Reliable, official numbers now in for February 2016 show that it smashed the previous record for the month
What is the significance of reaching this new milestone? And now that El Ni単o is waning, what might the future bring?

Pattern of temperature anomalies across the globe in February 2016. The month was the warmest on record. (Source: NASA GISS)
| Please see important correction at end |
Earlier this month, aspate of headlines proclaimed that February 2016 was the warmest such month on record for the globe. At that time,I wrote that we should wait until official, reliable analyses were in before drawing any final conclusions.
The first of those reliable analyses has just been released, and it shows that this past monthdid indeed set a new record forwarmest February in arecord extendingback to 1880.
According to the analysis by NASA’s Goddard Institute for Space Studies, this past month was 1.35 degrees C (2.43 F) warmer than the month’s long-term average (measured between1951and1980).
February’s spike was not just a one-off. January also set a record. In fact, we’ve now experienced a string of five record-setting months in a row.
But the increase temperature anomalyspike seen lastmonth was particularly steep.As Gavin Schmidt, head of NASA GISS, put it on Twitter today: “Normally I don’t comment on individual months (too much weather, not enough climate), but last month was special.”
According to Gerald Meehl, a research scientist at the National Center for Atmospheric Research, the oddsof monthly records being set are raisedright now, thanks to “the juxtaposition of a large El Ni単o and ongoing human-caused warming.”
A spike ofEl Ni単o warmth has, in fact, occurredatop the long-term global warming trend-line. But as the string of recent monthly records suggests, that trend line also seems to beangling sharply upward now, after what many climate scientists regard as a multi-year period of slower warming.
But Meehlalso cautions that we should not expect each successive month necessarily to be warmer than the preceding one. That’s in part because El Ni単o’s fade as this one appears to be doing. And they often transition into La Ni単a, the opposite of an El Ni単o, resulting in cooling.
Moreover, climate can be quite labile, with natural variation causing lots of ups and downs.
What’s going on and what should we make of it?
Inanticipation of the release of NASA’sclimate analysis for February (a second one from NOAA will follow soon), I’ve been in touch with six scientists to get their perspectives on a number of issues, including these:
- What take-home messages should we draw from these monthly and annual analyses of global climate?
- Since climate is a phenomena measured in decades, should we be focusing so much on monthly records?
- Given just how warm things have been, what arethe relative influences of El Ni単o, other natural variations, and human-caused climate change?
- With El Ni単o now on the wane, and it’s opposite La Ni単a possibly on the way, what might the next couple of years bring?
Deke Arndt,Chiefof theMonitoring Branch of theNational Centers for Environmental Information at NOAA, emailed me today to makea philosophical point about these issues:
There’s nothing magical about a calendar year. It’s entirely a human construct, and an accident of history, that a year begins on January 1. We (myself included) really, really overdo the cook-off comparisons of one year versus another. It’s an easy, convenient, and not particularly harmful way to organize our thinking about climate change.
But the fact is, we’ve been setting a new “warmest 12 month stretch in recorded history” record almost every month for the past year. That’s the story, scientifically. We choose a January 1 starting line because that’s when we reset the annual accounting of our lives. But it’s not that important, scientifically.
This graphic helps us see the pattern of change through an ironically beautiful pattern of colors:

Global temperatures visualized month-by-month since 1901. Each square iscolored to indicate how it varied from the long-term average for that month. The extraordinary warmth of February 2016 required the addition of a new color to the palette. (Source: Makiko Sato, Columbia University)
We’re clearly in the midst of a particularly warm stretch of months, thanks in large measure to human-caused climate change. But there are other important influences to consider as well,since they will also help determine what we’ll experience in the months, years and decades ahead.
To get a better handle on these issues, I posed some questions in an email to NCAR’sJerry Meehl. Hestudies El Ni単oand La Ni単a, human and natural influences on climate, and possible future changes in weather and climate extremes in a warmer world. Here’s what Meehl said in an email message:
. . . ‘global warming’ is not a relentless march towards warmer temperature with every month and season and year and decade being warmer than the preceding month and season and decade. That is because there is a lot of internally generated, naturally occurring variability in the climate system. This natural variability is superimposed on the response to human-caused warming.
Keep that in mindif you find yourself reading stories saying things like “global warming has gone into overdrive” (as this story did). Yes, the average temperature of the globe is climbing more steeply now than it has in recent years. And a spike of El Ni単o warmth has been superimposed on that.
But sooner or later, we’ll come off the extreme highs we’re seeing, and we could even experiencea temporary period of slower warming lasting years. This won’t repeal the long-term upward rise in global temperature not by a long shot. But when temperatures do cool off for a bit, peoplemight be left wondering whatever happened to global warming going into overdrive and crossing terrifying thresholds.
The graph above shows how temperatures have varied from the long-term averagefrom 1970 to the present. I’ve marked the two strongest El Ni単os during the period: in 1997/1998, and our current episode.
I’ve also indicated the period when warming of the Earth appears to have slowed despite all the greenhouse gases we humans emitted into the atmosphere.
