re:publica 25: Johan Rockström - Decisive Decade:  From Global Promises to Planetary Action

Brief Summary

The presentation addresses the critical state of Earth's stability, emphasizing the urgent need for rapid and large-scale action to reverse the current trajectory of environmental degradation. It highlights the unprecedented acceleration of global warming, the crossing of planetary boundaries, and the potential for irreversible tipping points. The speaker underscores the importance of adhering to the 1.5°C boundary, phasing out fossil fuels, and transforming global systems to ensure a sustainable future. Despite the challenges, the presentation conveys a message of hope, emphasizing the availability of solutions and the potential for a stronger, healthier, and more sustainable world.

  • The Earth is facing a decisive moment due to risks of destabilizing the planet's stability.
  • Evidence shows an unprecedented acceleration of warming and crossing of planetary boundaries.
  • Staying within the 1.5°C boundary and phasing out fossil fuels are crucial for a sustainable future.

Introduction: A Decisive Moment for Humanity

The speaker emphasizes the critical juncture humanity faces regarding the planet's future, highlighting not only geopolitical issues and assaults on science but also the risk of destabilizing the Earth's stability. For the first time in history, there is a serious consideration of the risk of irreversible damage to the life support systems that have allowed the world to develop over the past 250,000 years. The need for speed and scale is crucial to return to a safe operating space for a stable and habitable planet.

The Great Acceleration: Evidence of Environmental Impact

The evidence of environmental impact begins with the "Great Acceleration," illustrating hockey stick graphs from 1750 to the present. While industrialization has brought positives like improved health and life conditions, it has also led to massive GDP growth and resource exploitation. The focus is often on the carbon dioxide hockey stick, but any parameter related to human well-being shows a similar trend. Since the 1950s, there has been an exponential rise in biodiversity overexploitation, acid rain, deforestation, and other pressures, leading to the conclusion that we have entered a new geological epoch called the Anthropocene, where humans are the dominant force of change.

Exceeding 1.5°C: Shocking Data and Observations

In 2024, the global mean surface temperature rise exceeded 1.5°C, the warmest temperature in 100,000 years, pushing us outside the Holocene range. Recent scientific observations have been shocking, with air and sea surface temperatures showing unprecedented jumps. In 2023, there was a 0.3°C jump in temperature, far exceeding the normal annual increase. Despite entering a La Niña phase, temperatures are not cooling back as expected, leading to concerns about a potential shift in the trajectory of warming.

Candidates for Accelerated Warming

The scientific community is actively discussing the reasons for this accelerated warming. Candidates include natural variability like the El Niño oscillation and solar cycles. Paradoxically, policies reducing air pollutants, such as sulfate emissions from commercial shipping, may also contribute by allowing more solar radiation to reach the surface. Changes in the hydrological cycle and a potential reduction in the biosphere's capacity to absorb carbon are also considered. The Amazon rainforest, Earth's richest ecosystem, has already tipped over and become a carbon source, signaling a loss of resilience.

Climate Sensitivity and Global Carbon Budget

There is concern that the climate sensitivity, traditionally estimated at 3°C per doubling of carbon dioxide, may be higher due to underestimated loss of resilience in the Earth's system. If climate sensitivity is higher, the global carbon budget becomes even smaller, requiring an even faster phase-out of fossil fuels. The costs of exceeding 1.5°C are evident in the increased frequency and intensity of droughts, fires, floods, and heat waves, leading to significant economic impacts and loss of labor productivity.

Leaving the Corridor of Life: Historical Temperature Data

The planet is leaving the "corridor of life," as evidenced by ice core data from the past 400,000 years. For the last 10,000 years, the planet has remained remarkably stable, with temperatures varying within a narrow range. The Emian period, 110,000 years ago, peaked but never exceeded 2°C. This stability has enabled human civilization to develop. Pushing ourselves outside this corridor poses significant risks to the biophysical systems we depend on.

Tipping Points: Risks and Interactions

The planet is a self-regulating system with interactions and feedbacks. Pushing these systems too far can lead to crossing thresholds and triggering self-amplifying positive feedbacks. Sixteen tipping elements regulate the climate system, and many are at risk of crossing thresholds at relatively low temperatures. These tipping points can interact and lead to cascade impacts. For example, the melting of the Greenland ice sheet can slow down the thermohaline engine (AMOC), impacting monsoon systems and the melting of the West Antarctic ice sheet.

