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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Figure 4 | Geoscience Letters

Figure 4

From: Passive acoustic measurement of flow velocity in the Straits of Florida

Figure 4

Measurements of the system clocks’ drift using correlation of noise correlations. (a) Correlation between the positive- and negative-time-delay parts of the measured cross-correlation function C12. The function C12(t) is correlated with C12(−t) for the time delays 3.2 s < t < 3.6 s, which correspond to the deterministic acoustic arrivals. Line numbers indicate the quarter (first to fourth) of the available data set used in the C12 calculation. (b) Same as in (a) but for the measured cross-correlation function C23 for the 2–3 pair and 6.2 s < t < 7.0 s. (c) Least-square fits to the time shifts between 1–2 (solid line) and 2–3 (dashed line) instruments measured at different geotimes. The geotime is shown in hours following the pre-deployment clock synchronization.

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