ENSO: Recent Evolution,
Current Status and Predictions
Update prepared by:
Climate Prediction Center / NCEP
15 January 2024
Outline
Summary
Recent Evolution and Current Conditions
Oceanic Niño Index (ONI)
Pacific SST Outlook
U.S. Seasonal Precipitation and Temperature Outlooks
Summary
Summary
* Note: These statements are updated once a month (2nd Thursday of each month) in association
with the ENSO Diagnostics Discussion, which can be found by clicking here.
ENSO Alert System Status: El Niño Advisory
El Niño conditions are observed.*
Equatorial sea surface temperatures (SSTs) are above average across the
central and eastern Pacific Ocean.
The tropical Pacific atmospheric anomalies are consistent with El Niño.
El Niño is expected to continue for the next several seasons, with ENSO-neutral
favored during April-June 2024 (73% chance).*
Since March 2023, positive sea surface
temperature (SST) anomalies in the
eastern Pacific Ocean gradually
expanded and shifted westward.
In October and November 2023, SST
anomalies increased in the central and
east-central Pacific. Since early
December, the positive SST anomalies
have persisted.
In the far eastern Pacific, positive SST
anomalies have been gradually
weakening.
Recent Evolution of
Equatorial Pacific SST
Departures (oC)
Niño Region SST
Departures (oC) Recent
Evolution
The latest weekly
SST departures are:
Niño 4 1.5ºC
Niño 3.4 1.9ºC
Niño 3 2.0ºC
Niño 1+2 0.9ºC
SST Departures (oC) in the Tropical Pacific During the Last
Four Weeks
In the last four weeks, equatorial SSTs were above average across most of the Pacific
Ocean.
26
30
Global SST Departures (oC) During the Last Four Weeks
During the last four weeks, equatorial SSTs were above average across most of the Pacific Ocean,
the Indian Ocean, and the Atlantic Ocean.
26
30
30
Weekly SST Departures
during the Last Four
Weeks
During the last 4 weeks, above-average SSTs
persisted across much of the central and
east-central equatorial Pacific Ocean, while
weakening in the far eastern Pacific.
Positive SST anomalies have increased over
the far western Pacific Ocean.
Change in Weekly SST Departures over the Last Four
Weeks
During the last four weeks, negative changes in equatorial SST anomalies were observed
in the central and far eastern Pacific Ocean, while positive changes were evident over the
western Pacific Ocean.
Upper-Ocean Conditions in
the Equatorial Pacific
The basin-wide equatorial upper ocean (0-300 m)
heat content is greatest prior to and during the
early stages of a Pacific warm (El Niño) episode
(compare top 2 panels), and least prior to and
during the early stages of a cold (La Niña)
episode.
The slope of the oceanic thermocline is least
(greatest) during warm (cold) episodes.
Recent values of the upper-ocean heat
anomalies (above average) and thermocline
slope index (below average) reflect El Niño.
The monthly thermocline slope index represents the
difference in anomalous depth of the 20ºC isotherm
between the western Pacific (160ºE-150ºW) and the
eastern Pacific (90º-140ºW).
Central and Eastern Pacific Upper-Ocean (0-300 m)
Weekly Average Temperature Anomalies
Subsurface temperature anomalies were negative until mid-February 2023. Subsurface anomalies
became positive in February and increased through mid-April 2023 before leveling off. From late May
to mid-June 2023, anomalies increased. Anomalies decreased from mid-June to mid-July, increased
from late July through August, decreased in September, increased from early October through late
November, and decreased during December. Recently, positive anomalies have persisted.
Sub-Surface Temperature Departures in the Equatorial
Pacific
Most recent pentad analysis
Positive subsurface temperature anomalies dominate
most of the equatorial Pacific Ocean.
Negative subsurface temperature anomalies have
strengthened in the western Pacific Ocean and
expanded to ~150ºW, while remaining at depth.
