Research on Earth’s Raging Heat of 2023-24 Is Picking Up

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Yves here. The generally scary heat levels of this year are set to abate a bit. But a break in trends should not be mistaken for much of a change in trajectory.

By Bob Henson, a meteorologist and journalist based in Boulder, Colorado. He has written on weather and climate for the National Center for Atmospheric Research, Weather Underground, and many freelance venues. Bob is the author of “The Thinking Person’s Guide to Climate Change” and of “The Rough Guide to Climate Change,” a forerunner to it, and of “Weather on the Air: A History of Broadcast Meteorology”, and coauthor of the introductory textbook “Meteorology Today”. For five years and until the summer of 2020 he co-produced the Category 6 news site for Weather Underground. Originally published at Yale Climate Connections

f you’ve got a chronic health concern and you suddenly get acutely sick, you and your doctors face two big issues: what’s behind your short-term crisis, and what are the implications for your longer-term health?

Our world’s “planet doctors” have been at a similar stress point for close to a year now. They’ve been scrambling to figure out why Earth’s surface – including both atmosphere and oceans – got hit with an unprecedented spike of heat that’s run from mid-2023 well into 2024. They’ve also been addressing what, if anything, the spike tells us about the next few years and beyond.

Several fresh papers are out on two unique and much-publicized factors that may have influenced the astounding global heat of 2023-24. There’s much more coming down the research pike: for example, five journals within the Nature umbrella are joining forces for a special cross-journal issue that will focus on the spike. As the submission invitationput it, “It is not yet clear what caused the various climatic anomalies in 2023, but the answers will shape our understanding of what is to come – whether 2023 was a singular outlier year, or if it is a new baseline from which warming will continue to new levels.”

The planet’s immediate fever hasn’t yet broken. Looking at the global-scale averages calculated daily by the Copernicus Climate Change Service, surface air temperatures have set records on dozens of dates since mid-2023, and sea surface temperatures have set records each day for more than a solid year (see Figures 1 and 2 below).

Figure 1. Globally averaged daily surface air temperature from 1940 through June 2, 2024. Record global highs were set on nearly every date in the second half of 2023 and on many days in the first half of 2024. (Image credit: Copernicus Climate Change Service).
Figure 2. Globally averaged sea surface temperature (SST) from 1940 through June 2, 2024. Every date since May 4, 2023, has set a new global record for that date, and on March 20 and 21, 2024, the global SST average set the current all-time record high of 21.09°C. (Image credit: Copernicus Climate Change Service).

As catalogued here in monthly posts by Jeff Masters, every month since June 2023 has been the warmest globally in observations and analyses going back to 1850. This month NOAA and NASA will likely concur with the Copernicus Climate Change Service that May 2024 set yet another global monthly heat record.

In a special address on Wednesday (World Environment Day) titled “A Moment of Truth”, UN Secretary General António Guterres referred to the latest Copernicus data as well as a new report from the World Meteorological Organization. The WMO gave a 47% chance that the period 2024-2028 will average at least 1.5°C above preindustrial levels, and an 86% chance that at least one year in that period will set a new yearly global record, beating out 2023.


In April alone, 34 locations set all-time monthly highs for their respective nations and territories. And in May and early June, many populous tropical and subtropical locations from India to southeast Asia to Mexico have endured miserable, dangerous heat at or or near all-time records.

Even satellite-based lower-atmosphere temperature data – long used as ammunition by those who would dismiss or deny long-term warming – haven’t escaped the intense spike.


The handwriting does appear to be on the wall for the demise of the 2023-24 heat spike, mainly because the Pacific is rapidly transitioning toward La Niña. The upwelling caused by La Niña typically brings immense volumes of deeper, cooler water to the surface of the eastern tropical Pacific, spanning an area that can sprawl larger than the United States. We can expect that cool infusion to bring down globally averaged air and ocean temperatures by a few tenths of a degree Fahrenheit for at least a few months. That should be enough to end the current string of daily global records and near-records, perhaps as soon as July.

It may take a lot longer to fully understand what’s happened in the last year, and what it may portend for our future.

Ships, Smokestacks, and Sunlight

It should go without saying that the 2023-24 heat spike arose on top of relentless long-term warming, caused by the greenhouse gases pumped out as fossil fuels get burned. Global temperatures simply couldn’t have hit such a peak without a century-plus of global heating bolstering the spike.