Planetary Boundaries: Defining a Safe Operating Space

Quantifying the safe operating space for humanity involves identifying the Earth system processes that regulate stability and resilience. Nine planetary boundaries, including climate, biodiversity, land configuration, and chemical loading, have been quantified. Current assessments show that six of these boundaries are outside the safe space, supporting concerns about accelerated warming. To hold 1.5°C after a period of overshoot, carbon dioxide removal technologies and a transformation of the global agriculture system are necessary.

Exponential Trajectories and Decarbonized Solutions

Achieving the necessary transformations requires S-curves of exponential positive trajectories. Double-digit adoption of decarbonized solutions is emerging, with renewable energy and electric vehicles showing significant progress. Even difficult-to-abate sectors like steel, cement, and fertilizer are seeing potential solutions. While challenges remain, the assessment indicates that these problems are not impossible to solve.

Conclusion: Danger, Opportunity, and the Path Forward

The planet is in danger, with multiple planetary boundaries outside the safe space. However, we are not yet in a red zone where a turnaround is impossible. The fossil fuel era is at the beginning of its end, and there is still a chance to turn things around with available solutions. By standing up with science, we can create a stronger, healthier, more secure, and more competitive future.

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Transcript

Full transcript of “re:publica 25: Johan Rockström - Decisive Decade:  From Global Promises to Planetary Action”. Click a timestamp to open the video at that moment. Need another video? Use the YouTube transcript generator.

0:00 [Music] [Applause] [Music] Dear friends, it's uh great to be back on the Republica stage, but it's also really important for scientists to have this opportunity because we are facing undoubtedly in all forms of risk assessment a very decisive moment for humanity's future on planet earth. And I'm not talking only about the geopolitical turbulence in the world and

0:46 the destructive assaults on science and the denialism and populism. I'm talking about risk. I'm talking about the fact that we for the first time in human history on planet earth are forced to seriously consider the risk of destabilizing the stability of the entire planet. What does this mean? What it means that we are very close to approaching tipping points where we cause an irreversible drift away from the life support systems that has enabled the world to develop over the past 250,000 years. If you want to take the whole journey of humanity's existence on Earth, or at least the 10,000 years when we've developed civilizations as we know it since we left the last ice age. That's why I

1:31 picked this picture, the Christmas Day 1968, Apollo 8, Earthrise classic with this steep, transformative, exponential reflection of the moon. Because the only currency that matters today to have any chance of a manageable future for humanity is speed and scale. And I'll come to that in terms of the evidence that supports it. So we're talking today of the need to rapidly return into the safe operating space of a stable, resilient, habitable planet. The evidence starts with the great acceleration. All the evidence we have of the hockey sticks from 1750 until today. The x-axis is the same time frame. The red graphs here is the social economics. You know the journey. We

2:17 start burning coal in the late 18th century and off we go in the industrialized metabolism that leads to GDP growth, resource exploitation, all forms of massive growth which has had many very important positives in terms of health and and better life conditions and the possibility of a world to host now 8 billion people. But look at the right hand side on the hockey sticks and the impact on the planet. We tend to focus only on the carbon dioxide hockey stick on the upper leftand corner. But I can tell you pick any parameter that matters for human well-being. It looks the same. Up until 1950s we have linear yes increased environmental impacts

3:03 unsustainable exploitation but it's the takeoff point. In 1955, we're 3.5 billion people and off we go in the exponential rise in terms of overexloitation of biodiversity, acid rain, deforestation, loss of biodiversity, all forms of pressures on the planet take off at a point where we today conclude in the earth system sciences that we are in a whole new geological epoch. We're exiting the holosene and event the anthroposine. Anthros Greek for humans. We're now the dominating force of change on planet earth. We're hitting the ceiling of the biophysical processes, the hardwired processes that regulates the very functioning of the earth system. That is insight number one. Now

3:51 this is starting to cost us. We have today a situation where we for the first time last year in 2024 exceeded 1.5° CC of global mean surface temperature rise. Dear friends, referencing the IPCC, that's the warmest temperature on Earth over the past 100,000 years. We are already outside of the holosene range of variability. Now, let me bring you into the lab. Let me bring you into why we are so nervous today. Why we have over the past 12 months heard scientific language that I've never experienced in my whole career. mind-boggling, shocking data, observations that we could never have thought was possible, would never

