[Sea surface temperatures around the equator in the central and eastern Pacific were mostly cooler than average (blue) in July 2022. A few warm pockets (orange) dotted the far eastern Pacific. NOAA Climate map from our Data Snapshots collection.
[From NOAA Climate written by Emily Becker
] La Niña continues! It’s likely that the La Niña three-peat
will happen: the chance that the current La Niña will last through early winter is over 70%.
If it happens, this will be only the third time with three La Niña winters in a row in our 73-year record
. ENSO (El Niño/Southern Oscillation, the whole La Niña and El Niño system) has the greatest influence on weather and climate
during the Northern Hemisphere cold season, so forecasters pay especially close attention when it looks like ENSO will be active in the winter.
Hopelessly Devoted to You
La Niña is present
when the sea surface temperature in the east-central Pacific Ocean is at least 0.5 °C (0.9 °F) cooler than the long-term average, along with evidence of a stronger atmospheric circulation above the equatorial Pacific. In July, the sea surface temperature in the Niño-3.4 region of the tropical Pacific, our primary monitoring region, was 0.7 °C cooler than average (average = 1991–2020) according to the ERSSTv5
dataset. This makes 21 of the past 24 months
with a deviation from average below -0.5 °C.
[Three-year history of sea surface temperatures in the Niño-3.4 region of the tropical Pacific for the 8 existing double-dip La Niña events (gray lines) and the current event (purple line). Of all the previous 7 events, 2 went on to La Niña in their third year (below the blue dashed line), 2 went on to be at or near El Niño levels (above the red dashed line) and three were neutral. Graph is based on monthly Niño-3.4 index data from CPC using ERSSTv5. Created by Michelle L’Heureux.
We Go Together
The average circulation of the atmosphere over the tropical Pacific—called the Walker circulation—makes a giant loop: rain and rising air over the very warm waters of the far western Pacific and Indonesia, west-to-east winds at high altitudes, descending air and drier conditions over the relatively cooler central/eastern Pacific, and the east-to-west trade winds near the surface. La Niña’s cooler-than-average central/eastern Pacific acts to strengthen this circulation, with more rain than average over Indonesia, less rain over the central tropical Pacific, and stronger upper-level and lower-level winds. In turn, those stronger low-level trade winds cool the surface further, and help to keep warm water piled up in the far western Pacific.
[Generalized Walker Circulation (December-February) anomaly during La Niña events, overlaid on map of average sea surface temperature anomalies. Anomalous ocean cooling (blue-green) in the central and eastern Pacific Ocean and warming over the western Pacific Ocean enhance the rising branch of the Walker circulation over the Maritime Continent and the sinking branch over the eastern Pacific Ocean. Enhanced rising motion is also observed over northern South America, while anomalous sinking motion is found over eastern Africa. NOAA Climate drawing by Fiona Martin
July recorded all the expected strengthened Walker circulation features, including substantially stronger-than-average trade winds. The trade winds led to the cooler-than-average surface temperature strengthening over the month, a tendency we can see in the weekly measurements
, which started July at -0.5 °C and ended at -1.0 °C. While the weekly anomaly is useful for monitoring current conditions, ENSO is a seasonal phenomenon, so conditions must remain for several months to qualify, and to affect global weather patterns. Michelle gets into this in more detail in her internet-ancient—but still entirely relevant—post
Rock ‘n Roll Is Here to Stay
Another outcome of the stronger trade winds during July was the development of an upwelling Kelvin wave
, cooler-than-average water that travels west-to-east under the surface of the equatorial Pacific. As the trade winds drag the surface waters westward, cooler water is drawn up from the deeper ocean.
[Difference from average temperature in the top 300 meters (~984 feet) of the tropical Pacific between June 7 and August 1, 2022. A deep pool of cooler-than-average water (blue) spread eastward and will continue rising to the surface in coming months, feeding the current La Niña. Animation by NOAA Climate, based on data from NOAA Climate Prediction Center.
This upwelling Kelvin wave will provide a source of cooler water to the surface over the next couple of months, which in turn provides increased confidence to the short-term La Niña forecast. With most of our computer models
predicting La Niña will last into the winter, forecaster probabilities are fairly confident through December–February.
[NOAA Climate Prediction Center forecast for each of the three possible ENSO categories for the next 8 overlapping 3-month seasons. Blue bars show the chances of La Niña, gray bars the chances for neutral, and red bars the chances for El Niño. Graph by Michelle L'Heureux.
Several models are predicting that La Niña will transition to neutral in January–March, and the forecast team provides even chances (47%) for either outcome (La Niña or neutral). It would be pretty rare for the event to terminate so early in the year. If La Niña does decay to neutral in January–March 2023, it would be only the 4th
time in the 24 La Niña winters we have on record
As I mentioned up above, La Niña’s greatest influence on weather and climate is during the winter. Also, of course, La Niña can be conducive to an active Atlantic hurricane season
, something reflected in NOAA’s recent update to the outlook
During summer, local processes are more important for determining weather patterns, including the North American Monsoon
. This year, the Monsoon has contributed to some devastating floods, but also provided much-needed rain for the drought-stricken Southwest. I checked in with our consultants for the North American Monsoon post, Zack Guido and Mike Crimmins. They have an excellent podcast
with tons of fascinating detail about the Monsoon, so check it out if your interest is piqued!
[Rain and lightning over desert hills near Mesquite, Nevada, on August 30, 2021, during the summer monsoon. Photo by Flickr user John Getchel. Used under a Creative Commons license
Mike had this to say about this year’s Monsoon:
We just crossed through the typical middle of the season (early August), and the first half was really good for just about all of the Southwest. Over 80% of Arizona and New Mexico are observing near-average or better rainfall so far this season, and more than half of the region at above-average or better! The whole season started with some epic rains over New Mexico that helped end their record fire season, and the moisture and storms have kept coming ever since.
This year has been interesting and different from last year’s very wet monsoon. Last year we had great monsoon moisture and two unusual large upper-level low pressure systems bring several days of widespread rain in July and August of last year. We haven’t really had anything big like that this year, just sustained deep moisture and the occasional wiggle in the upper-level flow to help organize precipitation into lines of storms from time to time. It has felt a bit more like a solid, active season that hasn’t needed any special tricks to stack up the precipitation totals across the region.
The relationship between La Niña and the Monsoon is not strong , but I asked Mike if he could speculate a little. He had this to say:
I am not sure of the influence of La Niña this year, but it certainly could be there. Some research on ENSO and the monsoon suggest that La Nña is correlated with an early start to the season in Arizona and New Mexico and wetter-than-average conditions through July. The signal then decays through August. This season follows that pattern, but I’m not sure of the causal links.
[July–August rainfall anomaly averaged over North American Monsoon region for every year 1950–2019 (y-axis) versus Niño-3.4 index (x-axis). Wetter-than-average monsoons (green dots) are slightly more common during La Niña years, while drier-than-average monsoons (brown dots) are slightly more common during El Niño years. Monsoon region averaged over all land gridpoints, 20°N–37°N, 102°W–115°W. Data from Global Precipitation Climatology Centre (GPCC) and ERSSTv5. Figure by Emily Becker
You’re the One That I Want
The Monsoon has helped with the Southwest drought, something discussed in the recent August climate outlook
. However, La Niña often contributes to dry winters through the West
, so we’re far from out of the woods, drought-wise.
Edited for WeatherNation by Mace Michaels