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June El Niño update: Damn the torpedoes, full speed ahead

El Niño continues to pick up steam. NOAA CPC/IRI forecasters are now very confident that the event will continue through the fall (over 90% chance) and into the winter (~85% chance). Now that we’re emerging from the spring barrier, this month’s update provides a first guess of the potential strength of El Niño. It’s harder to predict the strength of the event than it is to predict its duration, so we are less confident about that, but forecasters currently favor a “strong” event for the fall/early winter. By “strong” we mean it’s expected that the three-month average sea surface temperature in the Niño3.4 region will peak at more than 1.5°C (2.7°F) above normal.

What’s happening right now?

During the month of May, we saw increases in a lot of the ENSO indicators. Sea surface temperature anomalies (the departure from average) were up all across the tropical Pacific, and the most recent Niño3.4 Index was 1.2°C. Both the lower-level and upper-level winds along the equator were substantially weaker than average last month, characteristic of El Niño’s weakened Walker Circulation. This feedback between the higher sea surface temperature anomalies and the atmosphere is critical to both perpetuating and strengthening an El Niño event, and to communicating the effects of El Niño to other areas of the globe.

Signs of another downwelling Kelvin wave have begun to appear in the upper levels of the equatorial Pacific. This reinforcing source of warmer-than-average waters follows the strong Kelvin wave that has been slowly moving east since February. The consistently warmer waters are reflective of the slower changes we’d expect to see when the ocean-atmosphere system has settled into an ENSO event, as opposed to the shorter-term changes that dominate the rest of the time.

Upper-ocean temperature anomalies

Hovmoeller plot showing the changes in upper-ocean heat content over the past year. The vertical axis shows time, starting in June 2014 (top) and going through June 2015 (bottom). Horizontal axis spans the equatorial Pacific Ocean, from 130°E to 80°W. Each row in the plot is the average temperature anomaly of the upper 300 m. For example, the last Kelvin wave (area of warmer-than-average waters) develops near the Date Line in March, and slowly moves eastward through time. For more on how to interpret these graphs, check out Tom’s post. CPC figure.

What signs are suggesting a possible strong event?

The physical observations I described above are a source of confidence that this event is continuing to build. Also, most climate models are forecasting a continued increase in Niño3.4 sea surface temperature anomalies, and many forecast a peak in the early winter above 1.5°, some above 2.0°C.

NMME model forecasts, June 2015

Climate model forecasts for the Niño3.4 Index, from the North American Multi-Model Ensemble (NMME). Darker purple envelope shows the range of 65% of all model forecasts; lighter purple shows the range of 98% of all model forecasts. NOAA Climate.gov image by Fiona Martin from CPC data.

It’s important to remember, though, that we only have a handful of strong El Niño events in the historical record—seven since 1950. And only three of those saw Niño3.4 index values of 2.0°C or higher: 1972-73, 1997-98 and 1982-83)*. Imagine if we’d only had seven hurricanes in the history of record-keeping; it would make it much harder to understand and predict how a future hurricane could develop. So, while we’re confident that this El Niño event will continue, there’s still plenty of uncertainty about how it will evolve.

That said… what would a strong event mean?

As Tony pointed out in our last post, ENSO impacts on North American weather and climate are most noticeable in the winter. This is largely because winter weather is governed more by large-scale processes (e.g. nor’easters) than summer weather, when local effects (e.g. isolated thunderstorms) tend to be more important. El Niño events affect the strength and position of the jet stream, and tilt the odds toward more rain than average along the West coast and in the Southeast during the winter.

El Niño loads the dice in favor of certain impacts, but it doesn’t guarantee them. However, stronger events tend to lead to more predictable effects. My brother asked me if he should repair the leaks in the roof of his campervan before he goes to Florida this winter… based on the ENSO forecast, I said yes. (I would probably have said yes anyway —who wants to stay in a drafty camper?— but that’s beside the point.)

Wintertime El Nino pattern

Changes in the winter atmosphere during El Niño. NOAA Climate.gov image by Fiona Martin. 

