In short
Whether the world is prepared for a “super El Niño” in 2026–27, and how climate change and political attacks affect climate science and preparedness.
Guest backgrounds
Ming Fang Ting, Professor of Climate at Columbia University; focuses on climate modeling (not direct observational fieldwork), using data and supercomputing.
Key claims
El Niño is driven by weakened trade winds that let warm Pacific water spread east, releasing heat to the atmosphere and shifting global rainfall via “teleconnections.” A “super” El Niño is defined using Nino indices: strong >1°C, super around >2°C. Forecasts give ~100% chance El Niño conditions, with ~63% chance of super strength. Climate change likely increases heat extremes, but models do not yet show it reliably changes El Niño behavior itself. Extreme weather attribution uses model comparisons (with vs without fossil-fuel warming) to estimate how much human-caused warming raises odds.
Notable examples
1877–78 “Great Famine” with ~50 million deaths; 2023–24 El Niño (~1.5°C) linked to widespread heat waves; 2015–16 El Niño coral bleaching (Great Barrier Reef); 2023–24 floods in Kenya; wildfire risk in Indonesia/northern and eastern Australia; flooding/landslides risk in California/southern U.S. and Peru. Mentions political proposal to dismantle ocean monitoring (Congress blocked it).
Written by AI. May contain mistakes. Listen to the episode to check what was said.
Chapters
Tap a time to open that second in VOThe Great Famine and El Niño
0:56 to 1:31
Learn about the Great Famine caused by El Niño and its historical significance.
“When you're running a business, the best days are the ones where priorities stay on track.”
The Great Famine and El Niño
1:42 to 2:32
Learn about the Great Famine caused by El Niño and its historical significance.
“The period is now remembered as the Great Famine.”
Understanding Super El Niño
2:34 to 3:40
An introduction to the current Super El Niño and its implications.
“Since 1970, our appetite for fossil fuels has been increasing global average temperatures by about 0.2 degrees Celsius every decade.”
Basics of El Niño Explained
3:40 to 4:36
Professor Ming Fang Ting explains the fundamentals of El Niño.
“Professor Ming Fang Ting, welcome to Zero.”
Mechanisms of El Niño
4:36 to 10:10
Explore how El Niño affects global temperatures and weather patterns.
“And it also, the cooling, you know, the water, warm water being moved away, it also allows the deep, cold, and rich water to come to the surface.”
Super El Niño Predictions
10:10 to 12:30
Discussion on predicting the strength of Super El Niño events.
“And it's in fact already exist, the conditions we're already seeing it.”
Historical Context and Future Preparedness
12:30 to 14:00
Comparing past El Niño events to current preparations for the upcoming one.
“Now, of course, over the last 200 years, we have been heating up the planet by burning fossil fuels and adding to the greenhouse gas blanket, which is heating up the planet.”
Understanding Super El Niño and Historical Context
14:00 to 16:42
Learn about the implications of the upcoming super El Niño and its historical impacts on global populations and agriculture.
“That's about 3 to 4 % of the global population at the time because of the droughts that happened and the famine that was caused.”
The Consequences of El Niño Events
16:42 to 21:05
Explore the environmental consequences of past El Niño events, including heatwaves, flooding, and agricultural impact.
“El Ninos that have happened and what kind of impacts have they led to?”
Factors Influencing El Niño Intensity
21:05 to 24:46
Discuss the factors contributing to the intensity of El Niño events, including La Niña and human-caused climate change.
“there can be really severe flooding that can lead to landslides, for example.”
Show all 20 chapters
The Unique Nature of El Niño Events
24:46 to 25:04
Understand why no two El Niño events are the same and how their impacts can vary based on multiple climate factors.
“So depending on how the weather pattern itself evolves under a certain El Nino condition, you can get very different impact in different regions.”
The Unique Nature of El Niño Events
25:10 to 26:11
Understand why no two El Niño events are the same and how their impacts can vary based on multiple climate factors.
“If you've learned something new from Xero, please do give us a rating on your favorite podcast app.”
The Unique Nature of El Niño Events
26:14 to 26:29
Understand why no two El Niño events are the same and how their impacts can vary based on multiple climate factors.
“Brokered services by Open to the Public Investing, Inc., member FINRA and SIPC.”
