Dune: we simulated the desert planet of Arrakis to see if humans could survive there

Dune, the epic series of sci-fi books by Frank Herbert, now turned into a movie of the same name, is set in the far future on the desert planet of Arrakis. Herbert outlined a richly-detailed world that, at first glance, seems so real we could imagine ourselves within it.

However, if such a world did exist, what would it actually be like?

We are scientists with specific expertise in climate modelling, so we simulated the climate of Arrakis to find out. We wanted to know if the physics and environment of such a world would stack up against a real climate model.

Here’s a visualisation of our climate model of Arrakis:

You can zoom in on particular features and highlight things like temperature or wind speed at our website Climate Archive.

When we were done, we were very pleased to discover that Herbert had envisioned an environment that for the most part meets expectations. We might need to occasionally suspend disbelief, but much of Arrakis itself would indeed be habitable, albeit inhospitable.

How do you build a fantasy world like Arrakis?

We started with a climate model commonly used to predict weather and climate here on Earth. To use these sorts of models you have to decide on the physical laws (well-known in the case of planet Earth) and then input data on everything from the shape of mountains to the strength of the sun or the makeup of the atmosphere. The model can then simulate the climate and tell you roughly what the weather might be like.

We decided to keep the same fundamental physical laws that govern weather and climate here on Earth. If our model presented something completely strange and exotic, this could suggest those laws were different on Arrakis, or Frank Herbert’s fantastical vision of Arrakis was just that, fantasy.

Height map (in metres) of Arrakis.
Farnsworth et al, Author provided

We then needed to tell the climate model certain things about Arrakis, based on the detailed information found in the main novels and the accompanying Dune Encyclopedia. These included the planet’s topography and its orbit, which was was essentially circular, akin to the Earth today. The shape of an orbit can really impact the climate: see the long and irregular winters in Game of Thrones.

Finally, we told the model what the atmosphere was made of. For the most part it is quite similar to that of the Earth today, although with less carbon dioxide (350 parts per million as opposed to our 417 ppm). The biggest difference is the ozone concentration. On Earth, there is very little ozone in the lower atmosphere, only around 0.000001%. On Arrakis it is 0.5%. Ozone is important as it is around 65 times more effective at warming the atmosphere than CO₂ over a 20-year period.

Having fed in all the necessary data, we then sat back and waited. Complex models like this take time to run, in this case more than three weeks. We needed a huge supercomputer to be able to crunch the hundreds of thousands of calculations required to simulate Arrakis. However, what we found was worth the wait.

Arrakis’s climate is basically plausible

The books and film describe a planet with unforgiving sun and desolate wastelands of sand and rock. However, as you move closer to the polar regions towards the cities of Arrakeen and Carthag, the climate in the book begins to change into something that might be inferred as more hospitable.

Yet our model tells a different story. In our model of Arrakis, the warmest months in the tropics hit around 45°C, whereas in the coldest months they do not drop below 15°C. Similar to that of Earth. The most extreme temperatures would actually occur in the mid-latitudes and polar regions. Here summer can be as hot as 70°C on the sand (also suggested in the book). Winters are just as extreme, as low as -40°C in the mid-latitudes and down to -75°C in the poles.

This is counter intuitive as the equatorial region receives more energy from the sun. However, in the model the polar regions of Arrakis have significantly more atmospheric moisture and high cloud cover which acts to warm the climate since water vapour is a greenhouse gas.

gif of temperatures
Monthly temperatures on Arrakis, according to the model. Both poles have very cold winters and very hot summers.
Author provided

The book says that there is no rain on Arrakis. However, our model does suggest that very small amounts of rainfall would occur, confined to just the higher latitudes in the summer and autumn, and only on mountains and plateaus. There would be some clouds in the tropics as well as polar latitudes, varying from season to season.

The book also mentions that polar ice caps exist, at least in the northern hemisphere, and have for a long time. But this is where the books perhaps differ the most from our model, which suggests summer temperatures would melt any polar ice, and there would be no snowfall to replenish the ice caps in winter.