Globally, this El Niño event is likely to lead to higher global temperatures, possibly record-breaking. On this, check out Deke Arndt’s post on our new sister blog, Beyond the Data. Also, as I mentioned last month, the tropical Pacific hurricane season is already breaking records, while the Atlantic hurricane season is forecast to be quieter than average—both effects linked to El Niño. For the coming summer (June-August), check out Tony’s post on potential temperature and precipitation impacts linked to El Niño.

Many, many different components are at work in the global climate system, making exact predictions impossible. However, the development of a climate phenomenon like El Niño can make some outcomes more likely than others, which is why we follow it so closely. We’ll keep you posted as this event continues.

*This is based on the current version of ERSST, ERSSTv3b. ERSSTv4 will be released next week, and may slightly change the ONI values (and therefore the number of events >1.5°C).

Comments

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how about showing the effects on Alaska and Hawaii? We're part of the U.S.! I'm in Alaska, I think based on previous El Niño we will be warm. But it would like to see NOAA include these states, we pay taxes too!

Submitted by Tempy Larew on Thu, 06/11/2015 - 17:48

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Here you go: http://www.claimsjournal.com/news/west/2015/05/22/263536.htm http://www.alaskapublic.org/2015/05/20/el-nino-returns/

Submitted by Anonymous on Fri, 06/12/2015 - 11:17

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podran publicarlo en espanol y como afectara baja calfornia gracias

Submitted by sergio tamez on Thu, 06/11/2015 - 18:50

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This could lead to a Mild start to Winter 2015-16, less snow.

Submitted by Benjamin Lovell on Thu, 06/11/2015 - 21:37

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Love the title of the article!

Submitted by Timothy on Fri, 06/12/2015 - 01:22

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Thanks,Interesting..Maybe California will get a break and some rain,lots of rain this fall and winter.

Submitted by Randy Haugen on Fri, 06/12/2015 - 15:50

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Wondering what the New Brunswick weather will be like this winter??? hehehe

Submitted by stinker373@hot… on Sat, 06/13/2015 - 20:40

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so your saying it's going to be another bad ski season in North Idaho??? Guess I shouldn't buy a seasons pass?!?!

Submitted by Bucky on Sun, 06/14/2015 - 12:36

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Consideran que la Costa Caribe Colombiana, al norte de Sudamérica, tendrá impactos desfavorables en este proceso?

Submitted by laura castro on Sun, 06/14/2015 - 18:20

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It would be very interesting to see a detailed analysis of how historical ONI values and El Nino/La Nina episodes compare when using SST anomalies computed from ERSSTv4 versus v3b. Other scientists at NOAA also seem to study SST using the "cold-biased" satellite-based data explicitly excluded from ERSST (see http://coralreefwatch.noaa.gov/satellite/sst.php for example). What do ONI values look like when computed from this data?

Submitted by Sam on Mon, 06/15/2015 - 08:48

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We won't be able to know precisely how the satellite data matches up until next year at the earliest when the 1986-2015 base period becomes available. The OISSTv2 record began in November 1981, and even though you could technically run ONI data on this dataset using a 1982-2010 or 2011 base period, this will yield slightly different ONI values from ERSSTv4 & v3b that are currently calculated against a 1981-2010 base period & at that point, you would be comparing apples-oranges. There are several other relatively independent SST reconstructions & sets that are available and ONI data could be derived from each, including Kaplan v1, Kaplan Extended v2, HADISST1, HADSST3, IOCADSv2.5, COBE SSTv2 (the COBE data has been extremely hard for me to get, I have to compute ~980,000 1x1 degree boxes in the NINO 3.4 region to get the monthly temps thru GrADS). The KNMI Climate Explorer is a great place to start.

Submitted by Eric J. Webb on Fri, 06/19/2015 - 09:12

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I have gotten to be a huge fan of this blog since I discovered it this last winter. Thank you. Is it my imagination, or did the upper and lower wind anomalies virtually disappear about when the the new monthly ENSO diagnostic report came out, which I think was quite close in time to this article? Looking at the big El Nino events, those strong wind anomalies were one characteristic that they had that the others did not-- even though the others seemed very strong at times except the wind anomalies. Am I off base? Did the wind anomalies pretty much die all of a sudden in the last week or so? What kind of effect will that cause if I am right? And, if I am wrong, have they picked back up or was I just misreading something? Thanks!