Tropical OLR and Wind
Anomalies During the Last
30 Days
Positive OLR anomalies (suppressed convection
and precipitation) were evident around Indonesia,
the Philippines, and northern Australia. Negative
OLR anomalies (enhanced convection and
precipitation) were observed around the Date
Line, and extend into the eastern tropical Pacific,
mostly north of the equator.
Low-level (850-hPa) wind anomalies were
westerly over the east-central equatorial
Pacific, and were easterly over the far western
Pacific.
Upper-level (200-hPa) wind anomalies were
easterly along the east-central and eastern
equatorial Pacific. An anomalous anticylonic
couplet straddles the equator in the east-
central Pacific.
A
A
Intraseasonal Variability
Intraseasonal variability in the atmosphere (wind and pressure), which is often related
to the Madden-Julian Oscillation (MJO), can significantly impact surface and subsurface
conditions across the Pacific Ocean.
Related to this activity:
Significant weakening of the low-level easterly winds usually initiates an eastward-
propagating oceanic Kelvin wave.
Weekly Heat Content
Evolution in the Equatorial
Pacific
Equatorial oceanic Kelvin waves have alternating
warm and cold phases. The warm phase is
indicated by dashed lines. Down-welling and
warming occur in the leading portion of a Kelvin
wave, and up-welling and cooling occur in the
trailing portion.
Significant equatorial oceanic Kelvin wave activity
(dashed and dotted lines) has been present
throughout the period shown. Six downwelling
waves have occurred since late November 2022.
Since March 2023, above-average subsurface
temperature anomalies have persisted across most
of the Pacific Ocean.
Since early November 2023, below-average
temperature anomalies have strengthened in the
western Pacific Ocean.
Low-level (850-hPa)
Zonal (east-west) Wind
Anomalies (m s-1)
Starting in mid-July 2023, westerly wind
anomalies became more predominant
over the equatorial Pacific Ocean.
At times, the Madden Julian-Oscillation
(MJO) has contributed to the eastward
propagation of low-level wind anomalies.
An eastward propagating pattern of
westerly and easterly wind anomalies was
evident starting in November 2023.
Westerly Wind Anomalies (orange/red shading)
Easterly Wind Anomalies (blue shading)
Upper-level (200-hPa)
Velocity Potential
Anomalies
Unfavorable for precipitation (brown shading)
Favorable for precipitation (green shading)
Note: Eastward propagation is not necessarily indicative of the Madden-Julian Oscillation (MJO).
Since the beginning of the period,
anomalous divergence (green shading) has
generally persisted near the Date Line,
while anomalous convergence (brown
shading) was mostly observed over South
America.
From late September to mid-November
2023, anomalous convergence strengthened
near Indonesia.
In November and December, eastward
propagation in the velocity potential
anomalies was observed.
Outgoing Longwave
Radiation (OLR) Anomalies
Drier-than-average Conditions (orange/red shading)
Wetter-than-average Conditions (blue shading)
During the period, negative OLR
anomalies (more convection) persisted
over the central equatorial Pacific Ocean,
and periodically emerged in the eastern
Pacific.
Since mid-July 2023, positive OLR
anomalies persisted around Indonesia.
Oceanic Niño Index (ONI)
The ONI is based on SST departures from average in the Niño 3.4 region, and is a
principal measure for monitoring, assessing, and predicting ENSO.
Defined as the three-month running-mean SST departures in the Niño 3.4 region.
Departures are based on a set of improved homogeneous historical SST analyses
(Extended Reconstructed SST – ERSST.v5). The SST reconstruction methodology is
described in Huang et al., 2017, J. Climate, vol. 30, 8179-8205.)
It is one index that helps to place current events into a historical perspective.
Note: a different SST dataset is used for weekly SST monitoring (slides #4-9) and is
using OISSTv2.1 (Huang et al., 2021).
NOAA Operational Definitions for El Niño and La Niña
El Niño: characterized by a positive ONI greater than or equal to +0.5ºC.
La Niña: characterized by a negative ONI less than or equal to -0.5ºC.
By historical standards, to be classified as a full-fledged El Niño or La Niña episode,
these thresholds must be exceeded for a period of at least 5 consecutive overlapping
3-month seasons.
