The key point of this question lies in interpreting the cross-correlation expression:
\[
x(t) = \sum_{\tau} u(\tau) v(\tau + t)
\]
This expression quantifies the similarity between the signal u(t) and a time-shifted version of v(t). A peak at a positive time lag means that the signal at station u occurs before the signal at station v, implying that seismic energy traveled from station u to station v.
Interpretation:
The ambient seismic noise source must be located such that the wavefront hits station u first and then reaches station v afterward.
Assuming a homogeneous medium:
Wave velocity is the same in all directions. So, the direction of wave propagation is aligned with the observed positive lag: from u to v.
Conclusion:
A positive lag indicates that the noise source lies in the direction from station u to station v. Referring to the figure provided (with sources labeled (i) through (iv)), source (ii) lies along the propagation direction consistent with this scenario.
Final Answer: Source (ii) is the most probable origin of the observed ambient seismic noise.