Submitted by Glenn Hall on Sat, 06/20/2015 - 00:58

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It was not your imagination! Starting a couple of weeks ago, the Madden-Julian Oscillation (MJO) was in the phase that gave increased convection (cloudiness and thunderstorm activity) over the Indian Ocean, and that is a phase that tends to militate against El Nino. You are correct that the wind anomalies in both lower and upper atmophere, that have been showing a clear El Nino pattern, weakened in response to this MJO factor. The Southern Oscillation Index (SOI) became much more weakly negative than it had been just a few weeks earlier. Fortunately (if you like El Nino), the much heavier flywheel of the sea temperatures, both at and below the surface, do not change very quickly, so this latest "gunshot" against the event will not make much of a dent and undo what has been building up over the last several months. Furthermore, the MJO is predicted to change phase in the next week or so, so as to be less unfavorable to the El Nino, and maybe even favorable to it. When the MJO phase is in the central or eastern tropical Pacific, it helps support (or even strengthen) an El Nino. The MJO can weaken or strengthen an El Nino (or La Nina) when it stays in the same phase for a long time, such as over 1 month. But that rarely happens, as the MJO tends to propagate around the globe every 30-60 days or so.

Congratulations on noticing this very relevant, and likely relatively brief, interruption to the atmospheric patterns defining this El Nino.

Submitted by anthony.barnston on Mon, 06/22/2015 - 18:32

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Looking at your last diagram, more rain in the California Central Valley is questionable, correct? I'd love to hear our farmers will be getting some rain, even though we also need that snow pack!

Submitted by Lorri Stellhorn on Sat, 06/20/2015 - 11:28

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You are correct that increased rainfall this winter in the Central Valley is questionable. The extended Pacific jet stream tends to bring increased rainfall to mainly southern California and the southwestern States (including snowpack as well as rainfall at lower elevations), so the San Juaquin Valley is in a better position to get good rainfall than the Sacramento Valley. Each event plays out differently, however, and we can't expect all events to bring the same patterns of rainfall departure from normal. I would say there is reason for hope for California this winter, especially late winter (Jan-Mar) with this developing El Nino that is already at moderate strength before mid-summer.

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As a hydrologist I am steeped in models based on past observations and predictions based on analogous years, etc. But climate change is forcing us to rethink our projections and those p values. My point is that while we have data and statistical methods Sir Gilbert Walker could not have dreamt of, we are also faced with trends our models, fancy as they are, would not have predicted a short 30 years ago. We don't have to look far to see manifestations of this - this winter's intrusions of the polar vortex deep into the central U.S., or the ongoing convective storm destruction wrought by converging air masses over mid-America. The jet stream is becoming both weaker and less organized. In large measure it was that weakness that brought us the polar vortex and those lingering storms and it is observed past tendencies of storm tracks driven by jet stream patterns that suggests that this el Nino will bring storms to southern CA. Bringing this uncertainty to the question of rainfall this winter in the Central Valley - leads to my favorite answer to the question - what to expect from perturbations of complex systems - surprise. I'm not suggesting your answer is wrong - there certainly is hope based on past experience - but I sure as hell would not bet the farm on it.

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I couldn't agree more that anlogues are no way to make a forecast, with or without climate change. We had a blog about this during the course of the last year: check out http://www.climate.gov/news-features/blogs/enso/why-past-enso-cases-are…; But anlaogues are interesting and are not completely worthless or irrelevant. Despite climate change, most scientists would agree that so far, even with the amount of climate change we have already had, the ENSO phenomenon has not changed materially and has not begun playing by very different rules. There have possibly been trends in certain details, such as a greater tendency toward central Pacific El Nino events, but these have not been marked. Regarding the tendency for southern California to get above normal rainfall in late winter with moderate-plus or strong El Nino events, it shows up not only in past cases (analogues) but is also confirmed in dynamical model experiments using the equations of the ocean and atmosphere. But if your point is that there is appreciable uncertainty in the forecast for late winter precipiation in California, hey, I'm 100% in agreement! We should be hopeful, but not get our hopes up too much.