The Unique Nature of El Niño Events
26:33 to 27:29
Understand why no two El Niño events are the same and how their impacts can vary based on multiple climate factors.
“Let's talk about healthcare for a second.”
Political Challenges in Climate Science
28:01 to 29:20
Explore how political attacks impact climate science and funding.
“Now, this is all happening at a time where, at least in the US, there are attacks from governments, from political actors on climate science itself.”
Communication Challenges in Climate Research
29:20 to 30:56
Learn how climate scientists communicate probabilistic outcomes.
“One of the biggest impact is the funding itself.”
Understanding Extreme Weather Attribution
30:56 to 33:18
Discover the process of extreme weather attribution and its implications.
“But one field that is emerging that is trying to make this communication simpler to say not all extreme weather is caused by climate change, but some we can clearly show the link to climate change.”
The Political Landscape of Attribution Science
33:18 to 35:34
Examine the political implications surrounding attribution science.
“National Academies of Science, Engineering and Medicine are conducting a study to look at attribution science.”
The Importance of Statistical Awareness
35:34 to 36:54
Understand the significance of communicating statistical risks to the public.
“the conclusions drawn by one group may not be accurate, I'm totally for it.”
The Importance of Statistical Awareness
38:35 to 39:34
Understand the significance of communicating statistical risks to the public.
“about everywhere you turn, every field and every function, but without identity, you can't trust they'll serve your business instead of jeopardizing it.”
Transcript
Automatic transcript. May contain errors.0:00The thing about AI for business, it may not automatically fit the way your business works.
0:05Mingfang Ting:At IBM, we've seen this firsthand. But by embedding AI across HR, IT, and procurement processes, we've reduced costs by millions, slash repetitive tasks, and freed thousands of hours for strategic work. Now we're helping companies get smarter by putting AI where it actually pays off, deep in the work that moves the business. Let's create smarter business, IBM. At Venture Global, we think about what can be done, not what's usually done. Through innovation, Venture Global is not only building some of the largest energy facilities in the world right here in the United States, but delivering American energy at a fraction of the cost and a fraction of the time.
0:49Mingfang Ting:So while others are busy talking, we're busy building. That's Venture Global. That's unstoppable energy. When you're running a business, the best days are the ones where priorities stay on track. For midsize and large companies, risk can affect multiple parts of the organization at once, from property and liability to cyber and regulatory challenges. At that level, managing risk becomes an ongoing discipline. At the Hartford, the focus is on helping businesses manage risk before it turns into something more disruptive. And when losses do happen, that work is paired with insurance coverage shaped by years of underwriting, risk engineering, and claims experience.
1:31Mingfang Ting:Learn more at thehartford.com slash risk mitigation. Policies provided by Hartford Fire Insurance Company and its property and casualty affiliates, Hartford, Connecticut.
1:41Akshat Rathi:More than 50 million people were killed between 1875 and 1878. The period is now remembered as the Great Famine. And one of the primary causes behind the famine was a naturally occurring phenomenon called El Nino. In fact, the 1877 El Nino is the strongest ever recorded. As of June, we have entered another El Nino event. And scientists are expecting this one to be very strong. Some call it a Super El Nino or even a Godzilla El Nino. So, are we better prepared in 2026? There are, after all, five times as many people as in 1877, and the planet is 1.4 degrees Celsius hotter. This is Zero. I am Akshat Rathi.
2:34Akshat Rathi:This week, understanding a monster. Since 1970, our appetite for fossil fuels has been increasing global average temperatures by about 0.2 degrees Celsius every decade. That is typically how much a single El Nino event raises global average temperatures by. And it does so by releasing vast amounts of heat from the Pacific Ocean. So this El Nino will not just cause disasters around the world, but it will also give us a taste of what climate change could look like in 2035 if we continue to burn fossil fuels at the same rate. To understand the El Nino phenomenon, I'm joined today by Ming Fang Ting, Professor of Climate at Columbia University.
3:23Akshat Rathi:We talk about the science of El Nino, how prepared the world is, and how scientists are responding to the increased political attacks on an overheating planet.
3:40Akshat Rathi:Professor Ming Fang Ting, welcome to Zero.
3:43Mingfang Ting:Thanks for having me.
