Title: The ENSO Cycle: Recent Evolution, Current Status and Predictions
1The ENSO Cycle Recent Evolution, Current Status
and Predictions
Vernon E. Kousky Climate Prediction Center / NCEP
2Outline
- Overview
- 2001-2002 Developments
- Current Conditions
- El Niño Outlook
- Typical U.S. Impacts and seasonal outlooks
- Summary
3Overview
- A Pacific basin warm (El Niño) episode is in
progress in the tropical Pacific. -
- Statistical and coupled model forecasts indicate
that the El Niño will continue through the
northern winter 2002-2003 and into the spring
2003. - All of the forecasts indicate that this El Niño
will be considerably weaker than the 1997-98 El
Niño. - Impacts on the United States are expected during
this fall and winter, but they should be
generally weaker than those experienced during
the very strong 1997-98 El Niño.
42001-2002 Developments
- A transition from La Niña to a developing
warm-episode (El Niño) began in mid-2001. An
evolution toward a basin-wide El Niño occurred
during December 2001-January 2002.
Time
Longitude
52001-2002 Developments
- Early El Niño impacts occurred along the coasts
of Ecuador and northern Peru during
February-April 2002. - During March-June 2002 the equatorial easterlies
gradually weakened, while the Southern
Oscillation Index (SOI) became persistently
negative. These features indicated a developing
El Niño.
6Time Series Nino 3.4, EQSOI, U850
LN
Positive SST departures Negative
EQSOI Weaker-than-normal equatorial easterly
winds
neutral
EN
7Subsurface Temperature Anomaly Index
T2
T1
Index of Upper Ocean Heat Content T1 T2 Index
of Anomalous Thermocline Slope T2 T1
8Heat Content Leads SST Anomalies
92001-2002 Developments
- El Niño conditions established during April-June
2002.
NOAAs Definition for El Niño Sea surface
temperatures 0.5C above average or greater,
averaged over three consecutive months, in the
Niño 3.4 region (120W-170W, 5N-5S).
10Current Conditions in the Tropical Pacific
- Ocean surface temperatures remain greater than
1C (2F) above average throughout the central
and east-central equatorial Pacific between 180W
and 105W.
SST Anomalies 15 SEP-12 OCT 2002
Precipitation Anomalies September 2002
11Current Conditions in the Tropical Pacific
Equatorial ocean subsurface temperatures remain
above normal (deeper than normal oceanic
thermocline), with anomalies (departures from
average) exceeding 2C over much of the central
and east-central Pacific during September.
12El Niño Outlook
- Statistical and coupled model forecasts indicate
that El Niño conditions will continue through the
remainder of 2002 and into northern spring 2003. - All of the forecasts indicate that this El Niño
is expected to be considerably weaker than the
1997-98 El Niño.
Courtesy Tony Barnston
13Typical Global El Niño Impacts
Region Period Impact
Indonesia Life of event Drier
Northeast Brazil March-May Drier
Central America /Mexico May-October Drier
West Coast South America March-May Wetter
Central South America June-December Wetter
Southeast Africa December-February Drier
14Typical El Niño impacts on North America
- El Niño impacts on North America are typically
strongest during the winter and early spring.
Impacts include -
- Fall
- Pacific Northwest -- drier than normal
- Winter/Early Spring
- Northern Tier of States, western and central
Canada, southern/southeastern Alaska - warmer
than normal - Northern Rockies, Ohio Valley drier than normal
- Southern Tier of States wetter than normal
- Texas eastward to the Carolinas cooler than
normal
15Seasonal OutlooksNov 2002 - Jan 2003
Temperature
Precipitation
Outlooks combine typical El Niño impacts and
long-term trends.
16Seasonal OutlooksFeb - Apr 2003
Temperature
Precipitation
Outlooks combine typical El Niño impacts and
long-term trends.
17Summary
- El Niño conditions are evident in the tropical
Pacific. -
- Statistical and coupled model forecasts indicate
that El Niño conditions will continue through the
end of 2002 and into the first half of 2003. - Some impacts on the United States are expected,
starting in the fall 2002, but they should
generally be weaker than those during the very
strong 1997-98 El Niño.