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El Nino

El Nino. El Nino – Typical surface ocean circulation

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Page 1: El Nino. El Nino – Typical surface ocean circulation

El Nino

Page 2: El Nino. El Nino – Typical surface ocean circulation

El Nino – Typical surface ocean circulation

Page 3: El Nino. El Nino – Typical surface ocean circulation

El nino conditions

• Normal

• El nino – strong counter-current

Page 4: El Nino. El Nino – Typical surface ocean circulation

El nino conditions

• Normal

• El nino – strong countercurrent

Page 5: El Nino. El Nino – Typical surface ocean circulation

• Prentice Hall Textbook animation link

El Nino: Normal Conditions

Page 6: El Nino. El Nino – Typical surface ocean circulation

• Prentice Hall Textbook animation link

El Nino: El Nino Development

Page 7: El Nino. El Nino – Typical surface ocean circulation

• Prentice Hall Textbook animation link

El Nino: La Nina

Page 8: El Nino. El Nino – Typical surface ocean circulation

Winter NH

• El Nino

• La Nina

Page 9: El Nino. El Nino – Typical surface ocean circulation

Summer NH

• El Nino

• La Nina

Page 10: El Nino. El Nino – Typical surface ocean circulation

El nino - precipitation

Page 11: El Nino. El Nino – Typical surface ocean circulation

El nino - precipitation

Page 12: El Nino. El Nino – Typical surface ocean circulation

Typical winter Effects

• El Nino

• La Nina

http://www.cpc.noaa.gov/products/analysis_monitoring/ensocycle/nawinter.html

Page 13: El Nino. El Nino – Typical surface ocean circulation

El Nino – weak Aleutian High

Page 14: El Nino. El Nino – Typical surface ocean circulation

La Nina – strong Aleutian High

Page 15: El Nino. El Nino – Typical surface ocean circulation

El Nino: US Winter Temperatures

• Higher in mid continent• Lower in south

Page 16: El Nino. El Nino – Typical surface ocean circulation

El Nino: US Winter Precipitation

• Higher in south and coastal regions

Page 17: El Nino. El Nino – Typical surface ocean circulation

Flooding in San Francisco

During the winter of 1997-98, wind-driven waves and abnormally high sea levels significantly contributed to hundreds of millions of dollars in flood and storm damage in the San Francisco Bay region. Recent analyses by U.S. Geological Survey (USGS) scientists of nearly 100 years of sea-level records collected near the Golden Gate Bridge found that these abnormally high sea levels were the direct result of that year's El Niño atmospheric phenomenon.

Page 18: El Nino. El Nino – Typical surface ocean circulation

Flooding in San Francisco

• Less land sea winds with El nino conditions result in higher sea level.

http://geopubs.wr.usgs.gov/fact-sheet/fs175-99/

Page 19: El Nino. El Nino – Typical surface ocean circulation

Hurricanes• El Niño contributes to more eastern Pacific hurricanes and fewer

Atlantic hurricanes. – Average US damage = $5.9 billion

• La Niña contributes to fewer eastern Pacific hurricanes and more Atlantic hurricanes.– Average US damage = $2.0 billion

US hurricane damage

Page 20: El Nino. El Nino – Typical surface ocean circulation

US TornadosTornado activity

Depends on the location of the polar jet stream (and thus the location an movement of mid-latitude cyclones)

• El Nino: More to the south

• La Nina: more to the north

Page 21: El Nino. El Nino – Typical surface ocean circulation

AKprecip

(in)

• El Nino:

• Nov- Dec

Page 22: El Nino. El Nino – Typical surface ocean circulation

AKTemperature

• El Nino:

• Feb - Apr

Page 23: El Nino. El Nino – Typical surface ocean circulation

Prediction of El Nino• Satellites

– provide data on tropical rainfall, wind, and ocean temperature patterns, as well as changes in conditions for hurricane formation.

• Ocean buoys – help to monitor sea-surface and upper ocean

temperatures.

• Radiosondes – balloon-borne instrument platforms with radio

transmitting capabilities, help to monitor global weather and climate patterns

• Super computers – gather all of the weather data around the world and

put it into useful formats used by scientists.– Run models for future change