3:43Akshat Rathi:So we are about to enter what people are calling a super El Nino. Before we start to talk about the super part, can you just walk us through the very basics of what an El Nino is?
3:57Mingfang Ting:El Nino is one of the most influential climate pattern. It impacts not only the local region where it starts, which is the tropical Pacific, but it also impacts regions far from that region through something we call teleconnection. And it can cause droughts in some parts of the world and flooding in other parts or hurricanes and other activities. So El Nino is a natural phenomenon. And to understand why El Nino occurs, we have to start from the normal state. So during the normal state of the tropical Pacific, we have this steady trade winds that blows from the east toward the west, which basically pushes warm surface water that is exposed to the sunlight toward the west, and forming something we call the Western Pacific Warm Pool.
4:59Mingfang Ting:And the warm water there then fuels precipitation, the rainfall, you know, convection and rainfall that leads to rainy climate in regions like, you know, Indonesia, you know, Northern Australia, and relatively cool climate in the eastern part of the Pacific, like the coast of Peru. And it also, the cooling, you know, the water, warm water being moved away, it also allows the deep, cold, and rich water to come to the surface. That also helps the ecosystem there, allows, you know, fish to flourish in that region. During El Nino, which is a disruption of this normal cycle, and what happens there is the wind tends to weaken, the trade winds tend to weaken, And that allows the warm water that is pushed toward the west to spread back toward the east, covering pretty much the majority of the tropical Pacific.
5:58Mingfang Ting:The tropical Pacific is a huge, you know, basin. So that allows a lot of the heat from the surface to be sent back to the atmosphere, increases the global mean surface temperature and, you know, causing convection changes that alters the atmospheric circulation, which means high pressure, low pressure in different regions. So that then leads to anomalous climate linked to surface temperature as well as precipitation, droughts, and other phenomena.
6:34Akshat Rathi:And the opposite happens in a La Nina phase where instead of the heat being released from the Pacific, more heat is stored in the Pacific, right?
6:43Mingfang Ting:Exactly. So there is an opposite phase of the El Nino, we call it ANSO, El Nino Southern Oscillation Cycle. And the opposite phase is the intensification of trade winds. So the wind actually becomes abnormally strong that pushes warm water further to the west that allows the warm pool to shrink. And that causes more or less opposite kind of impact to a lot of the global phenomena, climate phenomena, but not exactly. You know, there are some asymmetries between the two.
7:19Akshat Rathi:And just so we understand, obviously, the Pacific Ocean is the largest ocean by quite some distance. And when the heat from the Pacific Ocean is released or absorbed in these two phases, it has these global impacts because it can make a big global difference to average temperatures, right? What is the range in which typically global average temperatures increase or decrease during an El Nino versus a La Nina?
7:49Mingfang Ting:Very good question. Yes, one of the things El Nino does is that, as I mentioned, that the surface water becomes warm across the entire Pacific so that it allows more heat to be transferred from the ocean toward the atmosphere through this warm surface water. As you pointed out, the Pacific is the largest ocean. So once it's all covered by warm water, that is a very big source of heat to the atmosphere. And that actually increases the global mean surface temperature by the order of something like 0.5 degree globally averaged. This is what happened in some sense.
8:32Akshat Rathi:0.5 degree Celsius.
8:33Mingfang Ting:Celsius, yes. Half degree Celsius. This is what happened in 23, 24, the most recent El Nino. If you recall, there was this spike in the global mean surface temperature.
8:46Akshat Rathi:And now scientists are talking about a super El Nino. What is this definition of weak, normal, big, super El Nino? How is it measured exactly?
9:00Mingfang Ting:The strength of the El Nino is measured by what we call Nino indices. There are multiple indices. We basically average the surface temperature over a certain region of the tropical Pacific where we get the largest anomaly. So a normal El Nino is when that index is above 0.5 degrees over a certain period of time. and a strong El Nino would be above one degree and a super El Nino would be something like above two degrees Celsius. All of them are in Celsius.
9:41Akshat Rathi:And right now there's a discussion that this is a super El Nino. Do we know how much is the anomaly? Is it two degrees Celsius or more?
