Numerically modelling the ratio of cross-strait voltage to water transport for the Bering Strait
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- Pankratov Oleg V.
- Institute of Geoelectromagnetic Research, Russian Academy of Sciences
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- Avdeev Dmitry B.
- Institute of Geoelectromagnetic Research, Russian Academy of Sciences
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- Kuvshinov Alexei
- Institute of Geoelectromagnetic Research, Russian Academy of Sciences
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- Shneyer Vitaly S.
- Institute of Geoelectromagnetic Research, Russian Academy of Sciences
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- Trofimov Igor L.
- Institute of Geoelectromagnetic Research, Russian Academy of Sciences
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Abstract
We find out if the ratio of cross-strait voltage to water transport for the Bering Strait (BS) is constant. For this purpose, we have developed a technique to construct BS water velocity maps. We have built up a three-dimensional conductivity model for the BS region. Using this model, we have simulated coast-to-coast voltage for the various velocity maps constructed. We have found that the voltage/transport ratio remains constant for electromagnetic field periods exceeding 2 days. We have estimated the ratio as 239 ± 11 mV/ (km2 · m/s) assuming bottom sediment conductance to be 600 S. We conclude that measuring cross-strait voltage allows the monitoring of BS water transport.
Journal
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- Earth, Planets and Space
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Earth, Planets and Space 50 (2), 165-169, 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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Details 詳細情報について
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- CRID
- 1390282681487673472
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- NII Article ID
- 10002205953
- 130003955900
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- NII Book ID
- AA11211921
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- ISSN
- 18805981
- 13438832
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- Text Lang
- en
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- Data Source
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- JaLC
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed