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Equation 1 · Part 2 · The Machine Before Electronics

Symbol t

h(t)=H0+∑n=1NAncos⁡(ωnt+ϕn)h(t) = H_0 + \sum_{n=1}^{N} A_n \cos(\omega_n t + \phi_n)
tt

What this part means

t is an argument of the function-like quantity on the left; its role is set by that function’s stated inputs.

Its job in the formula

t is an argument of the function-like quantity on the left; its role is set by that function’s stated inputs.

The passage around this formula

Tides are the response of a rotating, irregularly shaped ocean to the gravitational forcing of the Moon and Sun. The forcing is not one periodic term but many, because the relevant astronomical cycles — lunar day, solar day, lunar month, the inclination of the orbits, the precession of the lunar nodes — beat against one another. The insight that made mechanical prediction possible was that the local water level can be written as a constant plus a sum of sinusoids whose frequencies are fixed by astronomy and whose amplitudes and phases are fixed by the harbour: h(t)=H0+∑n=1NAncos⁡(ωnt+ϕn)h(t) = H_0 + \sum_{n=1}^{N} A_n \cos(\omega_n t + \phi_n). Here ωn\omega_n is a known astronomical angular frequency, while AnA_n and ϕn\phi_n are constituents determined by…

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Learn the underlying idea

A variable is a named place for a value. Its letter is a local label: x can mean position in one formula and a data point in another.

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Sources cited in the article section

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