9:51Mingfang Ting:Right now the probability in all of the forecasts are probabilistic. We're based on multi-models. So we estimate using statistical methods of what is the likelihood of this El Nino happening and what is the likelihood of it reaching certain strengths. So currently, the model forecasts based on multiple models across the world is that there is 100 percent chance the El Nino will be happening. And it's in fact already exist, the conditions we're already seeing it. But even back in April, we knew quite a high likelihood this El Nino is happening. And currently, the chance of a super El Nino is about 63 percent.
10:38Mingfang Ting:So it's above 60 percent.
10:40Akshat Rathi:And in terms of trying to understand the El Nino system's strength and weakness, what causes certain El Ninos to be bigger than other El Ninos?
10:51Mingfang Ting:That's a very good question, which is something that we are still researching. We know the mechanism of how El Nino happens, which is when you have the heat during the normal time, you have the heat being pushed toward the west, and that heat is pushed toward the ocean. In the La Nina phase, including the normal phase, the heat is stored into the ocean, And that ocean will be accumulating heat and taking a lot of heat from the atmosphere. And eventually, it reaches a state that it can release that heat back into the atmosphere. And that is where El Nino will happen. Now, when exactly it releases that heat and what triggers it, we know a lot about it, But it's not like, you know, there's a random chance like the westerly, what we call westerly wind bursts is the reason, you know, it weakens the trade winds.
11:48Mingfang Ting:And the question of how strong it will be depends on the amount of heat that is stored and other ocean conditions, ocean dynamics and the release process. So what we know for sure is the model takes into account all of these conditions and was able to predict, you know, how strong it might become.
12:14Akshat Rathi:And so this La Nina and Nina phase, they cycle between two and seven years roughly and do this process of absorbing the heat and then releasing the heat. This is a natural phenomenon that has been happening on the planet for a very long time. Now, of course, over the last 200 years, we have been heating up the planet by burning fossil fuels and adding to the greenhouse gas blanket, which is heating up the planet. But it's also heating up the ocean because when you're heating the atmosphere, this La Nina El Nino system and of course the other oceans are absorbing the heat that's in the atmosphere.
12:51Akshat Rathi:Yes. Is it then that climate change, because of the heat being built up in the atmosphere, is supercharging the El Nino?
13:01Mingfang Ting:There are certainly possibilities that is happening, but currently the models are not showing us for sure that climate change, the global warming, fossil fuel-induced global warming is actually changing the behavior of the El Nino itself. So El Nino is still happening on a natural basis. It's the ocean atmosphere interaction in the tropical Pacific. But what you said, you know, that is something that we are all thinking about, how much of it could be contributed by the fact that the ocean is taking up more heat. Yes.
13:40Akshat Rathi:So the strongest El Nino on record is known to be between 1877 and 1878. and the various impacts that came from that El Nino and that were quite severe. You know, the world was much poorer a place back then. Something like 50 million people were killed across India, China, Brazil. That's about 3 to 4 % of the global population at the time because of the droughts that happened and the famine that was caused. Now, we are going into a strong super El Nino. Are we better prepared, do you think, in 2026-27 with 8 billion people on the planet?
14:25Mingfang Ting:I hope so. I certainly hope so. Yes, 1876-78 is what we call the Great Farming period. It caused severe drought across the globe, as you already mentioned, India, China, Africa, as well as Brazil. And those droughts obviously affected the crop yield. So crop failed in many, many regions. And one of the things I would say, the farming is obviously not directly caused by just crop yield drop that contributed, but a lot of it is policy as well. So people didn't know we are going to get into this period of droughts in multiple regions. So, for example, India, the crop trading at the time was continuing like normal.
15:23Mingfang Ting:So one of the things I would hope now we know is that we know exactly what's going to happen. I mean, not exactly. I have no very high likelihood we are going into a super El Nino. So we can be better prepared in terms of what we can do about it. By the way, I should mention India rainfall is already reduced this year. We're already seeing the impact of this El Nino. And I believe the onset of monsoons delayed, which partially also led to some of the, you know, contributed to the heat waves there earlier, pre-monsoon heat waves. So my hope is that people will be actually prepared in the sense of delay planting, for example, for agriculture side of things, and also not to export crops when droughts coming.
16:20Mingfang Ting:So yeah, I think there are a lot of ways, and technology as well.