CPC considers El Niño or La Niña conditions to occur when the monthly Niño3.4 OISST
departures meet or exceed +/- 0.5ºC along with consistent atmospheric features. These
anomalies must also be forecasted to persist for 3 consecutive months.
ONI (ºC): Evolution
since 1950
The most recent ONI value
(October – December 2023) is
1.9ºC.
El Niño
La Niña
Neutral
Historical El Niño and La Niña Episodes Based on the
ONI computed using ERSST.v5
Recent Pacific warm (red) and cold (blue) periods based on a threshold of +/- 0.5 ºC for the Oceanic
Nino Index (ONI) [3 month running mean of ERSST.v5 SST anomalies in the Nino 3.4 region (5N-5S, 120-170W)].
For historical purposes, periods of below and above normal SSTs are colored in blue and red when the
threshold is met for a minimum of 5 consecutive over-lapping seasons.
The ONI is one measure of the El Niño-Southern Oscillation, and other indices can confirm whether
features consistent with a coupled ocean-atmosphere phenomenon accompanied these periods. The complete
table going back to DJF 1950 can be found here.
Year DJF JFM FMA MAM AMJ MJJ JJA JAS ASO SON OND NDJ
2011 -1.4 -1.2 -0.9 -0.7 -0.6 -0.4 -0.5 -0.6 -0.8 -1.0 -1.1 -1.0
2012 -0.9 -0.7 -0.6 -0.5 -0.3 0.0 0.2 0.4 0.4 0.3 0.1 -0.2
2013 -0.4 -0.4 -0.3 -0.3 -0.4 -0.4 -0.4 -0.3 -0.3 -0.2 -0.2 -0.3
2014 -0.4 -0.5 -0.3 0.0 0.2 0.2 0.0 0.1 0.2 0.5 0.6 0.7
2015 0.5 0.5 0.5 0.7 0.9 1.2 1.5 1.9 2.2 2.4 2.6 2.6
2016 2.5 2.1 1.6 0.9 0.4 -0.1 -0.4 -0.5 -0.6 -0.7 -0.7 -0.6
2017 -0.3 -0.2 0.1 0.2 0.3 0.3 0.1 -0.1 -0.4 -0.7 -0.8 -1.0
2018 -0.9 -0.9 -0.7 -0.5 -0.2 0.0 0.1 0.2 0.5 0.8 0.9 0.8
2019 0.7 0.7 0.7 0.7 0.5 0.5 0.3 0.1 0.2 0.3 0.5 0.5
2020 0.5 0.5 0.4 0.2 -0.1 -0.3 -0.4 -0.6 -0.9 -1.2 -1.3 -1.2
2021 -1.0 -0.9 -0.8 -0.7 -0.5 -0.4 -0.4 -0.5 -0.7 -0.8 -1.0 -1.0
2022 -1.0 -0.9 -1.0 -1.1 -1.0 -0.9 -0.8 -0.9 -1.0 -1.0 -0.9 -0.8
2023 -0.7 -0.4 -0.1 0.2 0.5 0.8 1.1 1.3 1.6 1.8 1.9
CPC Probabilistic ENSO Outlook
Updated: 11 January 2024
El Niño is expected to continue for the next several seasons, with chances gradually
decreasing from the winter through the spring. A transition to ENSO-neutral is anticipated
by April-June 2024 (73% chance).
IRI Pacific Niño 3.4
SST Model Outlook
Figure provided by the International Research
Institute (IRI) for Climate and Society
(updated 19 December 2023).
The majority of models indicate El
Niño will persist through March-
May 2024 and then transition to
ENSO-neutral.
SST Outlook: NCEP CFS.v2 Forecast (PDF corrected)
Issued: 15 January 2024
The CFS.v2 ensemble mean (black dashed line) indicates El Niño may transition
to ENSO-neutral by March-May 2024.
