Try , . The boundary data force and . The time derivative scales as , advection as and the source as . Balancing all three gives and . Substitution then yields
For the pointwise initial trace at any fixed , the far-profile requirement is as on any smooth branch extending that far; a compact-support continuation also meets it. Solving or selecting a shock continuation was not required. The time-dependent source is singular at , so the similarity reduction is stated on .

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