1a. TAO/model comparisons
1b. Model exploration 1 (E Pacific mixing)
2. Model Exploration 2 (Other things)
3. Model Exploration 3 (circ E of Australia)
4. Two-delta-x wave? (This page)
5. Throughflow XBT lines
6. Writeup
-> From these plots it seems clear that the oscillation is
1) related to strong currents near topography;
2) very much stronger in v than in u;
3) does not propagate;
4) only in x;
5) extends over large vertical distances;
6) can have phase reversals with depth;
7) only weakly related to temperature variations.
Some exploration of the spatial distribution of this oscillation was done by high-pass filtering u and v (e.g. v-v[x=@spz:3]):