Uncertainty

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In the Long Run: The Future as a Political Idea – review

Published by Anonymous (not verified) on Mon, 26/02/2024 - 10:21pm in

Jonathan White‘s In the Long Run: The Future as a Political Idea examines how changing political conceptions of the future have impacted democracy, arguing that contemporary challenges like economic slowdown and climate change have led to reactive politics and short-termism. Though the book proposes ways to revitalise democracy, Aveek Bhattacharya suggests we may need to seek beyond our political institutions for strategies to build a more open future.

You can read an interview with Jonathan White about the book here. On Monday 11 March at 6.30pm White will speak at an LSE panel event, The politics of the future – find details and register here.

In the Long Run: The Future as a Political Idea. Jonathan White. Profile Books. 2024.

In the Long Run: The Future as a Political Idea is a book about the history of the future, and what it means for the present. More precisely, it describes how the way people think about the future has evolved over time, and the impact of these changes on democracy. Jonathan White’s central argument is that while optimism for the future once helped build democracy, economic slowdown, climate change, new technology and geopolitical tension mean that “the future no longer seems its [democracy’s] friend”.

For democracy to function, White observes, it is critical that people believe an “open future” is possible: that there are alternatives to the status quo, that society can evolve in a range of different ways, and that the people can choose between them. One of the key defining characteristics of democracy – the peaceful handover of power – is premised on changeability of the future: election losers believe that they will get their chance to achieve their vision of society again.

For democracy to function, White observes, it is critical that people believe an ‘open future’ is possible

In the present, White says, it is harder to maintain that patience and faith. The future is regarded with fear and claustrophobia. At various points he describes the future, far from being open, as “closing in”. Catastrophe – societal decay, conflict, environmental collapse – feels hard to avert. Insofar as there are options, they involve deferring to technocrats. There is a “now or never” urgency about politics, and a fear that waiting your turn means leaving it too late because the other side will destroy everything.

Via a tour of historical political thinkers, White sketches the ideas of the future that make for the most vibrant democratic system. Political and social outcomes must seem open, but not in such a destabilising manner as to trigger counter-revolution from those attached to the present. A strand of utopianism can be energising but must be linked to near-term political tactics to be practicable. Efforts to limit uncertainty, to render the future predictable, through calculation and technocracy risk squeezing out the necessary imagination and mass participation of vibrant democracy. At the same time, chaotic impulsiveness and pure disregard for expertise risks descending into fascism. Trying to control the future by keeping it secret is likely to generate conspiracy theories and discontent. Consumerism individualises the future and means we no longer share in it – we move from valorising Victorian steam trains to wanting our own personal cars.

Our perpetual state of emergency, while creating unpredictability, produces reactive politics, designed mainly to return things to the way they were.

The conception of the future we have arrived at today is not, in White’s opinion, sufficiently conducive to democracy. Our perpetual state of emergency, while creating unpredictability, produces reactive politics, designed mainly to return things to the way they were. Short-termism dominates – most notably, through the election cycle, but even longer-term threats like climate change are tractable only by converting them to benchmarks and deadlines. Managerialism and secrecy dominate, empowering organisations like the European Central Bank and the International Monetary Fund and triggering impulsive populist backlashes.

White’s proposals for rebuilding a more positive conception of the future and revitalising democracy are somewhat surprising. He is sceptical of direct democracy – while more referendums might give ordinary citizens more chance to shape the future, they raise the stakes and perpetuate the “all-or-nothing” politics he thinks is so baleful. Small-scale councils are too small-scale to create significant change, citizens’ assemblies too short-lived to pursue a persistent vision.

White calls for ‘radical representative democracy’, with mass participation in the development of party policy and party members having greater opportunity to recall politicians who fail to deliver on those agreed goals.

Instead, he puts his chips on political parties as the crucibles of a more inclusive, compelling and hopeful vision of the future. He calls for “radical representative democracy”, with mass participation in the development of party policy and party members having greater opportunity to recall politicians who fail to deliver on those agreed goals. It’s an argument with echoes of Peter Mair’s Ruling the Void, which also claimed that the disengagement of ordinary members and politicians from their political parties had led to “the hollowing of Western democracy”.