Atmospheric anomalies over
the North Pacific and North
America During the Last 60
Days
1 of 3
From mid-November through December, below-
average heights persisted in the eastern North
Pacific Ocean, with above-average heights and
temperatures evident over the northern tier of
the U.S. and western Canada.
Recently, below-average heights have shifted
over the contiguous U.S., with below-average
temperatures observed over the southern tier of
the U.S.
2 of 3
Atmospheric anomalies over
the North Pacific and North
America During the Last 60
Days
From mid-November through December, below-
average heights persisted in the eastern North
Pacific Ocean, with above-average heights and
temperatures evident over the northern tier of
the U.S. and western Canada.
Recently, below-average heights have shifted
over the contiguous U.S., with below-average
temperatures observed over the southern tier of
the U.S.
3 of 3
Atmospheric anomalies over
the North Pacific and North
America During the Last 60
Days
From mid-November through December, below-
average heights persisted in the eastern North
Pacific Ocean, with above-average heights and
temperatures evident over the northern tier of
the U.S. and western Canada.
Recently, below-average heights have shifted
over the contiguous U.S., with below-average
temperatures observed over the southern tier of
the U.S.
U.S. Temperature and Precipitation Departures During
the Last 30 Days
End Date: 13 January 2024
Percent of Average Precipitation Temperature Departures (degree C)
1 of 2
U.S. Temperature and Precipitation Departures During
the Last 90 Days
Percent of Average Precipitation Temperature Departures (degree C)
2 of 2
End Date: 13 January 2024
U. S. Seasonal Outlooks
Precipitation Temperature
January – March 2024
The seasonal outlooks combine the effects of long-term trends, soil moisture,
and, when appropriate, ENSO.
Summary
* Note: These statements are updated once a month (2nd Thursday of each month) in association
with the ENSO Diagnostics Discussion, which can be found by clicking here.
ENSO Alert System Status: El Niño Advisory
El Niño conditions are observed.*
Equatorial sea surface temperatures (SSTs) are above average across the
central and eastern Pacific Ocean.
The tropical Pacific atmospheric anomalies are consistent with El Niño.
El Niño is expected to continue for the next several seasons, with ENSO-neutral
favored during April-June 2024 (73% chance).*

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enso_evolution-status-fcsts-web.ppt

  • 1. ENSO: Recent Evolution, Current Status and Predictions Update prepared by: Climate Prediction Center / NCEP 15 January 2024
  • 2. Outline Summary Recent Evolution and Current Conditions Oceanic Niño Index (ONI) Pacific SST Outlook U.S. Seasonal Precipitation and Temperature Outlooks Summary
  • 3. Summary * Note: These statements are updated once a month (2nd Thursday of each month) in association with the ENSO Diagnostics Discussion, which can be found by clicking here. ENSO Alert System Status: El Niño Advisory El Niño conditions are observed.* Equatorial sea surface temperatures (SSTs) are above average across the central and eastern Pacific Ocean. The tropical Pacific atmospheric anomalies are consistent with El Niño. El Niño is expected to continue for the next several seasons, with ENSO-neutral favored during April-June 2024 (73% chance).*
  • 4. Since March 2023, positive sea surface temperature (SST) anomalies in the eastern Pacific Ocean gradually expanded and shifted westward. In October and November 2023, SST anomalies increased in the central and east-central Pacific. Since early December, the positive SST anomalies have persisted. In the far eastern Pacific, positive SST anomalies have been gradually weakening. Recent Evolution of Equatorial Pacific SST Departures (oC)
  • 5. Niño Region SST Departures (oC) Recent Evolution The latest weekly SST departures are: Niño 4 1.5ºC Niño 3.4 1.9ºC Niño 3 2.0ºC Niño 1+2 0.9ºC
  • 6. SST Departures (oC) in the Tropical Pacific During the Last Four Weeks In the last four weeks, equatorial SSTs were above average across most of the Pacific Ocean. 26 30
  • 7. Global SST Departures (oC) During the Last Four Weeks During the last four weeks, equatorial SSTs were above average across most of the Pacific Ocean, the Indian Ocean, and the Atlantic Ocean. 26 30 30
  • 8. Weekly SST Departures during the Last Four Weeks During the last 4 weeks, above-average SSTs persisted across much of the central and east-central equatorial Pacific Ocean, while weakening in the far eastern Pacific. Positive SST anomalies have increased over the far western Pacific Ocean.