In addition to these variations, you’ll also note lots of smaller ups and downs. But the long-term upward trend is clear.
Wiggles and squiggles
To understand these wiggles and squiggles better,along with the underlying trend, I spoke with John C. Fyfe, Senior Research Scientist with Environment and Climate Change Canada. Fyfe uses model simulations and observations to studyclimate variability and climate change.
The variation takes place across several scales, he said. First, there is the multi-decadal scale, which stretches across two or more decades. Thats the scale on which humans are causing long-term warming of the planet.
Thereis also a timescale between multi-decadal and annual. Jerry Meehl,who co-authored a paper on the global warming slow-down with Fyfe and other researchers, described it this way:
. . . it’s possible to have 15-year periods when the rate of global surface temperature increase slows compared to a previous 15-year period. Conversely, there can be a 15-year period when there is a more rapid rate of global surface temperature increase compared to a previous 15 year period.
El Ni単o and La Ni単a are phenomena that take place over the third timescale the annual one. They typically last two years, give or take.
Inthe graph above, note how the size of the warming spike in the 1997/1998 El Ni単o is roughly the same size as the spike right now. This isn’t surprising, since both El Ni単o episodes are probably in a tie for the strongest on record.
“El Ni単o events do cause an increase in the global mean temperature, usually within about a three-to seven- month lag,” says Anthony Barnston, a climate and ENSO forecaster with the International Research Institute for Climate and Society at Columbia University.
Follow the heat
The current El Ni単o peaked in November three months ago. So we are just now experiencing the strongest effects on global average temperature.
Thewarming occurs because a huge amount of heat energy pours out of the tropical Pacific ocean and into the atmosphereduring an El Ni単o. Most of it is not the result of human activities, according to Barnston.
But why the lag? As NOAA’s Deke Arndt puts it, “The reason the ‘back end’ of El Ni単os are often warmer is that the cumulative effect piles up during the course of the event.”
So right now, we’re experiencing the pile-up of El Ni単o heat energy.
But have a look at the graph again. Even though the El Ni単o spike in 1997/1998 is about as bigin magnitude as what we’re experiencing now, global temperatures todayare way higher. That’s because in all the years since 1998, long-term, human-induced warming has raised the baseline on which this year’s El Ni単o spike is built.
Bending the curve
There are also more than just El Ni単o spikes represented in that graph. There are also downwardLa Ni単a spikes as well. (Not all of the downward fluctuations are La Ni単a’s though.) Put enough of them together, and you’llbend the long-term trend down a bit, causing a slowing in globalwarming.
Fyfe believes thatmay have been a major contributor to the slower rate of warming noted in the graph above. (But keep in mind that there is a good deal of scientific debate over the slowdown.)
He alsosays it’s quite possible that we’re now coming out of it.In fact, we could be at the outset of a new trend.The future, Fyfe said, may bring fewer La Ni単asand more El Ni単os. “That may be where were heading with this recent superEl Ni単o.”Butit’s too soon to tell.
Amidst all these variations on different timescales, Fyfe emphasizes that“one thing is almost fixed: the long term, human-caused warming.It is unequivocal, and it will carry on into the future. All these wiggles are simply superimposed on it.”
Whither El Ni単o?
El Ni単o is expected to transition to neutral conditions by late spring in the Northern Hemisphere. Moreover, there’s a 50/50 chance that a La Ni単a could take hold in the fall.
At NOAA’s ENSO blog, Emily Becker notedthis recently:
La Ni単a conditions have followed six of the ten moderate and strong El Ni単os since 1950, including two of the three previous strongest El Ni単os. However, this small number of cases means that its hard to make a very confident forecast based only on the previous events.
If a strong La Ni単a does ensue, “It would make it likely that 2017 will average cooler than 2015,” said Columbia University’s Anthony Barnston.
But what aboutthe rest of this year? Have El Ni単o plusstrong human-caused warming combined to make it a “shoo-in” for warmest year on record, as one blogger put it recently?
That claim “is an unwarranted extreme statement,” says Kevin Trenberth, a colleague of Meehl’s at NCAR. That’s because there are major uncertainties this far out. Moreover,with El Ni単o on the wane,heat is starting to betaken up by the oceans. Thissuggests 2016 could well turn out to be cooler than last year, Trenberth argues.
Deke Arndt of NOAA has a different perspective:
If my wife asked me if I thought 2016 was going to be the warmest year, I’d say ‘yes’ pretty confidently. However, as a public servant and as a scientist, we’re a pretty conservative lot, and I don’t think we’d say that until we were 100 percent sure. For reference, we started expressing confidence in 2015’s first place status in late summer.
Two things are for sure. The firstis that we will soon find out!
The secondis this, from Jerry Meehl:
Human-caused warming due to increasing greenhouse gasescan best be seen over the long term so that the internal variations average out, leaving the more steady increase of global temperatures over those longer time scales.
Keep that in mind when a cool spell inevitably kicks in, and you then hear people questioning long-term global warming.
| Correction:An earlier version of this story said February was the warmest month of all months on record. That was incorrect. It was the warmest February in records that go back to 1880.|
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