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1 The Birth of Science - MSRI

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10.7 <strong>The</strong> Idea <strong>of</strong> Gravity from Aristotle to Hipparchus 267<br />

moon at the northern summer solstice; ignoring the high water interval,<br />

we then have a highest spring tide at point A on the Tropic <strong>of</strong> Cancer<br />

where it is noon, and at the antipodal point B on the Tropic <strong>of</strong> Capricorn,<br />

where it is midnight. <strong>The</strong> next high tide on the same spot is rather less<br />

severe, since point A has moved to A ′ and no longer has the moon and<br />

the sun on the zenith-nadir axis, but aslant (Figure 10.3, left). Thus the<br />

moon<br />

B<br />

A ′<br />

solstice<br />

A<br />

sun<br />

moon<br />

C ′<br />

A ′<br />

equinox<br />

FIGURE 10.3. Configuration <strong>of</strong> spring tides.<br />

diurnal inequality is large. On the other hand, an equinoctial spring tide<br />

(Figure 10.3, right) has diurnal inequality close to zero, as can be seen by<br />

comparing the same two points A and A ′ on the Tropic <strong>of</strong> Cancer (or, for<br />

that matter, any two points <strong>of</strong> same latitude where it is respectively noon<br />

and midnight). In this situation the highest spring tide is at points C and<br />

C ′ on the equator. On other days <strong>of</strong> the year we have an intermediate<br />

situation.<br />

<strong>The</strong> interesting thing is that in the Arabian Sea the actual behavior <strong>of</strong><br />

tides (which may in general depart far from what might be expected on<br />

the basis <strong>of</strong> simple models) agrees both with Seleucus’ description and<br />

with the theoretical scheme just discussed, as was recognized in 1898 by<br />

G. H. Darwin, one <strong>of</strong> the founders <strong>of</strong> modern tidal theory. 124<br />

Secondly, certain testimonia from Pliny imply that at least part <strong>of</strong> the<br />

preceding ideas were present in Hellenistic science. Just before talking<br />

about the moon’s attraction, Pliny states that the moon and the sun are<br />

the causes <strong>of</strong> tides, 125 and he may have Seleucus in mind when he mentions<br />

the diurnal inequality and the fact that it vanishes only during the<br />

equinox. 126 It is especially meaningful that Pliny discusses the lag with<br />

which actual tides occur 127 (the high water interval), a notion that only<br />

makes sense in connection with a theoretical explanation.<br />

124 [Darwin: Tides], p. 76.<br />

125 Pliny, Naturalis historia, II, 212.<br />

126 Pliny, Naturalis historia, II, 213.<br />

127 Pliny, Naturalis historia, II, 216.<br />

Revision: 1.11 Date: 2003/01/06 02:20:46<br />

A<br />

C<br />

sun

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