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I am a hydrologist and recognize the value of using past events as analogies for likely future conditions. But as we all know, systems are changing, making predictions riskier than ever. Yes, we have computing power and statistical methods Sir Gilbert Walker could not have dreamed of - but we are also witnessing climate change at a rate faster than any in recorded history. Of particular interest (to me) is the weakening and disorganized polar jet stream. Much of last winter's record cold in the midwestern and northeastern U.S. was associated with the weakening polar jet. This suggests to me that using analogous years prior to this weakening is very risky. I don't have a better predictor for you than good old analogous years, but I suspect our predicted outcomes will be more wrong than usual this winter. BTW - there truly are el Nino effects right now - but they are mostly in the ocean where warm temperatures dominate the northern latitudes and species assemblages from southern latitudes are being found far from home.

Submitted by Rich Domingue on Wed, 06/24/2015 - 19:06

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Again, I agree that analogues should not be used as the sole source of a real-time forecast, unless there is nothing else available. There is considerable uncertainty associated with the winter forecast for precipitation in California, but the tilt of the odds toward good results in the southern part of the state nonetheless exists, due to the expected extension of the Pacific jet stream even in the presence of climate change that may well be altering the usual jet patterns farther east in the US during winter.

Submitted by anthony.barnston on Fri, 06/26/2015 - 20:48

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Is it likely that Northern Ca will get increased rain and snow if this El Niño event plays out as predicted? I know I have read mainly the southern part of the state gets higher rainfall, but I remember the '82/'83 event and especially the '97/'98 event, and NorCal had greatly increased rainfall and I believe snow as well. Are we going to get some relief up our way too? It drives me crazy that whenever the state's drought situation and possible solutions to it, as well as El Niño, climate change, etc.... are discussed---only southern Ca is mentioned, as if the northern half of the state does not exist!!! Especially in light of the fact that we are having to send huge amounts of our water to the south and it is looking likely that we will have to be sending even more, it would be appreciated if more feedback and info for the northern half ( as well as research and positive ACTION on solutions for us!) --could be focused on as well!!

Submitted by Nancy on Fri, 06/26/2015 - 13:55

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In the strongest El Nino events, northern as well as southern Calif have received above average precipitation. In moderate El Nino events, central California may get good rains, but north of San Francisco the odds are not so good. The reason northern California is often left out of the forecast, is because it is in a transition zone between the region farther south that has the enhanced chance for above average precipitation (especially in late winter), and the region farther north (Oregon and Washington) that tend to be a bit drier than average during winter with El Nino. We're sorry, but that is what mother nature does, ON AVERAGE. In any particular case, it may or may not turn out this way, but over a large set of El Nino cases that is the tendency, based not only on empirical evidence (historical observations) but on dynamical (i.e. physical) modeling results where physical equations are used. As far as how strong the current El Nino may become by winter, it is somewhat up for grabs. At least a moderate event appears likely, but whether it will grow to become one of the very strong ones is unable to be resolved at this time. If it does become strong (with Nino3.4 and Nino3 index values of 1.5 or even 2 degrees C above average), central California will be in a better position to get a wet winter, and even farther north in California would have a decent shot at it. With the decadal climate possibly shifted from what it was between 1999 and early 2014, California also might stop having as bad a long-term drought situation. But we are not sure the decadal climate has shifted (I'm talking about the Pacific Decadal Oscillation, or PDO), since it needs to stay shifted for at least 2 or 3 years to be sure it is not just a 1 to 2 year break in the general 15-or-so year tendency. In any case, we hope California in general will get some relief from the drought, both from the El Nino and possibly from a shift of the PDO to positive phase after 1 to 2 decades in mainly negative phase. A lot going on here and it will be interesting to see the outcome! 

Submitted by anthony.barnston on Fri, 06/26/2015 - 21:01

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We don't see any evidence that "the blob" (the warm sea surface temperatures in the Gulf of Alaska) will impact this El Nino.  

