1964
DOI: 10.1111/j.1365-246x.1964.tb03859.x
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The Effect of an Ocean on Magnetic Diurnal Variations

Abstract: Theoretical calculations have been made for the idealized case in which an ocean is approximated by an infinitely long rectangular conducting sheet. The results indicate that even in the case of magnetic variations with periods as long as 24 hr one should expect a significant and easily observable enhancement in the vicinity of the edge of an ocean. When the inducing field is a function of local time only, it is found that the amplification of the variations is greater at the eastern edge of the ocean than at … Show more

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Cited by 54 publications
(20 citation statements)
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“…On the other hand, it has sometimes been pointed out that the geomagnetic variation anomalies in Japan might be due to the effects of the sea surrounding Japan (e. g., RODEN, 1964). According to RIKITAKE (1961) and RIKITAKE and SASAI (1969), it seems unlikely, however, that the anomalies in Japan are accounted for by the effects of the sea only.…”
Section: Introductionmentioning
confidence: 96%
“…On the other hand, it has sometimes been pointed out that the geomagnetic variation anomalies in Japan might be due to the effects of the sea surrounding Japan (e. g., RODEN, 1964). According to RIKITAKE (1961) and RIKITAKE and SASAI (1969), it seems unlikely, however, that the anomalies in Japan are accounted for by the effects of the sea only.…”
Section: Introductionmentioning
confidence: 96%
“…Calculations of Ashour [1971b] as well as model experiments of Roden [1964] indicate that possibility 1 is capable of generating a su•ciently large Z/H. However, both of these tend to exaggerate the induced currents because of the abnormally high vertical component of the primary field.…”
Section: B Local Modelsmentioning
confidence: 99%
“…This is understandable considering the decrease in vertical component caused by the image currents. One of the first applications of scale models to electromagnetic induction was an attempt byRoden [1964] to account for the Japanese anomaly. He used a purely vertical primary field, no conductosphere, and a fiat earth approximation.…”
mentioning
confidence: 99%
“…RIKITAKE (1964), who, along with his co-workers has studied geomagnetic variations in Japan in considerable detail, suggested in a short note presented to the IUGG Symposium on the Upper Mantle Project at Berkeley in 1963 that the major cause of the anomalous behaviour of the vertical magnetic field component near the Japanese coast is the complicated mantle structure beneath Japan. RODEN (1964) studied the effect of the Pacific Ocean on magnetic variations in Japan by the use of an analogue model and theoretical calculations and felt that the mantle structure is not the only cause of the anomalous effects, but there is some contribution due to currents induced in the ocean By using seismic and magnetic data, LAMBERT and CANER (1965) investigated the mantle structure beneath the British Columbia coastline. Also, Dosso (1966) has used analogue models of different coastal structures and examined the behaviour of the phases and amplitudes of the surface E and H components.…”
Section: Introductionmentioning
confidence: 99%