4:37 have been able to predict in our models. And it's this. It is the observations of air temperature on the left hand side and sea surface temperatures on the right. What you have here is from 1980s on the right hand side, from 2007 and onwards on the air temperature side. All the gray lines is the annual rise of temperatures which has led to the scientific conclusion that we have a global climate crisis. This is the graphs you all know. You have on the x-axis temperature and the y-axis burning fossil fuels. It's a linear relationship. The more we burn, the more temperatures rise. And we have entered a crisis because it's starting to cost the global economy and people so much that we are really in a situation of dire need of change. And then comes 2023 and we suddenly jump up in a jump that we've

5:24 never seen before. a 0.3° C jump in just one year when we normally have 0.03 per year. And just look at the graphs here. The orange line is 2023. The gray line behind it is 2024 showing the same level. But then comes 2025 which is this fat line here when we would have expected to go back into a let's say a normal crisis situation because we know that the two jumps 2023 2024 were El Nino years which are natural uh reinforcement years because it's when the Pacific Ocean releases heat into the atmosphere. But we're now in a leninia phase. You should expect a cooling back but we're not cooling back.

6:11 You may have seen WMO statement report coming out today which is really worrying because they predict with a 80% likelihood that we over the next 5 years will breach 1.5 one more time and that there's a 70% probability that we're stuck at this higher level. This is something wrong. What is happening? The honest answer is we do not know yet. There's a lot of work going on right now to try to explain why are we suddenly in a in a different trajectory of warming. Why do we see that the hockey stick of temperature in the air to the left and the ocean to the right suddenly shows this decade of accelerated warming? Just look at the graph to the left. This is

6:57 the climate crisis. 0.18 degrees Celsius per decade of warming caused by us humans. Then suddenly from 2014 onwards we jump up to almost 0.3° C per decade of warming. And the 2023 244 jump you see it right there. Now the candidates are discussed very very actively in the scientific community today. There's a mixture for sure of natural variability, the Ed Nino oscillation, the solar cycle having an all-time not all time but a high level but also that we have been able to reduce one of the planetary boundaries namely air pollutants. We have policies very positive policies on commercial shipping forbidding uh sulfate emissions from bunker oil which

7:43 reduces air pollutants which has a huge paradox. We're cleaning up air over the Atlantic and we're cleaning up cities like Beijing, which of course has a tremendously positive effect on reducing impacts on human health. 6 to 7 million people die prematurely each year because of air pollutants. But the paradox is that that air pollution has actually been cooling the planet. Get rid of it and we get more solar radiation hitting the surface of the planet. But that cannot explain all of it. very likely it's also the hological cycle that is ramping up causing um additional cloud dynamics which in turn has a net warming effect. And the third and final which is the scariest one is if we're starting to see a tendency of the living biosphere

8:30 reducing its capacity to take up carbon. We don't see that statistically yet. The ocean seems to still take up 25% of carbon dioxide from our fossil fuel burning. 25%. It's been doing that for 150 years leading to ocean acidification as I'm sure you're aware. But on land on the other hand, we're starting to see cracks in this carbon uptake capacity. We're starting to see more fires, more bark beetle outbreaks. We're seeing it in Germany. We're seeing it in Norway. We're seeing it in Russia and Canada. We have the latest data of the Brazilian part of the Amazon rainforest, which did you know this? Planet Earth's richest ecosystem on land, the Amazon basin, has in the Brazilian part, the largest part, tipped over already. It's no longer a

9:16 carbon sink. It's a carbon source. Now, this is a warning sign. And this can be therefore the first signs of a planet losing its resilience, losing its buffering capacity, which we in the climate science community call climate sensitivity. You've probably heard this holy grail number of 3° C per every doubling of carbon dioxide which has been guiding our climate science and climate policies for the past 100 years since in the late 19th century first did the estimates. What if the climate sensitivity is slightly higher? There are many modeling runs showing that that could well be the case. It can be four degrees for a doubling, 5 degrees for a doubling if we have underestimated the

10:01 loss of resilience in the buffering capacity of the earth's system. And this could be the first signs that that is where we're heading. And if that is the case, dear friends, then of course the global carbon budget gets even even smaller and the pace by which we have to phase out fossil fuels has to go even faster. And this is what we're struggling with right as we speak. That's where we are in the lab. But in 2023 when we touched 1.5 for the first time, we have the evidence now the costs. We've never seen the frequency and amplitude and strength of droughts, fires, floods, heat waves as in 2023. And the data, you have it here. Just look at the 60% increase of land under

10:46 drought in 2023. The massive increase of droughts, 50% increase just over that year. We have a massive loss of labor productivity. This is probably the most underestimated factor that heat is not only a life-threatening impact. In 2022, the latest estimates are that um up to 60,000 people across Europe lost their lives prematurely because of um heat levels hitting the most vulnerable citizens in Europe. It happened the previous time in 2003 where we also had one of these massive heat events. But this is of course impacting also the economy. So that is where we are in terms of the nervousness. So the

