Divide into equal subintervals of width , with . Linear interpolation between adjacent values of gives a trapezoid of signed area . Adding these areas produces the composite trapezoidal rule
For continuous , this tends to the integral as ; if has a bounded continuous second derivative, the error is at most .
The original PDF prints while using as the bound summation index and as the upper limit. Literally this does not specify a varying upper limit. Interpreting the intended limit as , and relabelling the summation index , gives the right Riemann sum
For , , and , the only difference from the composite trapezoidal rule is the endpoint weighting: . Hence
The given square wave agrees almost everywhere with an odd function on ; its assigned value at the single point does not affect any Fourier coefficient. Thus , while
The Fourier series is therefore
The Dirichlet convergence theorem for Fourier series applies because the periodic extension is piecewise smooth. It gives at each continuity point and the midpoint at the jumps, including ; it does not reproduce the assigned value there.
At the continuity point , and . Thus
No evaluation at a discontinuity or rearrangement of the conditionally convergent series is involved.
A Fourier sine series automatically meets the zero-temperature boundary conditions because . Equivalently, extend oddly from to and then periodically with period . Its Fourier series has only sine terms, with
The coefficient formula follows from the orthogonality identity
For piecewise smooth initial data the series equals at interior continuity points and the average of its one-sided values at interior jumps. More general square-integrable data have convergence in L2 norm convergence. A classical solution continuous at the initial corners additionally requires , in agreement with the prescribed boundary conditions.
Substitute the proposed Fourier sine series into the heat equation:
Projecting onto each sine using orthogonality gives for every mode with . The initial condition fixes , since already describes the initial amplitude. Hence
For a mode with , the value of is immaterial and the same convention is convenient. The positive thermal diffusivity damps every mode, with higher frequencies decaying faster. For square-integrable initial data the damping justifies termwise differentiation for and recovery of the initial data in L2 norm convergence as .
The left panel illustrates the Fourier series in part (b). The right panel is a self-generated example with and , showing the two normal modes decaying at rates and .

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