The Southern Oscillation Can Be Best Described as

Southwest strength matters. The difference of cotidal phase from the phase of a reference tide is the epoch.

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In Southern California and US.

. This rotation caused by the Coriolis effect is generally clockwise in the southern hemisphere and counterclockwise in the northern hemisphere. The stronger the episode ie the larger the sea surface temperature departures across the central equatorial Pacific are the more reliable. Tide tables can be used for any given locale to find the predicted times.

The reference tide is the hypothetical constituent equilibrium tide on a landless Earth. Over California and the Southwest the relationship between El Niño and above-average precipitation is weaker and it depends significantly on the strength of the El Niño.

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