11:31 question is is the nervousness only related to extreme events? Well, it's not. It's also related to what I hinted before that the planet is now leaving what I call the corridor of life. And the data here is now well established. This is ice core data for the past 400,000 years. You see three plates here. Let's focus first on the right hand side. This is where we are today at 1.2 to 1.3°C of global mean surface temperature. That could be good to take off when we have in the Paris agreement. We say we're going to legally hold warming well below 2°C and aim for 1.5. That is the scientific definition of temperature, which is the 10-year moving average. So, it's a it's a more

12:17 persistent breaching of 1.5 that we're talking about. So, in 2024, we breached 1.5, but it was a one-year event, but it doesn't mean that we've lost the the permanent level of 1.5. We are now at 1.3 actually in the 10-year moving average. But look at the last 10,000 years. a remarkably stable planet 14 degrees Celsius plus minus 0.5 degrees. It's within that narrow range. You have the medieval warm period. You have the little ice age. All variability has occurred within this very narrow range. And then we have the last ice age 18,000 years ago. We have one more warm period called the Emian 110,000 years ago. And then we have an ice age here. And this is

13:03 250,000 years ago when we as modern humans start working and walking this planet as far as we know today. So we've lived through two ice ages and two interglacials. Now the emian according to the latest science as you see it peaked but never exceeded 2° C. So the broad corridor of life actually a corridor of life that goes 1 million years back is that the planet has stayed within a very narrow range never exceeding two warm interglacial never going below minus5 deep ice age. That's the planet as we know it. That's the biogeeochemical systems that that we depend on. And then we leave the last ice age and we go into an even more stable planet. And we know our journey there. We are just a few million people

13:51 right here living in caves. We're hunters and gatherers. We have a rough time. Massive variability of life support systems until we enter the holos scene and we barely entered it and go through the neolytic. This is the domestication of animals and plants. We settle down as sedentary communities and villages. Off we go in the innovation pathways that has taken us to the modern industrial revolution where we are today. That's the journey. And we have so much evidence that it's thanks to the stability in the holosene that enabled us to take us where we are today. So that is evidence piece number two. We have a reference point of the desired planet. And that is why it's such a drama to now push ourselves outside of the corridor. The third and final piece

14:37 of evidence is that the planet is a self-regulating complex biogeeophysical system with interactions and feedbacks. push these systems too far and you cross thresholds. The system goes from being dominated by dampening feedbacks that cool the planet that can handle stress like heat imbalance caused by fossil fuel burning to self-amplifying heat dominated by positive feedbacks. When ice melts, the surface gets darker. Instead of reflecting 90% heat, a very dampening feedback, it absorbs heat. It becomes a positive amplifier. Now we have mapped the 16 tipping element system that regulates and contribute to control the climate system. Six of them are up in the Arctic. It's the ground zero on planet earth. The green ice

15:22 sheet, the boro forest system, Arctic winter ice, perafrost systems connected via the North Atlantic and the Amok, the Amazon rainforest, three big systems in Antarctica. You have the tropical coral reef systems. They are across the entire planet. large biohysical systems that we're all collectively dependent on because they regulate the stability of the climate system. And here they are the long list of 16 systems. By the way, they are even in the IPCC, the Intergovernmental Panel on Climate Change. Check up working group 1, table 4.10, 4.10 in the working group 1 report. They're there wellestablished science. What is new, which is in a paper we published just two years back, is what you see to the right hand side here. This is the so-called burning embers risk analysis of the likelihood

16:10 at what temperatures are these tipping elements likely to cross their thresholds. Admittedly, what you see there's a large uncertainty range for many of them. Um, the darker the color, the higher the likelihood of triggering a tipping point and you see the temperature range up on the x-axis. I just want you to focus on the top five because they have, you see these little white circles there? That's the median level. That is the likely temperature at which they are crossing a threshold where they irreversibly will tip over from a state that helps us and cools us and keeps the life support functioning to a state that drifts us off towards less and less life support and self-amplified warming. And look at the list. the green and ice sheep, the West Antarctic ice sheep, abrupt throwing of

