Fig. 7
From: Coherent modulation of the sea-level annual cycle in the United States by Atlantic Rossby waves
Hovmöller diagram of the steric modulator and estimates from a reduced gravity model. a Time-longitude section of the steric modulator for grid points east of the Bahamas at 26.5°N in the OCCAM model. The time series of the SLAC modulator averaged along the United States Gulf and Southeast coasts (ηgom−se) is also shown to the left. b Estimates of the SLAC amplitude at the Bahamas east coast based on a 1.5-layer, reduced gravity model for solutions one (orange) and two (blue), along with the SLAC amplitude (time mean removed) from OCCAM at the Bahamas east coast (black) and that averaged over tide-gauge stations 1–7 (red)
