Abstract
The O1 component of geomagnetic lunar daily variation, L(O1), in the horizontal intensity at Alibag for the period 1927-1970 is determined by the generalized method of Winch. Significant partial tides, comparable to the phase law tides, are observed. An increasing trend is indicated in the range of L(O1) with increasing sunspot number. The principal harmonics of L(O1) show a marked increase in amplitude from apogee to perigee.
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