16:56 perafrost, all tropical core reef systems, livelihoods for over 400 million people, and collapse of the Labrador Sea and collapse of the Baron Sea ice. This is the evidence we have today why 1.5° C is a boundary. It's not a target. It's not a goal. It's something we really need to respect because go beyond it and we take big risks. Now we have also more and more evidence that these tipping element systems interact with each other and can lead to cascade impacts. So even if the uncertainty range is large and even if the temperature levels for triggering for example a tipping point in the Amazon rainforest may be higher than 1.5, we have evidence that if the green ice sheet really crosses a tipping point and really starts to flush out cold

17:43 fresh water in the North Atlantic that slows down the thermmoaline engine that runs the AMO the whole overturning of heat in the North Atlantic because this is a thermohaline engine that operates from the fact that warm saline water flows naturally from the southern o ocean up to the tip southern tip of Greenland releases heat making it habitable in where I come from up in the Nordic and Sweden and this heavy saline water high density saline water then sinks and drives the whole Amok and flows back on the bottom of the ocean back to the southern ocean. Now when that is flushed with cold water and impacted by the ocean dynamics, this

18:28 whole sinking system slows down and the amoch slows down. We see a sign of the amoch having slowed down with up to 15% already today. And we have a cold blob which is exactly what you expect up in the southern part of the North Atlantic which is what you would expect because it's the only part of the ocean that is cooling down because of the slowdown of the AMO. That slowdown very likely pushes the monsoon system further to the south which can cause less rainfall over the Amazon which can trigger a higher degree of dieback and explain also why we see less and less rain over the Amazon. But if you get more surface water stuck in the southern ocean, this can also explain why the West Antarctic ice sheet is melting faster than we had expected because you have warmer southern ocean that we had expected

19:15 because it's not flowing as it should back to the North Atlantic. So this is a reminder that the planet is a very small unit. It's complex, but it's small. It's interconnected. And what happens in one corner can impact many other parts of the planet. And it impacts all of us. So there we are. Here is the evidence sheet. Welcome to the anthroposine. We're now in the driving seat. We humans are the largest force of change on planet Earth. The holosene is the reference point. It's our garden of Eden. And tipping points are hardwired. And this is why we need to quantify the safe operating space for humanity's future on planet Earth. Scientifically, we've been able to do this. We've been working on this for the past 15 years, identifying the nine Earth system processes that regulates the stability,

20:03 the resilience, and the life support on Earth. How to keep the planet in a holosene state depends not only on the climate system but also on biodiversity on the configuration of land on the bloodstream of the planet the hological cycle uh nutrient flows of nitrogen and phosphorus the ocean stability air pollutants the stratospheric ozone layer of course novel entities is how much loading of chemicals does the earth system cope with in terms of nuclear waste microplastics p5 fast persistent organic pollutants before you get permanent changes in genetic composition of species. And all of this has now been quantified with control variables. And this is the latest assessment from or not the latest, the second most recent

20:48 assessment from 2023 showing that six of the nine boundaries are outside of the safe space. So this is a verification of why there is even more support for the concern in my first graph showing the acceleration of warming because this is exactly what you would expect that if the climate boundary because of energy flow is outside of the safe space and we are allowing ourselves to undermine the stability of the biosphere. It's not so surprising, is it, that the ocean and the biosphere on land is is starting to show signs of weakening the capacity to buffer. Moreover, we are now in a situation where we need to, you know, buckle up for a journey that looks as follows on the screen. This is the 100

21:35 or so scenarios from the IPCC that can still hold 1.5° CC at the end of this century. But it does have a period of overshoot and it breaches 1.5 somewhere between 2030 and 2035. We scientifically today consider when I say we here it's the pot institute. I should be clear about that. We consider that this is the best that science can sort of say offer today. meaning that uh the possibility of of never exceeding 1.5 is no longer possible. We can still hold 1.5 but only after a period of overshoot and overshoot is as you see a long period 30 40 50 years of up to 1.7° Celsius of warming. This leads to two conclusions. Number one is that I'm afraid to say

22:22 with very high degree of certainty that it will get worse before it potentially gets better because every tenth of a degree means more extreme events, more fierce extreme events. But the second conclusion is the following. Why would the planet come back after overshoot? And we know the answer. It's that we remove carbon with carbon dioxide removal technologies. I'll come back to that. but also that we come back into the safe space of the planetary boundaries to ensure that we do not cross tipping points that we keep the buffering capacity of the planet intact. That's why we have now started to release every year a update of the planetary boundary science and the so-called planetary health check. This is the latest version of this. It's the

