- Shibuya Kazuo
- National Institute of Polar Research
Bibliographic Information
- Other Title
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- Reply〔to Imanishi′s comment〕
- Reply to Imanishi s comment
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Abstract
Imanishi (this issue) commented that (1) the noise level at Matsushiro, Japan (MA) is much lower than at Syowa Station, Antarctica (SY), (2) oscillation signals are not observed at MA, and therefore (3) peaks below 3 mHz observed at SY are unlikely to be real signals of free oscillations. We point out that (1) he made a comparison between MA in the Japanese quiet month and SY in the Antarctic windy month, (2) the Matsushiro record does show up oscillation signals, and therefore (3) his assertion that peaks below 3 mHz observed at SY are unlikely to be real signals is not founded.
Journal
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- Earth, Planets and Space
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Earth, Planets and Space 50 (10), 887-892, 1998
Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences
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Keywords
Details 詳細情報について
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- CRID
- 1390001206512487296
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- NII Article ID
- 10003736363
- 130003955878
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- NII Book ID
- AA11211921
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- ISSN
- 18805981
- 13438832
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- NDL BIB ID
- 4614403
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed