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September 10, 2020 NOAA Declares La Nina Conditions In Place

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9월 6, 2021
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Written by Sig Silber

NOAA updates the status of ENSO on the second Thursday of each month. This presumably plays a role in the issuance of the Seasonal Outlook which is issued on the following Thursday. We thought the status should have been updated to La Nina Advisory last month but it was a close call and this month they took the leap. There is not a huge difference between a weak La Nina and ENSO Neutral with a strong bias towards being La Nina. So this is not a major event but it solidifies the forecast to some extent. It also reminds us that La Nina is favorable for hurricane development in the Atlantic.

La Nina Advisory


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ENSO Report September 10, 2020

Later we provide excerpts from the ENSO Blog report by Emily Becker and it may be easier to follow than the above.

So it looks like the next two seasons: Autumn and Winter will reflect a weak La Nina.

This shows the new Meteorologist survey compared to the model results mid-month in August (August 19). It indicated La Nina then but much more strongly now.

Some useful information from the NOAA ENSO Blog. You can find this article here.

We have seen this flowchart before but it summarizes the situation well. The next graphic contains text that is a direct quote from the Emily Becker blog post.

This may be a better NINO 3.4 forecast than the IRI-CDC forecast that NOAA seems to rely on. It is hard to say but Emily Becker is not in the dark so this probably is useful information. A big question is the impact of deepening versus reversal from the highest negative reading of the NINO 3.4 Index on weather. Some believe it is a combination of the value and the trend (slope or first derivative).

Now I am deviating from Emily Beckers’s presentation to show the forecast from the Australian Bureau of Meteorology (BOM). It is about ten days old issued in late August.

BOM shows a shorter La Nina. I do not have the latest forecast from JAMSTEC but it also showed a shorter La Nina last month.

NOAA has their own proprietary model which they rarely use. It is not exactly clear why they shun their own model.

CFSv2 spread and bias correct ENSO forecast

This model is right in line with the NMME.
In most cases, I freeze the models as of the date of publication but for this one, I am going to just let the above model run so if you refer to the article in the future, the values in the above may not relate well to the discussion. But I am doing that so if you refer to this article in say two weeks, you will see if there has been any change in the forecast from this model.

I am going to introduce another graphic which is the current view of the subsurface along the Equator.

This is static but without showing the earlier views I can tell you that the warm anomaly is undercutting the cool anomaly. So the issue is when will it displace the cool anomaly. Not an easy question to answer but you can see the issue. Back to Emily Becker now. It is a quote but not shown as a quote because I turned it into an image

Generalized World Impact

For the World, La Nina tends to be wet, not dry.

North America Impact

It is not a surprise that the Jet Stream is the dividing line between cold and not so cold. The Jet Stream is farther north than usual.

Here is another way to look at it.

Here are three generalized graphics of the Walker Circulation during the various phases of ENSO. Generalized or idealized is the keyword as there is a lot of variability from one event to the next but it provides a good framework for discussion. I have presented these or similar graphics many times before. These were produced by Fiona Martin.

Walker Circulation - ENSO Neutral

It is all about where the is evaporation and convection in the Pacific. Convection is enhanced where the water at the surface is warm. The pattern of air rising and forming clouds and sinking and drying out is called the Walker Circulation which was mentioned earlier. In ENSO Neutral this is the general pattern.

https://www.climate.gov/sites/default/files/Walker_ElNino_2colorSSTA_large.jpg

With El Nino the two thick arrows are important. Notice there is rising air west of CONUS. It is not restricted to just near the Equator. On the other hand, the Maritime Continent is less wet than usual.

https://www.climate.gov/sites/default/files/Walker_LaNina_2colorSSTA_large.jpg

With La Nina, the warm water is pushed to the west so that is where there is the most convection. Offshore of CONUS there is a tendency for air to sink and dry out.

To summarize, the Maritime Continent is north of Australia. And you can see that during La Nina, with the Indo-pacific Warm Pool strong, there is a lot of convection there. With ENSO Neutral there is less; and with El Nino it reverses. Prior to the satellite imagery, the Southern Oscillation Index (SOI) was used to estimate the relative strength of this process between Darwin Australia and Tahiti.

B. Conclusion

NOAA says we are in La Nina Conditions and were in August which they have denied until today. I have a little problem with NOAA re being late to the party on some occasions. I wonder why.

C. How significant is a pronouncement of the state of ENSO.

What we are going to do now is look at all the historical La Ninas (their winter effects only) and while we are at it (since I found a good source of information, we are going to also look at all the historical El Nino’s. I might be missing one as this data source in one case goes up to 2017 and in another case goes up to 2018 and early next year the normals for the Equator will be updated and some weak El Nino’s and La Nina’s may drop off the list and some others may be added. But those adjustments do not diminish the value of what I will present now.

The purpose is to introduce the reader to the concept of the statistical average. Generally speaking the statistical average La Nina and the statistical average El Nino are used to make forecasts. NOAA adjusts for the predicted strength of the La Nina or El Nino. JAMSTEC does the same but also adjusts for the Modokishness of the El Nino and also to a lesser extent the La Nina. NOAA will not admit to doing that.

In all cases, everyone is hampered by the small number of events in the historical record. Statistics is based on having a large number of events. You will see why that is important now.

NOAA provides the tools to create graphic displays like below. In theory, I could do that myself. But like most things involving software those who work with it frequently learn how to use it. So I am happy to find these graphics. The reference provided is where I found the graphic. In some cases that person produced it. In other cases, they got it from someone else and provide attribution. In all cases, they provide a discussion that assists with understanding what is being shown.

It is important to understand what the importance of the state of ENSO is. It probably is the most important factor in forecasts other than possibly decadal trends in temperature. The stronger the event (the deviation of the NINO 3.4 value from 0, the more significant we would expect the impacts to be. In the current case, we are expecting a pretty weak La Nina.

First, we look at La Nina

Temperature Record. Source and a discussion: Tom Di Liberto

They are shown from top to bottom and with rows from left to right from the strongest to the weakest. There is a lot of variation.

Precipitation Record Source and a discussion: Tom Di Liberto

La Nina winter precipitation

It is organized in the same way

Now even though it does not apply right now we will look at El Nino….mostly for my benefit so I can find these graphics when I will need them.

Temperature Record Source and a discussion: Rebecca Lindsey

El Nino Precipitation History

Precipitation Record. Source: Rebecca Lindsey

I have done additional analysis on this information with respect to New Mexico in terms of how the state of the AMO and PDO might impact the results but I am not going to present that now for a number of reasons include we are in a La Nina not an El Nino.

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