sio 210: enso conclusion dec. 2, 2004 interannual variability (end of this lecture + next)...

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SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) Tropical Pacific: El Nino/Southern Oscillation Southern Ocean imprint of ENSO Tropical Atlantic: dipole mode This powerpoint was prepared for purposes of this lecture and course only. It contains graphics from copyrighted books and journals. Please do not use without acknowledgment of these sources.

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Page 1: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SIO 210: ENSO conclusionDec. 2, 2004

• Interannual variability (end of this lecture + next)– Tropical Pacific: El Nino/Southern Oscillation– Southern Ocean imprint of ENSO– Tropical Atlantic: dipole mode

This powerpoint was prepared for purposes of this lecture and course only. It contains graphics from copyrighted books and journals. Please do not use without acknowledgment of these sources.

Page 2: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO: normal and La Nina conditions

http://www.pmel.noaa.gov/tao/elnino/nino_normal.html

Page 3: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO: El Nino conditions

http://www.pmel.noaa.gov/tao/elnino/nino_normal.html

Page 4: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Map to show location of Tahiti and Darwin

TahitiDarwin

Walker cell: low pressure at Darwin, high pressure at Tahiti Southern Oscillation Index: Tahiti SLP minus Darwin SLP

Page 5: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Southern Oscilllation index (NCEP)

During El Nino:

SOI is low:

Tahiti minus Darwin is low, meaning that the pressure difference between them is reduced.

Therefore the trade winds are weaker during ENSO.

Note that Darwin and Tahiti anomalies are out of phase

El Ninos: low SOI

http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/bulletin/index.html

Page 6: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO indices: based on SST.

Most commonly used is the Nino3

or Nino3,4

http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/bulletin

Page 7: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SOI and 110°W temperature as of this week

Page 8: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SST imagery - today’s image

Page 9: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Normal conditions in the tropical Pacific

Page 10: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

El Nino conditions in the tropical pacific

Page 11: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Tropical Pacific this week

TAO Project Office PMEL/NOAA

Page 12: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Temperature - mean and anomalies along the equator

November 2002: El Nino November 2004: weak El Nino

Page 13: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Time series: SST at equator

El Nino

La Nina

Page 14: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SST and zonal wind anomalies, equator

Page 15: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SST and dynamic height anomalies, equator

Page 16: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

El Nino-La Nina surface height

(NASA altimetry)

http://topex-www.jpl.nasa.gov/science/el-nino.html

Page 17: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO sea surface height anomaly

http://www.osdpd.noaa.gov/

Page 18: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

La Nina sea surface height anomaly

http://www.osdpd.noaa.gov/

Page 19: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

This month’s surface height

(altimetry):El Nino is

not developing strongly

http://topex-www.jpl.nasa.gov/science/el-nino.html

Page 20: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Sea level pressure and anomalies NCEP October 2004

Page 21: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SST anomalies October 2004 NCEP

Page 22: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SST anomalies time series NCEP

Page 23: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO - long time series of Nino3 index

Page 24: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Very long time series of ENSO: Kim Cobb et al. Based on corals.

Page 25: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Tool: Sea surface temperature pattern associated with El Nino/Southern Oscillation

Correlation of SST record at each location with the Southern Oscillation Index

Page 26: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO (SOI) SST and SLP patterns

Page 27: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

SOI surface zonal wind and “clouds”

Page 28: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

ENSO global precipitation

effects

Page 29: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

USA impacts of El Nino and La Nina: temperature

Page 30: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

USA impacts of El Nino and La Nina: precipitation

Page 31: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

Compare with SW US monsoon: monsoon is pretty much the same pattern as

ENSO

ENSOENSO

monsoonmonsoon

Page 32: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

El Nino - where are we right now?

• An El Nino event is building, and predictions of this winter’s conditions in N. America are related to it.

Page 33: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

El NinoWe are in a weak El Nino pattern now.

NOAA Climate Prediction Center winter 2004-2005 patterns prediction:

Figure 5. Seasonal U. S. temperature (left) and precipitation (right) outlooks for December 2004-February 2005. Outlooks prepared in mid-September 2004 reflect a blend of ENSO-related impacts and long-term trends.

http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/enso_advisory/

warm dry

coolwet

Page 34: SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean

El Nino

Great websites:http://www.pmel.noaa.gov/tao/elnino/nino-home.html

http://topex-www.jpl.nasa.gov/science/el-nino.html