  • 9. Change in Weekly SST Departures over the Last Four Weeks During the last four weeks, negative changes in equatorial SST anomalies were observed in the central and far eastern Pacific Ocean, while positive changes were evident over the western Pacific Ocean.
  • 10. Upper-Ocean Conditions in the Equatorial Pacific The basin-wide equatorial upper ocean (0-300 m) heat content is greatest prior to and during the early stages of a Pacific warm (El Niño) episode (compare top 2 panels), and least prior to and during the early stages of a cold (La Niña) episode. The slope of the oceanic thermocline is least (greatest) during warm (cold) episodes. Recent values of the upper-ocean heat anomalies (above average) and thermocline slope index (below average) reflect El Niño. The monthly thermocline slope index represents the difference in anomalous depth of the 20ºC isotherm between the western Pacific (160ºE-150ºW) and the eastern Pacific (90º-140ºW).
  • 11. Central and Eastern Pacific Upper-Ocean (0-300 m) Weekly Average Temperature Anomalies Subsurface temperature anomalies were negative until mid-February 2023. Subsurface anomalies became positive in February and increased through mid-April 2023 before leveling off. From late May to mid-June 2023, anomalies increased. Anomalies decreased from mid-June to mid-July, increased from late July through August, decreased in September, increased from early October through late November, and decreased during December. Recently, positive anomalies have persisted.
  • 12. Sub-Surface Temperature Departures in the Equatorial Pacific Most recent pentad analysis Positive subsurface temperature anomalies dominate most of the equatorial Pacific Ocean. Negative subsurface temperature anomalies have strengthened in the western Pacific Ocean and expanded to ~150ºW, while remaining at depth.
  • 13. Tropical OLR and Wind Anomalies During the Last 30 Days Positive OLR anomalies (suppressed convection and precipitation) were evident around Indonesia, the Philippines, and northern Australia. Negative OLR anomalies (enhanced convection and precipitation) were observed around the Date Line, and extend into the eastern tropical Pacific, mostly north of the equator. Low-level (850-hPa) wind anomalies were westerly over the east-central equatorial Pacific, and were easterly over the far western Pacific. Upper-level (200-hPa) wind anomalies were easterly along the east-central and eastern equatorial Pacific. An anomalous anticylonic couplet straddles the equator in the east- central Pacific. A A
  • 14. Intraseasonal Variability Intraseasonal variability in the atmosphere (wind and pressure), which is often related to the Madden-Julian Oscillation (MJO), can significantly impact surface and subsurface conditions across the Pacific Ocean. Related to this activity: Significant weakening of the low-level easterly winds usually initiates an eastward- propagating oceanic Kelvin wave.
  • 15. Weekly Heat Content Evolution in the Equatorial Pacific Equatorial oceanic Kelvin waves have alternating warm and cold phases. The warm phase is indicated by dashed lines. Down-welling and warming occur in the leading portion of a Kelvin wave, and up-welling and cooling occur in the trailing portion. Significant equatorial oceanic Kelvin wave activity (dashed and dotted lines) has been present throughout the period shown. Six downwelling waves have occurred since late November 2022. Since March 2023, above-average subsurface temperature anomalies have persisted across most of the Pacific Ocean. Since early November 2023, below-average temperature anomalies have strengthened in the western Pacific Ocean.
