| Introduction |
| RTE'87 |
| map |
| data |
| rays |
| TOPEX/Poseidon |
| map |
| movie |
| AMODE |
| map |
| data |
| M2 table |
| resonant wave |
| diurnal energy |
| HOME |
| map |
| travel times (N) |
| travel times (S) |
| thermistors |
| mode 1 |
| mode 2 |
| amps&energy (N) |
| amps&energy(S) |
| Conclusions |
|
|
| HOME Barotropic |
| data&prediction |
| table 1 |
| table 2 |
| ellipses |
| travel times (low freq) |
The Sum of Reciprocal Travel Times - Sound Speed/Temperature
The tidal amplitude of the axial ray is much larger than that of the deep turning rays.
ca. 1991-2: [Assorted colorful comments from various people (4th floor POSS) about the result...
deleted.... Internal tides were not on many radar screens in 1991-2.]