23:09 same planetary boundary assessment. Here's a safe space and the safe boundary. Here you enter a danger zone in the uncertainty range of science. in the yellow space and here you enter high-risk zone. We've done it like this as blood sample example to give the communication that we're taking the planet to the doctor to do a full health check. It confirms the six of the nine boundaries are outside of the safe space. The direction of travel as you see unfortunately is still that we're moving in the wrong direction. We've not bent the curves yet. It's starting to cost. This is just headlines from 2024. The global economy is starting to really show signs of double-digit numbers of impact on GDP growth. We published recently again the Potsam Institute led by Maxmillian Kauala paper with very

23:56 standard basic climate economics showing that income levels are very likely going to be reduced by 19% by 2050 if we follow the current path as today compared to a business as usual development. So we're starting to see big costs to the global economy and we also know that now in order to have a chance of coming back after overshoot we also have to phase out the fossil fuels record fast. And here is the story of the journey. We have 200 billion tons of carbon dioxide in the remaining global carbon budget. 200 to have a 50% chance of holding 1.5 after overshoot. That is equivalent to 5 years of global emissions. It's this journey. We have to phase out fossil fuels at a pace that takes us to net zero by 2050, which is

24:44 equivalent to 5 to 10% reduction of global emissions per year. That's the pace we have to take. But we also need to transform the global agriculture system from a source to a sink. And we have to start removing carbon dioxide with carbon dioxide removal technologies at at a as you see at a record scale up to five to six to 7 billion tons of carbon dioxide per year. And then we have to secure the carbon sinks on land and in the ocean. So dear friends, this is what science gives us as the best journey. It's a global sustainability transformation. It's a planetary boundary transformation. Even if you care only about solving the climate crisis, this is the journey we have to follow. Now to close just to say, well, is this possible to achieve? Well, for

25:29 one, there's no more linear incremental journey that can take us to the right place. It's only S-curves of exponential positive trajectories. And of course we're looking for these positive big system changes today going back all the way to Everett Rogers 1960s theory of diffusion of innovation showing that when you have a good idea which is better than the incumbent when you come to roughly 20 25% of adoption you can have a takeoff point and tip over the logic also in the inert majority that tends to just sit still and not move in the right direction. So are we starting to see doubledigit adoption of decarbonized solutions? The answer is yes. And I'm just giving a few example

26:15 here. Here is the renewable energy trajectory. Look at the global south which is now passing soon 10%. The global north is starting to reach 20% soon. The global south and Africa, South Asia are actually not on linear trajectories anymore. This is often forgotten that even the global south is really moving on on a on a nonlinear exponential pathway on renewable energy. This is the classic story that we have um all started to learn about the Norwegian social tipping point on electric vehicles. Just look at this scurve. 90% of vehicles sold in Norway today are full electric. I take that again. 90%. They are they would never return to the internal combustion engine. But

27:00 remember that Denmark is also on that path. Just look at Denmark almost at 60% penetration of electric vehicles. Often I get told, well, but you know, electric vehicles, that's an easy thing. But I've just been playing around. I say playing around because this is unpublished, so let it keep stay in this room. Here are just a list of the difficult to abate sectors. I mean, we're talking steel, cement, fertilizer, plastics, chemicals, transport, food system. These are generally considered being really difficult to have any solutions for. But when you just map and talk to the industrial leaders in the world, there are solutions and they've come quite a long way. I assess it like this that you have in green areas that are starting to now be possible to commercialize,

27:46 possible to really start scaling and we're talking steel, fertilizer, food system transitions, and of course mobility. It's a race going on right now. Admittedly, you have a few difficult ones like aviation and plastics, but it's not as if this is an impossible problem to solve. So therefore, I leave you with this. We have accumulated for the first time all the planetary boundaries into one assessment. We placed the planet in our expert elicitation and all our analytics where you see the planet there. What does this tell us? It tells us number one, we are in danger. Admittedly, we are outside of the safe space for the health of the entire planet. But secondly, it also tells us we're not yet in the red zone. We're not

28:31 yet in a place where we do not have an opportunity to transition this around. And I was very inspired when Billy Isish was in Berlin just a few weeks back and um her dramatic song when the part is over making clear that the fossil fuel era is now at the beginning of the end. And I agree with that. But the scientific me message is also that the game is not over. The window is still open even though it's gradually closing or or quite rapidly closing. But we have a chance to turn this around and we have the solutions. And in the other end, we know we'll come out stronger, healthier, more secure, and more competitive in a more modern future than before. So therefore, it's so important to stand up with science today in a world that is

29:17 suddenly in a very shakeup on this agenda. Thanks for your patience. [Music]

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