A comparison of spring coastal upwelling off central Chile at the extremes of the 1996–1997 ENSO cycle

Southerly wind pulses are repeatedly observed in connection with upwelling off Point Curaumilla (33°S), around 20 km south of Valparaı́so. The remote forcing of coastal upwelling associated with intraseasonal coastal-trapped waves and the local, wind-driven upwelling forcing, are characterised there in terms of sea level, meteorological observations, surface weather charts and satellite-derived SST and chlorophyll a, from observations taken in late austral springs of 1996 (La Niña) and 1997 (El Niño). nd cold coastal SST periods lasting from 15 to 20 days are associated with intraseasonal (30–50-day periods) coastal-trapped waves which are detected in time series of adjusted sea level. These waves produce shoaling/deepening cycles in the thermocline depth and hence a modulation of the local wind-driven upwelling efficiency in bringing cold, nutrient-rich waters to the surface. mospheric forcing of the wind-driven upwelling pulses is closely related to atmospheric coastal-trapped disturbances (coastal lows) in which the active/relaxed phase of the upwelling occurs ahead of/after the sea-level pressure minimum with clear/overcast skies. Time series of the alongshore pseudo-wind-stress at two coastal locations reveal that the local atmospheric forcing is always active and largely independent of the thermal phase of both the intraseasonal and interannual (ENSO) cycles. Similar differences in satellite derived sea-surface temperatures at the extremes of both the ENSO and intraseasonal cycles of 2–3°C were observed, although upwelling within cold intraseasonal periods was restricted to a narrower coastal strip during El Niño than during La Niña.