. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography M ! 1 l> 358 3° BERMUDA 35 63cm - 0 0, ^> - A0ML1 . °, 34 45cm A0ML3 358 9° 33 60cm 5 REIKO 0 7° m 1 EDIE ^r • 2 5°, 32 07cm 1. Fig. 2. Right panels show Dietrich's (1944) cotidal lines in the North Atlantic for Ki and M2 tides, respectively. Values are in solar hours, with dashed curves designating our interpolation. The MODE area falls within the shaded square which is shown on an enlarged scale in the left panels, for com- parison
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography M ! 1 l> 358 3° BERMUDA 35 63cm - 0 0, ^> - A0ML1 . °, 34 45cm A0ML3 358 9° 33 60cm 5 REIKO 0 7° m 1 EDIE ^r • 2 5°, 32 07cm 1. Fig. 2. Right panels show Dietrich's (1944) cotidal lines in the North Atlantic for Ki and M2 tides, respectively. Values are in solar hours, with dashed curves designating our interpolation. The MODE area falls within the shaded square which is shown on an enlarged scale in the left panels, for com- parison with the results at MODE stations (•). relative to the other MODE epochs and to the Dietrich configuration. Dietrich does not show co-range lines and the M2 cotidal lines are too complex in this region to infer readily whether the M2 amplitudes are con- sistent with distance from an amphidrome. Although the Tiron el al. (1967) M2 cotidal chart has the XIIh (same as Oh) in a similar position and orienta- tion as Dietrich's, one would interpret his progression in time in the MODE area to be to the northwest, contrary to Dietrich's chart and to the values for three MODE stations. The orientation of the Tiron el al. XIIh line would call for the AOML3 epoch to be between the epochs of EDIE and the central mooring stations (REIKO and AOML1); thus, on this chart, too, the AOML3 epoch seems to be slightly low (early). The orientation and progression of the Tiron el al. co-range lines call for the largest MODE amplitude at the central mooring, as is found to be the case. A0ML3 amplitude conforms in that its value falls between those for EDIE and the central mooring. b. K\ tides All stations are roughly 2°-3° early relative to the cotidal lines, yet they are consistent in that they pro- gress toward the south-southeast with spacing matching that of the inferred cotidal lines. As expected, ampli- tudes increase with distance from the amphidrome. c. Baroclinic noise In making d
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