If only that were true. Unfortunately, we
anticipate that global temperature will rise steeply, well above the
trend line – not that we would be happy to stay on the trend line. How
steeply global temperature rises depends in part on hard-to-predict
ENSO. Columbia University’s International Research Institute for Climate
and Society (IRI) collects and distributes model predictions monthly, which are also made available by the Climate Prediction Center
of NOAA’s National Center for Environmental Prediction. The full range
of Niño predictions by climate models (Fig. 1) extends from a strong La
Niña to a Super El Niño, but, except for those two extreme cases, most
of the other 22 models yield Niño-neutral conditions continuing into
late 2022. One of the models (included in Fig. 1) just touches the
+0.5°C Niño3.4 temperature that separates Niño-neutral from El Niño,
while three models go below –0.5°C into La Niña territory.
In our temperature update last month,[3] we
speculated that an El Niño could begin later in 2022, and, if so, 2023
was likely to be the warmest year in the instrumental record. We expect
that even a little futz of an El Niño, such as the one in 2019 (Fig. 1),
would produce record temperatures, because Earth is now substantially
out of energy balance. Here we first comment on why we think that an El
Niño is possible, then note how irregular and difficult to predict Niño
variations are, and finally suggest a diagnostic that tracks
acceleration of global warming independent of ENSO.
Global temperature anomalies relative to the trend line are compared in
Fig. 3 with anomalies of Niño3.4 temperature and anomalies of
temperature in the upper 300 meters of ocean in the Niño region.
Correlations of both Niño3.4 and the upper 300 meters with global
temperature are significant (almost 60%), but the upper 300m provides a
more useful indicator because it precedes global temperature change by 9
months.
As arm chair observers of Niño data, we noted that the temperature of
the upper 300 meters of ocean in the equatorial Pacific is now rising
rapidly in connection with an eastward propagating Kelvin wave that will
reach the coast of South America in March. If this results in
sufficient warming of the ocean surface near South America, it would
work in the sense needed to help support the Bjerknes feedback – warming
in the east tends to affect atmospheric pressure so as to reduce the
strength of the prevailing easterly winds, thus helping warmer surface
water in the western Pacific to slosh back toward South America, as
required for an El Niño. That’s not enough though. Kelvin waves
seemingly propagating a warm anomaly toward South America are common.
Most of them don’t kick off an El Niño. Conditions need to be right and
the fickle, changeable zonal winds need to provide a kick-in-the-pants –
westerly wind anomalies pushing warm surface water toward South
America. Good timing of Madden-Julian Oscillation (MJO) activity
(eastward propagating 30-60 day weather variability in the tropical
atmosphere) can help. So, Niño developments are noisy and hard to
predict.
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