Secular variations of the geomagnetic total field difference (hence force GTFD) of Mizusawa-Kakioka were detected using the proton data with 0, 1 nT observation sensitivity over a period of about 11 years of sunspot cycle from Apr . 1969 to Jun. 1980 through the following external field elimination methods; (1) Kp index-sunspot numbers method (2) External field enm elimination method. From the analysis based on (1), a biennial oscillation which seems to be due to an effect of sunspot solar cycle was detected in the secular variation of GTFD after elimination of the 11 year sunspot cycle. It was found that the phase pattern of the secular trend of GTFD excepting the biennial oscillation shows the minimum phase near 1974, which is observed in the secular variation of the vertical field difference . Generally speaking, in the secular variation of GTFD, annual, biennial and irregular oscillations can be found, which seem to be related to the periodic change in the formation of magnetosphere produced between summer and winter solstices, the solar cycle effect excepting 11 year sunspot cycle and those coupling effects or tectonomagnetic effect, respectively. From the analysis based on (2) to investigate the above results, the phenomena which seem to be due to an effect of tectonomagnetism were detected in the duration period from 1976 to Jun. 1980, comparing with the strain data of Sanriku and Tateyama Crustal Observatories. It was found that the crustal motion seems to precede the secular variation of GTFD about 1.5 month. As a conclusion, it is suggested that the secular variation of GTFD of Mizusawa-Kakioka may be able to interprete mostly as the result of tectonomagnetic effect due to the compression from the Pacific plate . The origin of the change of fine structure is still uncertain, though the change in speed gradient of the macroscopic secular variation of GTFD and the frequency modulation are seen barely from near the latter half of 1974.
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