Numerically modelling the ratio of cross-strait voltage to water transport for the Bering Strait

Details Numerically modelling the ratio of cross-strait voltage to water transport for the Bering Strait Numerically modelling the ratio of cross-strait voltage to water transport for the Bering Strait

Feb 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998ep%26s...50..165p&link_type=abstract

Earth, Planets and Space, Volume 50, p. 165-169.

Physics

Scientific paper

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 2days. 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.

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