16:27Akshat Rathi:And in the recent decades, when we have had technology both to make predictions about El Nino and then ideally make some policy changes, what are the recent strong El Ninos that have happened and what kind of impacts have they led to?
16:46Mingfang Ting:The most recent one is 2324 El Nino. That one's actually really unusual. It's not a super El Nino. It's a strong El Nino. It's reached, index reached 1.5 degrees Celsius. So it is a strong El Nino, but it is not a super one. One consequence of that El Nino was the actual concurrent heat waves. We experienced in July 23, the summer of 23, and both summer of 23 and 24, in fact, we had lots and lots of heat waves happening across different continents. And I think that is, you know, as we talked earlier, is contributed partially by the increase in global surface temperature on top of already gradually increasing temperature.
17:41Mingfang Ting:Right.
17:42Akshat Rathi:The heatwaves we are experiencing are the El Nino 0.2 degrees Celsius temperature increase on top of the 1.2 or 1.4 degrees Celsius of climate change that we have caused. And that makes the heatwaves even more extreme than they would have been had we not caused climate change.
18:00Mingfang Ting:Yes, exactly.
18:01Akshat Rathi:And in that case then, is it accurate to say that, you know, when we see this El Nino phase, we are sort of getting a flavor of what extreme weather would look like in five or 10 years as we continue to burn fossil fuels and heat up the planet?
Read the full transcript
18:21Mingfang Ting:Absolutely. I mean, we are definitely seeing the temperatures continue to rise. So on top of that, if we have another super onion, you know, like this upcoming one, then that adds to additional heat into the atmosphere. So that kind of, you know, higher global mean surface temperature, obviously the global mean when we say, you know, the 0.5, 0.2, 0.5 degrees Celsius is in the global mean. It's regionally can be much higher. So they're not evenly distributed. So some regions may be up to one degree, two degrees. So that is a substantial amount being added. So we can definitely expect to see a lot more of concurrent heat when that happens, which means basically you are seeing heat wave happening across different regions at the same time.
19:12Akshat Rathi:And let's just talk through some of the impacts. We've mentioned in the 1877 El Niño, the strongest ever, there were famines. But the thing that El Niño does is increases droughts in certain regions, but also increases flooding in other regions. It just changes rainfall patterns in multiple places. And both can have impact on agricultural yields. But as we've also become much more urban in the last two centuries, it can have massive impacts on cities and people. The 23, 24 El Nino, for example, had catastrophic floods in Kenya. And then there are other impacts from El Ninos that can come through.
19:54Akshat Rathi:So the 2015-2016 El Nino is known for having caused a lot of coral bleaching, especially in the Great Barrier Reef in Australia. What other impacts should people be aware of?
20:07Mingfang Ting:Impact like wildfires is very severe. As we know, global warming already are causing drier conditions in many regions, like California, for example, southwestern U.S. And so that already increased wildfire risk. So in this case, El Nino is very well known to be linked to increased wildfire risk in regions like Indonesia, northern Australia, eastern Australia, where the suppressed rainfall happens. You know, when the rainfall shifts toward the central Pacific, the warm water moves toward the east, the rainfall also moves with it. So that is causing a lot of the drying conditions there, and wildfire is one of them.
20:57Mingfang Ting:As you pointed out, flooding is another common risk associated with El Nino. In regions like California, south-southern U.S., and some part of Peruvian coast regions, there can be really severe flooding that can lead to landslides, for example. hazards like that.
21:23Akshat Rathi:One way in which one of the scientists explained to me the super part of the El Nino was to think about the things that put heat into the ocean, which then eventually comes out. So one is because of human-caused climate change, we are heating up the planet, some of that heat is being transferred into the ocean. The other is the La Nina phase, which is a phase where there is more than normal heat that is absorbed by the oceans, and then it gets stored in the Pacific. And typically, an El Nino follows a La Nina. And so you get sort of a battery that is being charged, then that gets released in the El Nino.
22:05Akshat Rathi:And then there are other factors that we are still to understand. And of course, this is a very complex phenomenon. So all the factors are not yet understood. But is there any other factor that we should be thinking about on how much more heat is released in an El Nino?