The next biggest factor was the El Niño event of 2023-24, the strongest since 2015-16 and one of the two strongest of the 21st century thus far. In contrast to La Niña, the oceanic warmth slathered across the eastern tropical Pacific by El Niño typically raises global surface air temperature by several tenths of a degree Fahrenheit.

In fact, Michael Mann (University of Pennsylvania) and others have argued that much like the El Niño heat peak of 2015-16, the 2023-24 values fall within the margin of natural variability around the longer-term warming trend.

Still, there was a hefty difference of around 0.24 degree Celsius or 0.43 degrees Fahrenheit between the 2015-16 and 2023-24 peaks (based on May-to-April data from NOAA, as shown in Fig. 3 below). And questions remain: exactly how did natural variability, and/or something more, manage to produce such a jump from one strong El Niño event to the next? And why was September 2023 in particular such a record-destroyer?

It’s when you drill down past long-term warming and El Niño that the science saga gets more intriguing and more contentious.

Figure 3. Global surface temperatures (land and ocean), averaged for 12-month periods from May through April. The 2023-24 period was 0.24°C (0.43°F) warmer than 2015-16, compared to a long-term warming trend (1974-2024) of 0.15°C (0.27°F) when carried across the same eight-year period. (Image credit: Annotated from original via NOAA/NCEI)

One of the often-cited secondary factors at work is a sharp drop in the sulfate aerosol emissions spewed out from global shipping. That decline was triggered by regulations put into effect by the International Maritime Organization in 2020. They reduced sulfate emissions from shipping by some 70% and global sulfate emissions by roughly 10%.

The direct effect – fewer sun-blocking aerosols and thus more sunlight reaching Earth’s surface – is fairly straightforward. Changes in sulfates also have indirect effects: the presence of aerosols can shift the numbers and size distribution of cloud droplets, which in turn affects how much sunlight reaches Earth’s surface.

Taking both processes into account, a 2023 analysis by Carbon Brief estimated that global temperatures will be about 0.05 degrees Celsius warmer than otherwise expected by 2050 as a result of the 2020 sulfate emission cuts – in effect, speeding up global warming by about two years.

That may seem like a mere drop in the climate-change bucket. But the influx of energy has been greatest along oceanic shipping lanes – including, importantly, those across the North Atlantic, the spawning ground for U.S. Gulf and Atlantic hurricanes. Sea surface temperatures across the North Atlantic have been smashing records over most of the past year. They’re now at unprecedented heights for the start of hurricane season, as discussed here by Michael Lowry in a May 22 post.


A new paper in Communications Earth and Environment led by Tianle Yuan (GESTAR-II/University of Maryland) estimates that the increased solar input from the drop in sulfates – which the paper calls an “inadvertent geoengineering termination shock” – could lead to a doubled rate of global warming in the 2020s compared to the last half-century. The new energy balance estimates from the Yuan paper are roughly consistent with earlier studies, but there’s been some pushback on technical grounds in the paper’s extrapolation from energy balance to global temperature trends.

“This is a timely study, but it makes very bold statements about temperature changes and geoengineering which seem difficult to justify on the basis of the evidence,” said Dr. Laura Wilcox, associate professor at the UK’s National Centre for Atmospheric Science in the University of Reading, in a roundup of reactions at Science Media Centre.

Update (June 5): Another new paper – still in preprint form at EGUSphere, and not yet peer-reviewed – describes CESM ensemble simulations that incorporate a 90% drop in sulfate emissions from shipping in 2020, and produce a delayed global-warming spike in 2023 not unlike the one actually observed.


Figure 4. A view from the Himawari-8 satellite of the Hunga Tonga–Hunga Haʻapai volcanic eruption as it pushed above the Southwest Pacific at 0450 UTC on January 15, 2022. (Image credit: Japan Meteorological Agency, via Digital Typhoon and Wikimedia Commons)

What About That Undersea Volcano?

The eruption of the Hunga Tonga–Hunga Haʻapai volcano in the Southwest Pacific on January 15, 2022, grabbed the attention of vulcanologists and climate scientists worldwide. The eruption was the most powerful since that of Mount Pinatubo in the Philippines in 1991.

The immense blast from Pinatubo spewed enough sulfates into the stratosphere to bring down global temperatures by as much as 0.6 Celsius (1 degree Fahrenheit) over the next year-plus. The new wrinkle with the latest eruption: Hunga Tonga is located beneath the Southwest Pacific, rather than atop an island. The eruption ended up pushing less sulfur dioxide than Pinatubo into the atmosphere, but it added a massive infusion of water vapor, enough to boost the total amount of stratospheric moisture by as much as 10 percent. The added water vapor has since worked its way to higher latitudes within the stratosphere.

