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Brief mathematical derivations of the various groups of terms in the tide-generating potential are given, and the resulting lunar magnetic tides and seasonal variations are tabulated. The inverse problem of relating lunar magnetic tides and the appropriate term in the tide-generating potential is then treated. Results for 36 different lunar magnetic tides computed from 40 years of hourly mean values recorded at the Watheroo magnetic observatory are presented.
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Winch et al. (1972) studied this question.
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