. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography N + 2 E Z + 0 8--1 -2 Fig. 1. Analysis of variance for EDIE-MAY PI. The left upper panel gives the ratio of residual to recorded diurnal variance for the first 29 days (record A), with prediction weights based on the A record (self-prediction) and B record (last 29 days), respectively. The remaining upper panel gives the B residuals and corresponding semidiurnal ratios. In each case the dashed lines refer to "self-predic- tions," the solid
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography N + 2 E Z + 0 8--1 -2 Fig. 1. Analysis of variance for EDIE-MAY PI. The left upper panel gives the ratio of residual to recorded diurnal variance for the first 29 days (record A), with prediction weights based on the A record (self-prediction) and B record (last 29 days), respectively. The remaining upper panel gives the B residuals and corresponding semidiurnal ratios. In each case the dashed lines refer to "self-predic- tions," the solid lines to future (B residuals from A weights) or past (A residuals from B weights) predictions, respectively. The lower panels give the corresponding amplitude ratios (solid) and phase lags (dashed) relative to Bermuda reference, as a function of frequency (1 cpd±0, 1, 2 cpm for diurnals, 2 cpd±0, 1, 2 cpm for semidiurnals), for 1, 2, ..., 5 complex weights. With increasing number of weights the self-prediction residuals (but not necessarily those for the future predictions) diminish, and the admittances become in- creasingly difference between the IGPP and AOML gauges, it seems prudent to use the REIKO, ED IE capsules for comparison between central mooring with the area to the south and the AOML1, AOML3 capsules for com- parison between central mooring with the area to the east. Station differences are consistent for different con- stituents within each species. At the central mooring the semidiurnal tides are about 8% larger and 2° earlier than at EDIE; the diurnal tides are about equal in amplitude and 3°-4° earlier than at EDIE. Comparing the AOML data, at the central mooring the semidiurnal tides are about 2% larger and 2° later than at AOML3; the diurnal tides slightly smaller and earlier at AOML3. These comparisons imply that both the 1 and 2 cpd tides progress from the northeast, arriving first at AOML3, then the central mooring, and finally at EDIE. 4. C
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