As with other greenhouse gases at high altitudes, the radiative effects of the water vapor added by Hunga Tonga have been to cool the stratosphere while slightly warming Earth’s surface. A couple of early estimates were that the eruption’s sulfates led to around 0.004°C of global cooling in 2022, and that the water vapor would lead to as much as 0.035°C of global warming over five years, perhaps accounting for a minor slice of the recent global heat spike.

A paper in review at ESS Open Archive led by Mark Schoeberl (Science and Technology Corporation) estimates that the net effect from both water vapor and sulfate aerosols from Hunga Tonga has actually been a tiny cooling of Earth’s surface, and that the combined radiative effects were nearly gone by the end of 2023. The study does not evaluate conditions above 35 km in the stratosphere, where water vapor remains roughly 10 to 20 percent more prevalent than before the eruption, as the effects on climate from water vapor at such high altitudes have been considered negligible.


Another recent paper, this one just published in the Journal of Climate, asserts that we could see a complex web of regional weather and climate effects for years to come as a result of Hunga Tonga’s water vapor. Led by Martin Jucker (University of New South Wales), the paper uses the WACCM global climate model, which incorporates stratospheric chemistry, to simulate a Hunga Tonga-like eruption and its impacts up to a decade out.

The study’s estimate of global warming from the added water vapor was a mere 0.015 degrees Celsius. What’s much more striking is a projected reshuffling of weather patterns over the latter half of the 2020s, apparently caused by interacting circulation changes and cloud feedbacks. If this new study’s projections end up on target, winter warming across the northern high latitudes (including the Arctic) and springtime warming across much of Eurasia could intensify, while Australian winters could be cooler and wetter than average, all else being equal. There are also hints of El Niño conditions being favored in the tropical Pacific.

Discussing these and other “surprising, lasting impacts” in an essay for The Conversation, Jucker added: “…we hope that our study will stir scientific interest to try and understand what such a large amount of water vapor in the stratosphere might mean for our climate.”

Yet another (but very minor) factor is the timing of the ongoing peak in the 11-year solar cycle. Variations in solar heat energy across the cycle are minimal (less than 1%) compared to the forcing from greenhouse gases, and the ups and downs of the cycle don’t affect our long-term warming trajectory. Still, the sun is now approaching the peak of Solar Cycle 25, spitting out active regions (and triggering a spectacular auroral display in May), so there may be a tiny, temporary dollop of extra solar energy in the mix right now. This cycle has been more active than predicted, even if it’s still among the weakest of the last 200 years.

The Main Headline Hasn’t Changed

For all the cool science it’s generating, the 2023-24 heat spike is first and foremost a danger sign. Even assuming that globally averaged air and sea temperatures manage to drop a bit below record levels for the next one to several years – something that’s quite possible, perhaps even likely – the spike has given us a preview of what might become “normal” as soon as the 2030s, as greenhouse gases from human activity continue to accumulate in the atmosphere. That accumulation will continue even when global emissions level out and begin to drop, as may happen over the next several years. Only when emissions drop to near zero will the accumulation cease.

Given how strange the spike has been, it’s wise not to assume too much about its demise just yet. One of the most ominous recent takes is from eminent NASA climate scientist James Hansen, who asserted with coauthors in a 2023 Oxford Open Climate Change paper, Global Warming in the Pipeline, that declining global aerosol emissions (including the cuts triggered by the new shipping regulations) will accelerate the planetary warming rate well beyond standard projections.

Zeke Hausfather offered a counterpoint in a Carbon Brief post on April 4, stressing that some acceleration in warming has long been projected by models and that the 2023-24 spike may not signal anything unusual: “There is a risk of conflating shorter-term climate variability with longer-term changes – a pitfall that the climate science community has encountered before.”

An ongoing thread launched with a RealClimate post on May 30 is highlighting new research and data points related to the 2023 extremes. Post author Gavin Schmidt, who succeeded Hansen as director of NASA’s Goddard Institute for Space Studies, also penned a commentary in Nature on March 19 entitled Climate models can’t explain 2023’s huge heat anomaly — we could be in uncharted territory. In that writeup, Schmidt stressed:

…the 2023 temperature anomaly has come out of the blue, revealing an unprecedented knowledge gap perhaps for the first time since about 40 years ago, when satellite data began offering modelers an unparalleled, real-time view of Earth’s climate system. If the anomaly does not stabilize by August — a reasonable expectation based on previous El Niño events — then the world will be in uncharted territory.”