Submitted by michelle.lheureux on Thu, 07/09/2015 - 19:21

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There have been torrential rains in the part of the country east of SJ for the past 8 days, with much associated damage. Are these storms the result of El Nino?

Submitted by Barbara on Sat, 07/04/2015 - 04:24

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During El Nino, the large scale pattern favors drier than average conditions over Central America and the Caribbean.  However, typical El Nino impacts are usually best seen in "seasonal" or an average of 3 months of data.  What you are pointing out appears to have been a significant, shorter-term weather event.  

Over the last 30 day average, here is the broader larger scale patttern as estimated by TRMM  (as of this posting, the dates are shown from June 9-July 8th 2015):

http://www.cpc.ncep.noaa.gov/products/fews/central_america/trmm_rainfal…

From this snap shot, most of the larger region is drier than average (i.e. consistent with El Nino).  But over Costa Rica, I see a wetter than average signal, which appaers to be mostly the exception rather than the rule.  

Overall, it is importat to realize that an El Nino does not guarantee impacts and there will be exceptions even during a stronger El Nino.  

 

Submitted by michelle.lheureux on Thu, 07/09/2015 - 19:35

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It appears the NOAA is lagging behind the Japanese Meteorology Association (JMA) since the JMA declared an El Niño during the summer of 2014. JMA is also forecasting possible historic El Niño conditions later this year. In light of this news, should the NOAA return to ERSSTv3b (without the high frequency filter) since it appears to have been a better indicator of El Niño conditions than the current ERSSTv4? Or should the NOAA expand the 3.4 zone under the current ERSSTv4? The new v4 dataset show a four month period of 0° C variation during the summer of 2014. How odd it would be if this is indeed the largest recorded El Niño, and one which the NOAA never saw coming. JMA El Nino Index: http://ds.data.jma.go.jp/tcc/tcc/products/elnino/elmonout.html#fig1 JMA El Nino Forecast: http://ds.data.jma.go.jp/tcc/tcc/products/elnino/elmonout.html#fig9 ERSSTv3b: http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears_ERSSTv3b.shtm ERSSTv4: http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears.shtmll

Submitted by Luke on Sat, 07/11/2015 - 16:59

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Are you aware of a past archive for JMA forecasts/outlooks? I’ve looked for it before on the web and wasn’t able to find it. Therefore, it’s hard to compare forecasts with JMA so I can’t answer that part of your question... CPC has an archive of past outlooks here:

http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/enso_advisory… (click "Archive" link).

NOAA CPC/IRI declared El Nino in March 2015. It is our opinion that this is the start of El Nino irrespective of the ERSST dataset. This is because we do not declare ENSO events -- from month-to-month -- on the basis of a single index (or dataset) that is SST only (covered here: http://www.climate.gov/news-features/blogs/enso/why-are-there-so-many-e… and here: http://www.climate.gov/news-features/blogs/enso/decembers-enso-update-c…)

The Oceanic Nino Index (based on ERSST) is only one index to monitor ENSO and it is an simple way of classifying historical events and drawing comparisons. However, please always keep in mind that no index (or single dataset) is foolproof and ENSO is a *coupled* (meaning ocean + atmosphere) phenomenon, so for the weaker/borderline events in particular, we think it is important to consider other ENSO indices in addition to the SST based ones. In late 2014, we did not see a clear atmospheric response, so we did not declare an El Nino (http://www.climate.gov/news-features/blogs/enso/do-recent-global-precip…).

Since March 2015, we have seen both the tropical ocean and atmospheric indices aligned and more clearly exhibiting coupled behavior, which is why we have been calling it an El Nino. Also, our forecast probabilities for El Nino were fairly elevated (40-50%) prior to March (Feb forecast: http://iri.columbia.edu/our-expertise/climate/forecasts/enso/2015-Febru…), so we don't think it's accurate to say we never saw it coming.

A final (more minor point), recent values of the ONI will continue to change when the climatology changes. ONI values for 2014-15 will change slightly until the climatology becomes fixed in the year ~2030. More details here: http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ONI…

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