“…8) clearly show a region of strong equatorward and onshore currents, expected from the westward propagation of a Rossby wave and the onshore shift in the California Current. Conditions during the spring 1998 were very similar to those reported for the 1982-3 and 1991-2 El Niño events (Simpson, 1983(Simpson, , 1984a(Simpson, , 1984b(Simpson, , 1992Huyer & Smith, 1985;Rienecker & Mooers, 1986;Chavez, 1996;Ramp, McClean, Collins, Semtner, & Hays, 1997). The striking difference was a rise of the thermocline in the nearshore (Fig.…”