  • 16. Low-level (850-hPa) Zonal (east-west) Wind Anomalies (m s-1) Starting in mid-July 2023, westerly wind anomalies became more predominant over the equatorial Pacific Ocean. At times, the Madden Julian-Oscillation (MJO) has contributed to the eastward propagation of low-level wind anomalies. An eastward propagating pattern of westerly and easterly wind anomalies was evident starting in November 2023. Westerly Wind Anomalies (orange/red shading) Easterly Wind Anomalies (blue shading)
  • 17. Upper-level (200-hPa) Velocity Potential Anomalies Unfavorable for precipitation (brown shading) Favorable for precipitation (green shading) Note: Eastward propagation is not necessarily indicative of the Madden-Julian Oscillation (MJO). Since the beginning of the period, anomalous divergence (green shading) has generally persisted near the Date Line, while anomalous convergence (brown shading) was mostly observed over South America. From late September to mid-November 2023, anomalous convergence strengthened near Indonesia. In November and December, eastward propagation in the velocity potential anomalies was observed.
  • 18. Outgoing Longwave Radiation (OLR) Anomalies Drier-than-average Conditions (orange/red shading) Wetter-than-average Conditions (blue shading) During the period, negative OLR anomalies (more convection) persisted over the central equatorial Pacific Ocean, and periodically emerged in the eastern Pacific. Since mid-July 2023, positive OLR anomalies persisted around Indonesia.
  • 19. Oceanic Niño Index (ONI) The ONI is based on SST departures from average in the Niño 3.4 region, and is a principal measure for monitoring, assessing, and predicting ENSO. Defined as the three-month running-mean SST departures in the Niño 3.4 region. Departures are based on a set of improved homogeneous historical SST analyses (Extended Reconstructed SST – ERSST.v5). The SST reconstruction methodology is described in Huang et al., 2017, J. Climate, vol. 30, 8179-8205.) It is one index that helps to place current events into a historical perspective. Note: a different SST dataset is used for weekly SST monitoring (slides #4-9) and is using OISSTv2.1 (Huang et al., 2021).
  • 20. NOAA Operational Definitions for El Niño and La Niña El Niño: characterized by a positive ONI greater than or equal to +0.5ºC. La Niña: characterized by a negative ONI less than or equal to -0.5ºC. By historical standards, to be classified as a full-fledged El Niño or La Niña episode, these thresholds must be exceeded for a period of at least 5 consecutive overlapping 3-month seasons. CPC considers El Niño or La Niña conditions to occur when the monthly Niño3.4 OISST departures meet or exceed +/- 0.5ºC along with consistent atmospheric features. These anomalies must also be forecasted to persist for 3 consecutive months.
  • 21. ONI (ºC): Evolution since 1950 The most recent ONI value (October – December 2023) is 1.9ºC. El Niño La Niña Neutral
  • 22. Historical El Niño and La Niña Episodes Based on the ONI computed using ERSST.v5 Recent Pacific warm (red) and cold (blue) periods based on a threshold of +/- 0.5 ºC for the Oceanic Nino Index (ONI) [3 month running mean of ERSST.v5 SST anomalies in the Nino 3.4 region (5N-5S, 120-170W)]. For historical purposes, periods of below and above normal SSTs are colored in blue and red when the threshold is met for a minimum of 5 consecutive over-lapping seasons. The ONI is one measure of the El Niño-Southern Oscillation, and other indices can confirm whether features consistent with a coupled ocean-atmosphere phenomenon accompanied these periods. The complete table going back to DJF 1950 can be found here. Year DJF JFM FMA MAM AMJ MJJ JJA JAS ASO SON OND NDJ 2011 -1.4 -1.2 -0.9 -0.7 -0.6 -0.4 -0.5 -0.6 -0.8 -1.0 -1.1 -1.0 2012 -0.9 -0.7 -0.6 -0.5 -0.3 0.0 0.2 0.4 0.4 0.3 0.1 -0.2 2013 -0.4 -0.4 -0.3 -0.3 -0.4 -0.4 -0.4 -0.3 -0.3 -0.2 -0.2 -0.3 2014 -0.4 -0.5 -0.3 0.0 0.2 0.2 0.0 0.1 0.2 0.5 0.6 0.7 2015 0.5 0.5 0.5 0.7 0.9 1.2 1.5 1.9 2.2 2.4 2.6 2.6 2016 2.5 2.1 1.6 0.9 0.4 -0.1 -0.4 -0.5 -0.6 -0.7 -0.7 -0.6 2017 -0.3 -0.2 0.1 0.2 0.3 0.3 0.1 -0.1 -0.4 -0.7 -0.8 -1.0 2018 -0.9 -0.9 -0.7 -0.5 -0.2 0.0 0.1 0.2 0.5 0.8 0.9 0.8 2019 0.7 0.7 0.7 0.7 0.5 0.5 0.3 0.1 0.2 0.3 0.5 0.5 2020 0.5 0.5 0.4 0.2 -0.1 -0.3 -0.4 -0.6 -0.9 -1.2 -1.3 -1.2 2021 -1.0 -0.9 -0.8 -0.7 -0.5 -0.4 -0.4 -0.5 -0.7 -0.8 -1.0 -1.0 2022 -1.0 -0.9 -1.0 -1.1 -1.0 -0.9 -0.8 -0.9 -1.0 -1.0 -0.9 -0.8 2023 -0.7 -0.4 -0.1 0.2 0.5 0.8 1.1 1.3 1.6 1.8 1.9
  • 23. CPC Probabilistic ENSO Outlook Updated: 11 January 2024 El Niño is expected to continue for the next several seasons, with chances gradually decreasing from the winter through the spring. A transition to ENSO-neutral is anticipated by April-June 2024 (73% chance).
  • 24. IRI Pacific Niño 3.4 SST Model Outlook Figure provided by the International Research Institute (IRI) for Climate and Society (updated 19 December 2023). The majority of models indicate El Niño will persist through March- May 2024 and then transition to ENSO-neutral.
  • 25. SST Outlook: NCEP CFS.v2 Forecast (PDF corrected) Issued: 15 January 2024 The CFS.v2 ensemble mean (black dashed line) indicates El Niño may transition to ENSO-neutral by March-May 2024.
  • 26. Atmospheric anomalies over the North Pacific and North America During the Last 60 Days 1 of 3 From mid-November through December, below- average heights persisted in the eastern North Pacific Ocean, with above-average heights and temperatures evident over the northern tier of the U.S. and western Canada. Recently, below-average heights have shifted over the contiguous U.S., with below-average temperatures observed over the southern tier of the U.S.
  • 27. 2 of 3 Atmospheric anomalies over the North Pacific and North America During the Last 60 Days From mid-November through December, below- average heights persisted in the eastern North Pacific Ocean, with above-average heights and temperatures evident over the northern tier of the U.S. and western Canada. Recently, below-average heights have shifted over the contiguous U.S., with below-average temperatures observed over the southern tier of the U.S.
  • 28. 3 of 3 Atmospheric anomalies over the North Pacific and North America During the Last 60 Days From mid-November through December, below- average heights persisted in the eastern North Pacific Ocean, with above-average heights and temperatures evident over the northern tier of the U.S. and western Canada. Recently, below-average heights have shifted over the contiguous U.S., with below-average temperatures observed over the southern tier of the U.S.
  • 29. U.S. Temperature and Precipitation Departures During the Last 30 Days End Date: 13 January 2024 Percent of Average Precipitation Temperature Departures (degree C) 1 of 2
  • 30. U.S. Temperature and Precipitation Departures During the Last 90 Days Percent of Average Precipitation Temperature Departures (degree C) 2 of 2 End Date: 13 January 2024
  • 31. U. S. Seasonal Outlooks Precipitation Temperature January – March 2024 The seasonal outlooks combine the effects of long-term trends, soil moisture, and, when appropriate, ENSO.
  • 32. Summary * Note: These statements are updated once a month (2nd Thursday of each month) in association with the ENSO Diagnostics Discussion, which can be found by clicking here. ENSO Alert System Status: El Niño Advisory El Niño conditions are observed.* Equatorial sea surface temperatures (SSTs) are above average across the central and eastern Pacific Ocean. The tropical Pacific atmospheric anomalies are consistent with El Niño. El Niño is expected to continue for the next several seasons, with ENSO-neutral favored during April-June 2024 (73% chance).*