1 ENSO: Recent Evolution, Current Status and Predictions Update prepared by: Climate Prediction Center / NCEP 29 June 2015
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 El Niño conditions are present.* ENSO Alert System Status: El Niño Advisory Positive equatorial sea surface temperature (SST) anomalies continue across most of the Pacific Ocean. There is a greater than 90% chance that El Niño will continue through Northern Hemisphere fall 2015, and around an 85% chance it will last through the winter.* * Note: These statements are updated once a month (2 nd Thursday of each month) in association with the ENSO Diagnostics Discussion, which can be found by clicking here.
4 Recent Evolution of Equatorial Pacific SST Departures ( o C) During September-December 2014, positive SST anomalies covered most of the equatorial Pacific. During January through mid-march 2015, near-to-below average SSTs were observed in the eastern Pacific, and positive SST anomalies persisted across the western and central Pacific. During the last three months, positive SST anomalies strengthened across the eastern Pacific.
5 Niño Region SST Departures ( o C) Recent Evolution The latest weekly SST departures are: Niño 4 Niño 3.4 Niño 3 Niño ºC 1.4ºC 1.9ºC 2.6ºC
6 SST Departures ( o C) in the Tropical Pacific During the Last Four Weeks During the last four weeks, equatorial SSTs were above average across the central and eastern Pacific, with the largest anomalies off the coast of S. America.
7 Global SST Departures ( o C) During the Last Four Weeks During the last four weeks, equatorial SSTs were above average across the central and eastern Pacific and the Indian Ocean.
8 Weekly SST Departures during the Last Four Weeks During the last four weeks, positive equatorial SST anomalies extended across most of the Pacific.
9 Change in Weekly SST Departures over the Last Four Weeks During the last four weeks, an increase in equatorial SST anomalies occurred in the eastern Pacific.
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 (positive) and thermocline slope index (negative) reflect El Niño conditions. 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 increased from mid-october to mid-november 2014 before decreasing to near zero in early January Temperature anomalies grew from January to March, decreased during April, and increased during May. During June, anomalies have decreased.
12 Sub-Surface Temperature Departures in the Equatorial Pacific During the last two months, positive subsurface temperature anomalies were observed across most of the equatorial Pacific Most recent pentad analysis In the western Pacific, negative anomalies at depth have shifted slightly eastward.
13 Tropical OLR and Wind Anomalies During the Last 30 Days Negative OLR anomalies (enhanced convection and precipitation) were evident across the central and eastern tropical Pacific. Positive OLR anomalies (suppressed convection and precipitation) were located near Indonesia and the Philippines. Anomalous low-level (850-hPa) westerly winds were located across the east-central equatorial Pacific. Anomalous upper-level (200-hPa) easterlies were observed over the central equatorial Pacific. An anomalous anticyclonic couplet straddled the equator over the east-central tropical 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 eastwardpropagating oceanic Kelvin wave.
15 Weekly Heat Content Evolution in the Equatorial Pacific During November - January, the upwelling phase of a Kelvin wave shifted eastward. This was followed by a significant downwelling Kelvin wave. Since mid May, another downwelling phase of a Kelvin wave has shifted eastward. 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.
16 Low-level (850-hPa) Zonal (east-west) Wind Anomalies (m s -1 ) During early March and early May, westerly wind bursts were observed between 140ºE and 180º. In the last couple of weeks, westerly wind anomalies were evident across the western equatorial Pacific. Westerly Wind Anomalies (orange/red shading) Easterly Wind Anomalies (blue shading)
17 Upper-level (200-hPa) Velocity Potential Anomalies During March 2015, the Madden-Julian Oscillation (MJO) was associated with eastward propagating velocity potential anomalies. Since mid-january 2015, negative anomalies and anomalous upper-level divergence (green shading) have mostly prevailed near the Date Line and/or eastern Pacific. In the last week, an MJO contributed to upper-level divergence shifting eastward across the tropical Pacific. Unfavorable for precipitation (brown shading) Favorable for precipitation (green shading)
18 Outgoing Longwave Radiation (OLR) Anomalies During early March, negative OLR anomalies shifted from Indonesia to the Date Line, where they persisted until late May. Since early May, negative OLR anomalies have persisted in the eastern Pacific. More recently, negative anomalies have redeveloped in the central Pacific. Drier-than-average Conditions (orange/red shading) Wetter-than-average Conditions (blue shading)
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.v4). The SST reconstruction methodology is described in Huang et al., 2015, J. Climate, vol. 28, ) It is one index that helps to place current events into a historical perspective
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 (March May 2015) is 0.7 o C. El Niño Neutral La Niña
22 Historical El Niño and La Niña Episodes Based on the ONI computed using ERSST.v4 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.v4 SST anomalies in the Nino 3.4 region (5N-5S, W)]. 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
23 CPC/IRI Probabilistic ENSO Outlook Updated: 11 June 2015 The chance of El Niño is at least 85% into early 2016.
24 IRI/CPC Pacific Niño 3.4 SST Model Outlook Almost all of the models indicate Niño 3.4 SST anomalies will remain greater than or equal to +0.5C through the end of The dynamical model average and CPC CON suggest that Niño 3.4 will exceed +1.5C (a strong El Niño) later on this year. Figure provided by the International Research Institute (IRI) for Climate and Society (updated 16 June 2015).
25 SST Outlook: NCEP CFS.v2 Forecast (PDF corrected) Issued: 29 June 2015 The CFS.v2 ensemble mean (black dashed line) predicts El Niño through JFM 2016.
26 Atmospheric anomalies over the North Pacific and North America During the Last 60 Days From May June 2015, above average heights and temperatures have generally prevailed over eastern and western North America. 1 of 3
27 Atmospheric anomalies over the North Pacific and North America During the Last 60 Days From May June 2015, above average heights and temperatures have generally prevailed over eastern and western North America. 2 of 3
28 Atmospheric anomalies over the North Pacific and North America During the Last 60 Days From May June 2015, above average heights and temperatures have generally prevailed over eastern and western North America. 3 of 3
29 U.S. Temperature and Precipitation Departures During the Last 30 Days End Date: 27 June 2015 Percent of Average Precipitation Temperature Departures (degree C) 1 of 2
30 U.S. Temperature and Precipitation Departures During the Last 90 Days End Date: 27 June 2015 Percent of Average Precipitation Temperature Departures (degree C) 2 of 2
31 U. S. Seasonal Outlooks July September 2015 The seasonal outlooks combine the effects of long-term trends, soil moisture, and, when appropriate, ENSO. Precipitation Temperature
32 Summary El Niño conditions are present.* ENSO Alert System Status: El Niño Advisory Positive equatorial sea surface temperature (SST) anomalies continue across most of the Pacific Ocean. There is a greater than 90% chance that El Niño will continue through Northern Hemisphere fall 2015, and around an 85% chance it will last through the winter.* * Note: These statements are updated once a month (2 nd Thursday of each month) in association with the ENSO Diagnostics Discussion, which can be found by clicking here.
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