22:23Mingfang Ting:I think you have covered most of it. Your understanding is so complete. I can't think of any additional factor that we haven't talked about. I think, you know, yes, ultimately, we are still trying to understand better. One of the things you mentioned is La Nina before El Nino, which is a phase that heat is being put into the ocean, storage phase. So there were studies indicating the longer the La Nina, La Nina seem, you know, tend to be lasting longer. Not this time. This time, you know, after the 23, 24 El Nino, we entered the La Nina phase and pretty much just ended right before this El Nino.
23:11Mingfang Ting:So it wasn't a super long La Nina heat storage phase. So there are studies indicating longer La Nina phase could lead to stronger El Nino. But I don't think that is being widely accepted as a valid mechanism because we don't see that in data. So that could be one, you know, is how La Nina behaves right before El Nino. that could determine the intensity of the following El Nino. But ultimately, I think we still have a lot to understand.
23:48Akshat Rathi:And then one of the scientists I was listening to said, no two El Ninos are the same. What does that mean?
23:56Mingfang Ting:Right. So first of all, yes, exactly. It means none of the, no two, and you can try to find the exact replica of the El Ninos. They always differ in some ways. But I think what it means more is that even if you have identical El Nino, the impact will never be exactly the same. I think that is more of what we usually mean in the sense that El Nino is putting, again, the weight to the dice. So it's not the only factor. Rainfall patterns here and there, droughts, all of that, that can be impacted by multiple factors in the climate system. El Nino is just adding a weight to one direction. So depending on how the weather pattern itself evolves under a certain El Nino condition, you can get very different impact in different regions.
25:03Akshat Rathi:After the break, I asked Professor Ming Fang Ting how climate scientists are responding in the face of increased political attacks. If you've learned something new from Xero, please do give us a rating on your favorite podcast app. It helps new listeners find the show.
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28:13Akshat Rathi:Now, this is all happening at a time where, at least in the US, there are attacks from governments, from political actors on climate science itself. Now, climate science is not new to political attacks. These have happened over the past three decades in many different ways. and the climate scientists community, including yourself, have worked to try and figure out what is the best way to showcase the work that you're doing, why it helps people, what are the facts and how it allows us to prepare for a better world. But particularly in this period, you know, there are direct impacts that can come through on people's lived experiences.
28:58Akshat Rathi:So there was a recent proposal from the Trump administration to dismantle the ocean monitoring system that you talked about, which can help us predict an El Nino. Of course, Congress has stopped that from happening. And so the ocean monitoring system will continue to support El Nino work for much longer. But as a climate scientist, how have you been affected?
29:24Mingfang Ting:We are all affected in different ways. One of the biggest impact is the funding itself. So, you know, all our works depend on funding, you know, our graduate students, our postdocs, you know, and other facilities that we need to do the work. Myself, I'm not an observational climate scientist in the sense that I don't go out and collect data. But as you pointed out, that is a super important part of our research because we rely on data. And my work is mostly relying on model. So that needs supercomputer infrastructure like that to help us continue our research. So one of the things I wanted to bring up is, you know, climate science itself, it's a physical science.
30:14Mingfang Ting:It's not really political. But I think we can communicate better in the sense, you know, it is a kind of like, you know, you're thinking about a throw of dice. you're really saying you're putting weight on certain higher numbers. Climate change is basically doing that. You're not equal chance of getting all the numbers, but rather now you're getting extremes more likely.
30:39Akshat Rathi:Yeah. And thinking about life in probability terms is very difficult for people in general, even for people who understand probability and who are working on statistical methods. And so that becomes a difficult issue to communicate. But one field that is emerging that is trying to make this communication simpler to say not all extreme weather is caused by climate change, but some we can clearly show the link to climate change. And that science is extreme weather attribution science. Can you just walk us through what extreme weather attribution work looks like? Yes.
31:20Mingfang Ting:This is a very mature science now. We're basically using models to help us understand what is likely this event happened. Let's say European heat wave. Currently, we're all talking about it. So how likely this event would happen in a world without fossil fuel versus with fossil fuel? We run model runs with those two conditions and then get a probability of this kind of event happening. And I don't know if you've read the news report, the World Weather Attribution Group has already done that. And they're always, you know, really fast in producing that. And the conclusion there is that it's very unlikely this event would happen without fossil fuel contribution into the climate warming.
