The heat equation is linear and homogeneous in : the operator satisfies . Thus the superposition principle applies to its solutions. Spatial translations are also allowed because the coefficients are constant.
Choose in part (b) and multiply by to make the initial amplitude one. Taking the two shifts and then givesAt this reproduces both initial peaks. Each term is an instance of Gaussian initial data for the heat equation, so their sum satisfies the equation. Its extension to negative times is a real smooth solution precisely on the connected intervalAt the lower endpoint the peaks narrow without bound and their heights diverge; there is no finite classical continuation there. For positive times each peak spreads and decreases in height while preserving its integral.
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