Jeff Masters contributed to this post.

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14 comments

  1. PlutoniumKun

    A key problem in our analyses is the inbuilt assumption that climate change is a steady, linear process. In reality, if you spend any time studying bog/lake or soil cores from the post glacial period, you will see that it can often be very swift and dramatic – a regional climate balance can literally switch over the course of a few years – perhaps even a season. During the holocene, over the course of a few thousand years, the climate of north-western Europe was alternatively very cold and wet (glaciers), cold and dry (permafrost), cool and wet (bogs everywhere), warm and very, very wet (rapidly melting glaciers), mild and very dry (resulting in huge areas getting covered with metres of dust, which became the very fertile soils of central France). And thats not including things like the mild blowingly huge tsunamis that resulted from sea level change

    Almost all these changes were very rapid and were to a large degree catastrophic for whatever ecosystems or human populations happened to be in the wrong place at the wrong time. With a trained eye you can see these impacts written all over the landscape. The results were invariably catastrophic, and thats before you had agriculture and cities.

    Unfortunately, the notion of steady linear change is built into how we deal with these issues – as Taleb would put it, we are very bad at thinking about long tail risks. Climate change is stuffed with long tail risks of many kinds. Whatever happens at a global level, we have no idea if the regular spring rain in our local area will come every year, or if your local river will dry up, or be subject to what used to be a 1000 year flood event every year. Two decades ago I was at a conference on the subject and jokingly someone asked the climate scientists where they would move with their children if they could. A favourite choice was the Pacific north-west. None of them had anticipated the impact of climate change on forest fires and consequent air pollution which we now know is going to be a huge problem in that region.

    In many ways, our belief that we can ‘manage’ the change may be more dangerous than climate change denial.

    1. ACPAL

      Not only is climate change non-linear at many levels our weather/climate appears more chaotic than linear, or any of the other branches of mathematics. While the weather services can make short-term predictions (a few days), medium-term predictions (annual), and perhaps some recurring trends (ex: El Nino) a quick look at a wind direction map or satellite cloud photo easily shows the chaotic nature of weather. I seriously doubt any of the global climate models take into consideration that they are dealing with a chaotic system. Nor have I heard of any of the modelers admit that there is great uncertainty in their models.
      https://m.media-amazon.com/images/I/714+48Bus9L._AC_SY450_.jpg

      1. Jeremy Grimm

        There are many climate models and they are commonly fed the same data and run against each other to arrive at probable error bounds on predictions based on their aggregated predictions. There is disagreement about what values to assign model parameters and what features of climate to incorporate. Most modellers and climate scientists would agree that many features of climate change are unknown and unmodeled and many other features, though known are poorly understood:
        “The role of aerosols in climate change is uncertain because aero­sol properties are not measured well enough to define their cli­mate forcing.” [p. 13, “Climate Warming in the Pipeline”]

        I have long been impressed by the way relatively simple systems can manifest chaotic behavior –e.g. double pendulum systems, and how long it took before chaos was discovered. I suppose that might offer evidence of an inherent bias against chaos.

    2. Susan the other

      But what choice do we have? All over the western US, controlled burns are becoming the standard. In some places they wait for the winter snow or rain to do those burns so they don’t escape the site. There might be a variety of methods to avoid fire altogether, like manufacturing good mulch from a combination of underbrush and deadwood with collected kitchen waste. Seems logical that there could be all sorts of solutions involving serious industrial-level recycling as part of the prevention. Not just the obvious that the products of recycling will not only clean up our huge garbage and plastics problems but preclude using new energy sources to manufacture new products from scratch which are still essential for our maintenance. And etc.

    3. wilroncanada

      2 weeks ago, PK, I listened to a talk from a retired climate scientist friend. His introduction included the note that we are possibly the luckiest people in the world in terms of overall climate. This is roughly the “Pacific north west” you mentioned; in our case the Cowichan Valley, on Vancouver Island 50 kms north of Victoria. We have always had liveable temperature range, sufficient, but not too much, rainfall, and mostly benign winds. We have also been subject to a heat dome 4 years ago, floods from an atmospheric river 3 years ago, and some worrisome forest fire activity, but no major forest fires near enough to cause long-term breathing issues. That, in the world’s best climate location, shows what climate change is doing everywhere.

