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Published equation contexts

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

Why this formula appears here

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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nn

Symbol n

n appears in the bound of this sum. The bound states where the repeated operation starts, ends, or which values it includes.

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NN

Symbol N

N appears in the bound of this sum. The bound states where the repeated operation starts, ends, or which values it includes.

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ϕn\phi_n

Symbol phi_n

constituents determined by fitting the expression to a record of observed water levels at that specific place.

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n=1n=1

Starting index or lower bound: n=1

This label says where the repeated addition, multiplication, or accumulation starts. Read its value or condition together with the article’s description of the index.

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NN

Ending index or upper bound: N

This label says where the repeated addition, multiplication, or accumulation stops. It sets the last term or end of the range.

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Published contexts (1)

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

Equation 1 · History of Computing

The Machine Before Electronics

This equation states an equality: the expressions on both sides have the same value under the article’s assumptions.

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…

Meanings in this article

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