32:20Akshat Rathi:Yeah, we are recording this episode during the heatwave in Europe in June. And the study says that this is the worst recorded heatwave in Europe and that it would be virtually impossible without human-caused climate change having run this model. And one of the scientists who was involved in the study put it very plainly. It's Frederica Otto. She's a professor at Imperial College London. And she said, yes, this is climate change. Yes, it is us causing this climate change. No, it's not El Nino that is making this extreme heat wave worse. And then she adds, we have the solutions and we are not implementing them fast enough.
33:06Akshat Rathi:And that clear communication is, of course, coming from a base of, as you said, a mature science. But there's already a layer of politics getting involved. Now, the U.S. National Academies of Science, Engineering and Medicine are conducting a study to look at attribution science. They did so a decade ago, and now methods have improved and become more precise. And so they are doing another study to look at effectiveness of these methods. And there is an effort from political actors, some in the government, some in think tanks, who want to weaken attribution science's value because they worry that it will be used in courts to try and hold powerful actors like governments or corporations to account.
33:58Akshat Rathi:What can scientists do to ensure that attribution science doesn't come under these kinds of political attack?
34:06Mingfang Ting:Again, you know, attribution science itself is a science. So, you know, I'm not familiar with this new attribution study conducting on the National Academy of Science. But even if they redo it, they'll be using the best model available. And I can't imagine scientists would claim otherwise. The results are going to be what it is. But it is probabilistic. So even though it is virtually impossible, it doesn't mean it's completely impossible. This could happen without climate change. So, you know, communication like, you know, adding some kind of emphasis, you know, compared to 1970s. I think in their study, they already done that compared to 1970s condition where fossil fuels already, you know, been burning for a while.
35:04Mingfang Ting:And it's about 200 times less likely in the 1970s condition. So I think put out more numbers like this could help. So this is not something we just sort of grab out of the same air. I believe in scientists' integrity. I think if people are truly believing they are exploring possibilities, the conclusions drawn by one group may not be accurate, I'm totally for it. I think the more the better.
35:42Akshat Rathi:Yeah, and 200 times more likely or less likely is a huge number, right? If suddenly someone were to tell me, if you cross the road today, there's a 200 times more likelihood that you'll get hit by a car, I would be scared. I would take care about crossing the road. I would make sure that the traffic light is red and not cross over without that. Same thing with, you know, taking a plane or a car. If you are going to die, then the probability increases by 200 times. Yes. You'd be very careful. And so people must heed what the statistics are telling us.
36:20Mingfang Ting:Yes. I think another example we can talk about is smoking. You know, a lot of people believe smoking increases the chance of getting lung cancer. And I hope a lot of young people learn that and not stop smoking because they know the probability shift, right? The odds change. So absolutely, I agree with you. The 200 times is a huge number. And we definitely should heed to that, change our behavior in some ways.
36:53Akshat Rathi:Thank you, Mingfang.
36:54Mingfang Ting:You're welcome.
37:01Akshat Rathi:And thank you for listening to Zero. Now for the sound of the week.
37:17Akshat Rathi:That is the sound of lava flowing from the most recent eruption of Mount Etna, which happened on the 26th of June on the Italian island of Sicily. If you like this episode, please take a moment to rate and review the show on Apple Podcasts, YouTube and Spotify. This episode was produced by Somersadi and Oscar Boyd. Our theme music is composed by Wonderly. Special thanks to Blake Maples, Laura Milan and Alyssa MacDonald. I am Akshat Rati, back soon.
37:55Thank you.
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From the publisher
The great famine of the 1870s killed 50 million people – and El Niño was a key driver. Another El Niño phase has just begun and it’s expected to be among the strongest. There are five times as many people in 2026 as there were in the 1870s and the planet is 1.4C hotter. So are we better prepared?
In this weekend's listen, Bloomberg’s Akshat Rathi speaks with Mingfang Ting, professor of climate at Columbia University, about the natural phenomenon and its interaction with human-caused climate change.
Read more:
- Bloomberg Green's deep dive on extreme heat
Thoughts or suggestions? Email zeropod@bloomberg.net. For more coverage of climate change and solutions, visit https://www.bloomberg.com/green.
See omnystudio.com/listener for privacy information.