    4. Jeremy Grimm

      “A key problem in our analyses is the inbuilt assumption that climate change is a steady, linear process.”
      This is true, but I believe the characterization of the “assumption that climate change is a steady, linear process” as “inbuilt” bears further examination. I believe many people prefer to think in terms of steady linear processes because so much of modern life has been linearized, and because steady linear processes are much easier to conceptualize and they feel more comfortable and comforting, — more controllable. I believe our politicians seized on this tendency in the Populace in constructing the climate change narrative they have championed since the 1979 Charney report. The Charney report offered a simple linear constant with which to calculate the rise in the Earth’s temperature as the level of CO2 in the atmosphere increased. This Charney ‘doubling’ constant served as tool economists could use to conjure up a Carbon Budget. Charney’s doubling constant also tucked a bunch of unpalatable assumptions, caveats, and constraints nicely under the covers of the depths of Charney report — little things like ignoring the slow climate feedback mechanisms when calculating the Charney’s doubling constant. I wonder whether the “assumption that climate change is a steady, linear process” is inbuilt or more accurately characterized as deliberately built-in.

  2. Ignacio

    The paper by Yuan moves us to another polemic on “geoengineering” that I believe should be parked as a distraction or deviation from what should be the global goal reducing GHGs. This is not to say that the impact of lower sulphur emissions shouldn’t be considered and entered in the models (with the limitations models have) but now, it will be tempting for many to argue about a “need” to increase sulphur emissions from ships that as a matter of fact would do nothing to stop the global warming. Distractions do not help.

    Last phrase from PK’s comment is spot on certainly.

  3. GrimUpNorth

    My expertise is the the formation/growth of water/ice in clouds, not Global Climate Modelling, Having Just seen PlutoniumKun post, I do not wish to seem like I approve of managing climate change over actually stopping it.

    The removal of so2 from the ship pollution, gives an exciting/scary opportunity for scientists to study the potential effects of a climate engineering strategy proposed far back in the late 80s by John Latham (RIP, a nicer guy you will not meet) and Salter. The idea is to seed the clouds which cover vast areas of the ocean. This seeding enhances the number of water droplets formed in the cloud and as they are all competing for water vapour they are smaller, this makes the cloud brighter causing it reflect light. Ship tracks that actually do this can be seen on a satellite image.

    Obviously changing tropospheric temperature in large areas of the Atlantic ocean is going to change the weather in many countries. We now have real data (if we can separate it from other effects) on what happens when you warm the ocean air, we can extrapolate to what happens when we cool it, Of course the ocean temperatures are increasing anyway (Note ocean/air coupling is complex), so we would just be offsetting this increase.

    Can we get away with doing this? With little hope of us changing the current economic system I think it inevitable that we will try, not only is it quick and easy to do, it could also decrease the strength of hurricanes in the USA.

    1. Jeremy Grimm

      Considering the current state of knowledge about the Earth’s climate and its evident complexity deliberate experiments playing with geoengineering seem very unwise. We are already engaged in a few inadvertent experiments with the Earth’s climate that could promise some catastrophic results. Maybe now is not the best time to play with more experiments.

  4. ET

    No mention of gas pipeline explosion. Seems ridiculous to not bring that up since methane is many times worse than co2.

    1. cousinAdam

      And let us not forget the thawing of methane in (not so) ‘perma’frost and undersea methane clathrates in steadily warming arctic waters. Pity those clathrates couldn’t be harvested as a substitute for natural gas instead of letting it boil away into the atmosphere as a greenhouse gas (20x more potent than CO2 until it decomposes, thankfully fairly quickly, but still…..it becomes largely CO2 as well).

  5. Wukchumni

    Another recent paper, this one just published in the Journal of Climate, asserts that we could see a complex web of regional weather and climate effects for years to come as a result of Hunga Tonga’s water vapor. Led by Martin Jucker (University of New South Wales), the paper uses the WACCM global climate model, which incorporates stratospheric chemistry, to simulate a Hunga Tonga-like eruption and its impacts up to a decade out.
    ~~~~~~~~~~~~

    Volcanoes have often been game changers in humanitys’ past, except nobody knew it. This one is a rare ‘Submarine Volcano’ of which scant information is known as only a little over 100 have known to have occurred.

    Our wildflower season in the Sierra foothills was a month late in arriving, and while that means nothing save some waiting for them to arrive, the same sequence has dire effects on food crops which we plant & hope to harvest at fairly precise times, and this could go on for many years as it did when a couple of Icelandic volcanoes blew up in 1783-85, fomenting the French Revolution many years later.

    1. steppenwolf fetchit

      I am confident our climate systems will get back on global warming track after a few years of Hunga Tonga perturbation, just as they did a few years after the Pinatubo Event.

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