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Simulation methodology for inference on physical parameters of complex vector valued signals

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Figure

Fig. 1. Q-Q plots for standardized eastward ocean current speeds, {V ˇi1}, the empirical quantiles, againsttheoretical spherical Gaussian quantiles at depths (m): (a) 110, (b) 760, (c) 1260, (d) 1760, (e) 2510, and
Fig. 2. Estimated rotary coe�cient (solid dot), corresponding 95% theoretical confidence intervals (thinhorizontal bars), and simulated confidence intervals (thick horizontal bars) for the six observation depthsat frequencies (c/h) of approximately (a) 0.05,
Fig. 3. (a) 95% confidence intervals for outer coherence (from series 3 and 4) at four frequencies given inthe text (left to right)

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