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. 2000 Mar 21;97(8):3814–3819. doi: 10.1073/pnas.070047197

Figure 2.

Figure 2

Extension of Fig. 1 to illustrate millennial periodicity in tide raising forces since 500 B.C. The angular velocity, γ, was computed from functions listed in Table 2. Events of a 180-year cycle, all at full moon, are labeled with times of occurrence (B.C. or A.D.). The 1,800-year cycle is evident as a progression of solar-lunar declination difference, listed at the top of the figure in degrees of arc of the moon above (or below) the ecliptic.