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THE JOURNAL OF THE JAPANESE ASSOCIATION OF GROUNDWATER HYDROLOGY
Vol. 10 (1968) No. 2 p. 9-14

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http://doi.org/10.5917/jagh1959.10.9


Using the FOURIER series, we obtained the theoretical equations, (3), (4) and (5) that showed the manthly average cyclic variation of the shallow groundwater temperature near the water table for a year. The values calculated by Eqs. (3), (4) and (5) were close to the observed ones as shown in Figs.2,3 and 4.

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