In case of treating the earth tidal data observed by gravimeter, it is a difficult problem how to eliminate fully the drift. As the method available, 25 hours successive moving mean have been used customarily for the long time, but since 1941, Doodson-Warburg's method was adopted as a good method. Recently, Pertzev has devised the excellent one.In this paper, the dispute is made summarily from the stand-points of both the accuracy of results and the labour of analysis pertaining to the problem of drift. And several methods are devised newly which are more accurate and excellent compared with any one hitherto adopted.
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