White’s rebooted party system sounds good in theory, but invites scepticism about its practicality. His central assumption is that citizens’ disempowerment is the root cause of our current democratic malaise, and that the opportunity for greater influence will suffice to tempt enough people to give up their evenings and weekends to political causes. It is not encouraging that the existing parties that have done most to engage with mass movements and improve participation with things like online platforms – Podemos in Spain and the Five Star Movement in Italy – do not seem to have restored democratic confidence in their countries.

The Victorian capitalists who built the factories and railroads may not have been personally attractive, but they inspired progressives and socialists to dream about how their innovations could be used to benefit all.

White is oddly dismissive of the pockets of optimism that do exist outside the political system – most notably Silicon Valley, where ideas like “Effective accelerationism”, the view that technological progress is likely to obviate many of our deepest societal challenges, has taken root. For White, they display the wrong sort of optimism: too consumerist and individualistic, too inclined towards anti-system chaotic thinking, tendencies encapsulated in the figure of Elon Musk, presented as fascistoid, if not fascist. Setting aside whether that is a fair characterisation of Musk, the question it raises is why the confidence of tech companies seems so divorced from the sentiments of wider society. The Victorian capitalists who built the factories and railroads may not have been personally attractive, but they inspired progressives and socialists to dream about how their innovations could be used to benefit all. There are some – figures like Aaron Bastani on the far left and Derek Thompson on the centre left – that are trying to do something similar today, but White does not recognise them as such.

White assumes that the problems of democracy are endogenous: that they are caused by political institutions and must be resolved by them.

Most fundamentally, White assumes that the problems of democracy are endogenous: that they are caused by political institutions and must be resolved by them. But there are more straightforward explanations for the modern morosity. Stagnant economic growth, and the failure of new technologies to demonstrably improve living standards, would naturally be expected to undermine confidence that things will improve. The demographic shift to an older population in rich countries may also have contributed to a lack of vitality and enthusiasm, and a tendency to look back with nostalgia rather than forward with hope. Even among the young, we should not necessarily take perceptions at face value. Phenomena like “climate anxiety” seem to reflect anxiety at least as much as they reflect the climate, and as such will often be psychological, not just political in nature.

That’s not necessarily a comforting thought. Maybe technological abundance is around the corner, maybe the economy will turn around, maybe the mental health crisis will abate – whether by sheer luck or unusually effective action – and people will start to feel better about the future. But In the Long Run suggests that fixing democracy’s problems, renewing our faith in the open future, is a much bigger task than tweaking its institutions.

This post gives the views of the author, and not the position of the LSE Review of Books blog, or of the London School of Economics and Political Science.

Image credit: Ryan Rodrick Beiler on Shutterstock

Q and A with David Stainforth on Predicting Our Climate Future: What We Know, What We Don’t Know, and What We Can’t Know

Published by Anonymous (not verified) on Thu, 16/11/2023 - 11:58pm in

We speak to David Stainforth about his new book, Predicting Our Climate Future: What We Know, What We Don’t Know, and What We Can’t Know, which argues for a re-evaluation of how we go about the study of climate change in the physical sciences, the social sciences, economics and policy.

You can watch a public LSE event with David Stainforth to launch the book from October 2023 on YouTube here.

Predicting Our Climate Future: What We Know, What We Don’t Know, and What We Can’t Know. David Stainforth. Oxford University Press. 2023.

Find this book: amazon-logo

Book cover of Predicting Our Climate Future by David Stainforth showing a breaking wave inside a compass on a white background.Q: Where did the idea for the book come from and what were you setting out to do in writing it?

Between 2000 and 2015, I became aware that my perspective on what we should be trying to do in climate change science wasn’t at all reflected in the practice of research in research institutions. It seemed to me important to write something that would engage people with all the fascinating challenges that exist in understanding the problems of climate change. Doing so, I hoped, would help make clear the separation between what we know and what we don’t know.

Many big, fundamental, questions – philosophical, mathematical, physical, and economic questions – about climate change tend not to be examined, probably because of the urgency for society to act.

