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El Nino and La Nina
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El Nino-Southern Oscillation (ENSO)
El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in equatorial eastern Pacific that occurs periodically around Christmastime Southern Oscillation = change in atmospheric pressure over Pacific Ocean accompanying El Niño ENSO describes a combined oceanic-atmospheric disturbance
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Normal conditions in the Pacific Ocean
Figure 7-18a
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El Nino conditions (ENSO warm phase)
Figure 7-18b
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La Nina conditions (ENSO cool phase; opposite of El Nino)
Figure 7-18c
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Anomaly maps Anomaly (a = without, nomos = law) maps show the difference from normal conditions Sea Surface Temperature (SST) anomaly maps are useful for identifying unusually warm or cool water: Positive SST anomaly values = water warmer than normal Negative SST anomaly values = water cooler than normal
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January 1998 SST anomaly map
Pg. 220 Figure 7-19a
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January 2000 SST anomaly map
Pg. 220 Figure 7-19b
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Offshore California SST anomaly map: January 1998
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Offshore California SST anomaly map: January 1999 (1 year later)
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El Nino/La Nina & weather in southern California
Typical weather during El Niño? Strong El Niños: Lots of powerful storms (good waves), lots of rain ( = more than double our normal rainfall), but not always… Moderate/Weak El Niños: can have drought conditions or lots of rain or no effect at all Typical weather during La Niña? Extremely dry conditions ( = 1/3 normal rainfall)
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El Nino recurrence interval
Typical recurrence interval for El Niños = 2-12 years Pacific has alternated between El Niño and La Niña events since 1950 Figure 7-20 Pg. 221
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Effects of severe El Nino
Pg. 222 Figure 7-21
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