If I was a sixth-former now, I would certainly see climate change as an important issue for society, but I’m not sure I would be passionate about trying to understand it. That’s because it appears that we already understand it, although in fact we don’t. Many big, fundamental, questions – philosophical, mathematical, physical, and economic questions – about climate change tend not to be examined, probably because of the urgency for society to act. My book addresses these questions. I would love for my book to stimulate high-school students and undergraduates across diverse disciplines to say, actually, there’s something really fascinating to get my teeth into here; something that humanity hasn’t yet understood.

Of course, none of this undermines the importance and urgency of acting on climate change, but acting and understanding need to go hand in hand.

Q: What are the limitations of scientists’ understanding of the climate system? How do these affect our ability to predict how the climate will change?

The central issue is complexity and there are two aspects of complexity that create a barrier to predicting what the climate future will look like.

The climate system is made up of many components – the atmosphere, the oceans, land ecosystems, ocean ecosystems, biogeochemical systems, the cryosphere etc. Many of these can be broken down further into subsystems, and all of this is before you get into the social aspects. The first aspect of complexity is simply how these many disparate components interact.

Certain types of system, like the climate system, have real barriers to predictability because what happens in the future can be very sensitive to the state of the system today. This is what’s meant by the “butterfly effect”.

The second aspect of complexity is more mathematical. Certain types of system, like the climate system, have real barriers to predictability because what happens in the future can be very sensitive to the state of the system today. This is what’s meant by the “butterfly effect”. At the same time, the relationship between our models and reality is unclear: how close does a model have to be to reality for it to be able to tell us something about how reality will behave? That’s a difficult question to answer; it might be that our models could represent reality very closely, but still provide unreliable predictions. This is something that Erica Thompson has named the “hawkmoth effect”; it’s something we haven’t really begun to study.

These types of complexity affect how we should be designing our climate models and what sort of experiments we should run with them.

Q: What do Global Climate Models (GCMs) do and what are their limitations?

Global Climate Models break down the atmosphere and ocean into grid points and at each grid point they solve the equations of motion to tell us how things change over time. This is what’s known as a reductionist approach to modelling, and it allows us to work out what the state of the atmosphere or ocean system might be at some point in the future. Solving the equations on a computer can typically only tell us how things will change over about 10 minutes, so you’ve got to repeat the process millions of times to get information for 100 years ahead.

There are lots of elements of the climate system that can’t be modelled [in a reductionist] way, either because we don’t know what the fundamental equations are or because the processes take place on scales that are far too small to include in the models.

But there are lots of elements of the climate system that can’t be modelled that way, either because we don’t know what the fundamental equations are or because the processes take place on scales that are far too small to include in the models. Examples include how ecosystems absorb and release carbon dioxide and how clouds and rainfall form. For these components there are various different ways to approximate the processes at play, but it’s not easy to know how reliable these approximations are. And because all aspects of the climate system affect all the other aspects of the climate system, this means that the model predictions can’t simply be taken as predictions of reality.

Q: Why do we rely so heavily on GCMs for climate prediction and policy development today? Is there a danger in relying too heavily on these models?

When we study climate change, we don’t have multiple climates to examine. The time scales and the system are defined: it’s our real-world climate system that we’re interested in, and how it will change through the 21st century. We are doing an experiment on the real climate system through humanity’s emissions of greenhouse gases, but we’ll only ever get one result, and that will come too late to be of much use to us. The models enable us to study what we can’t study in reality – for instance, multiple possible scenarios of future greenhouse gas emissions. But we need to always remember that we’re studying a model, not reality. The power, the detail and the ubiquity of the models encourages us to avoid asking the big questions about how the model predictions relate to reality – whether what they’re telling us is actually what we think will happen.

When we study climate change, we don’t have multiple climates to examine. The time scales and the system are defined: it’s our real-world climate system that we’re interested in, and how it will change through the 21st century.

Research on climate, particularly with models, has grown out of work on weather forecasting. The reliability of weather forecasts over the last 20 to 30 years has massively improved, principally because of these models. But in the shift from weather forecasting to climate forecasting, we are dealing with a fundamentally different problem. In weather forecasting, we don’t need to get the whole of the climate system right: it’s mainly just about simulating the atmosphere. Furthermore, we repeat the weather forecasting process three or four times a day, so we can compare the model’s predictions against what happens in reality. That means we can test whether our models are doing a good job in a way that is impossible for climate predictions

With climate, you need to bring in many other elements of the climate system, including oceans and ecosystems, and we don’t have the same possibility to verify the results. This puts us in a very different domain, but the problem is that it doesn’t feel that way. It feels as though weather forecasting and climate predictions are very similar because they use similar, related models. This represents a barrier to using the models effectively to help us provide reliable information about future climate.

Q: Why do you argue that greater diversity of climate models rather than greater “realism” of climate models should be the goal for better climate prediction?

Aiming for realism tends to take us to higher and higher resolution models. These models represent atmospheric behaviour better and they look more realistic, but this lulls us into a false sense of security. Despite the “realistic” appearance of these models, we can’t tell if they are accurate because we’ve never observed the planet in the warmed state that we’re interested in.

High-resolution models also take a lot of computing time to run, and consequently they remove the possibility of exploring other uncertainties such as how we represent the carbon cycle or biogeochemical processes. There’s a substantial risk therefore that we adapt society to be resilient to the changes in our models, when what might actually happen could be very different.

If […] we were to address different ways of building our models and of accounting for the many uncertainties, this would give us a diversity of predictions.

If instead we were to address different ways of building our models and of accounting for the many uncertainties, this would give us a diversity of predictions. Having a better understanding of the wide range of different changes that could plausibly happen would enable us to be better prepared and is, in my view, crucial to building a robust response to climate change.

Q: How does the separation between disciplines, which approach the issue in very different ways, hamper our understanding of, and ability to act on, climate change?

Assessments of the economics of climate change and of the consequences for our societies, for our wealth, for our welfare etc., often don’t take sufficient account of the uncertainties in the physical science. There is a real need for economists to understand the processes of the physical sciences better.

Assessments of the economics of climate change and of the consequences for our societies, for our wealth, for our welfare etc., often don’t take sufficient account of the uncertainties in the physical science

However, if we want the physical climate sciences to help us prepare effectively for our future world, then we need to ask, what are the questions that are being addressed by agricultural scientists, by city planners, by economists and by policy makers. Only when we are clear what kind of information is being sought, can we direct the physical sciences in a useful way. At the moment, the physical scientists set the questions and pass on the resulting information to social scientists rather than focusing their experiments and models on what social scientists and society need to know most.

We are stuck in a traditional approach which is not serving society well.

Q: How could we enable greater interdisciplinary research around climate change?

We require big changes in how we do climate change research. We need to be a lot clearer about what we’re trying to address and how the connections between disciplines work. I think that means high-level change to how we study the problem.

Historically climate change research has been very siloed, as academia generally is. There is a need for the research funders to grasp the nettle of wholesale change and for universities and research institutes to come together and create career paths that enable people to research across disciplinary boundaries.

There is a need for the research funders to grasp the nettle of wholesale change and for universities and research institutes to come together and create career paths that enable people to research across disciplinary boundaries.

I don’t think the importance of multidisciplinarity for understanding fundamental features of the threats posed by climate change has been fully recognised. There are still many funding calls that are essentially answer-driven. It’s a “tell us what will happen to this bit of the system” approach, but that’s not what climate change is. You can’t tell what’s going to happen to one aspect without connecting it with everything else. It’s a big, complex problem and needs to be addressed as such.

As a starting point we need funding – 10, 20 million pounds – for a centre that can bring truly diverse researchers together from philosophy to physics to economics, and give them the stability of five to 10 years to work on these problems together. That’s the starting place for better information about our climate future. It’s also the starting place for training a cohort of experts who have both the breadth and depth of knowledge to be able to build climate resilient societies and communicate what climate change risks actually look like.

Note: This interview gives the views of the author, and not the position of the LSE Review of Books blog, or of the London School of Economics and Political Science. The interview was conducted by Anna D’Alton, Managing Editor of LSE Review of Books.

Main Image: Arctic sea ice by Kathryn Hansen / NASA on Flickr.