Hot but habitable

Could humans survive on such a desert planet? First, we must make an assumption that the human-like people in the book and film share similar thermal tolerances to humans today. If that’s the case then, contrary to the book and film, it seems the tropics would be the most habitable area. As there is so little humidity there, survivable wet-bulb temperatures – a measure of “habitability” that combines temperature and humidity – are never exceeded.

The mid-latitudes, where most people on Arrakis live, are actually the most dangerous in terms of heat. In the lowlands, monthly average temperatures are often above 50-60°C, with maximum daily temperatures even higher. Such temperatures are deadly for humans.

Four people in black rubbery suits in desert
Stillsuit models, autumn 10191 collection.
Chiabella James / Warner Bros

We do know that all humanoid life on Arrakis outside of habitable places must wear “stillsuits”, designed to keep the wearer cool and reclaim body moisture from sweating, urination and breathing to provide drinkable water. This is important as stated in the book that there is no rainfall on Arrakis, no standing bodies of open water and little atmospheric moisture that can be reclaimed.

The planet also gets very cold outside of the tropics, with winter temperatures that would also be uninhabitable without technology. Cities like Arrakeen and Carthag would suffer from both heat and cold stress, like a more extreme version of parts of Siberia on Earth which can have both uncomfortably hot summers and brutally cold winters.

It’s important to remember that Herbert wrote the first Dune novel way back in 1965. This was two years before recent Nobel-winner Syukuro Manabe published his seminal first climate model, and Herbert did not have the advantage of modern supercomputers, or indeed any computer. Given that, the world he created looks remarkably consistent six decades on.


The authors modified a well-used climate model for exoplanet research and applied it to the planet in Dune. The work was carried out in their spare time and is intended as an appropriate outreach piece to demonstrate how climate scientists use mathematical models to better understand our world and exoplanets. It will feed into future academic outputs on desert worlds and exoplanets.The Conversation

This blog is written by Cabot Institute for the Environment members, Dr Alex Farnsworth, Senior Research Associate in Meteorology and Dr Sebastian Steinig, Research Associate in Paleoclimate Modelling, University of Bristol; and Michael Farnsworth, Research Lead Future Electrical Machines Manufacturing Hub, University of Sheffield.

This article is republished from The Conversation under a Creative Commons license. Read the original article.

Violence and mental health are likely to get worse in a warming world

As heat levels increase, mental health conditions are likely to worsen.
Pxfuel

Extreme weather has been the cause of some of the biggest public health crises across the world in recent years. In many cases, these have been enhanced by human-induced climate change. For instance, in 2003, high summer temperatures in Europe were believed to cause 50,000 to 70,000 excess deaths across 16 European countries.

Globally, it’s been estimated that a total of 296,000 deaths over the past two decades have been related to heat.

But heat doesn’t just affect physical health. It can have equally serious effects on mental health conditions. Research has shown that rising temperatures are associated with an increase in suicides and in violent behaviour, as well as exacerbating mood and anxiety disorders.

Studies in England and Wales conducted between 1993 and 2003 have revealed that, when temperatures were above 18°C, every 1°C rise in temperature was associated with a 3.8% increased risk of suicide across the population.

Between 1996 and 2013 in Finland, every 1°C increase in temperature accounted for a 1.7% increase in violent crime across the country. It has even been estimated that 1.2 million more assaults might occur in the United States between 2010 to 2099 than would without climate change.

The association between high temperatures and mental health is an active area of research. Scientists have found that some health consequences of increased heat, like disturbed sleep and levels of serotonin – a hormone critical for adjusting our feelings, emotions and behaviours – might play a role in triggering the appearance of mental health conditions.

A world map coloured red, with darker areas indicating greater temperature rises (up to 6°C).
This map shows the projected changes in daily temperature extremes at 1.5°C of global warming compared to the pre-industrial period (since 1861).
Author provided

Sleep deprivation often occurs during heatwaves, which then may lead to frustration, irritability, impulsive behaviours and even violence.

Extreme temperatures, such as those observed during heatwaves, are also found to be associated with some forms of dementia and disturbed mental health states, especially for those who are already in vulnerable conditions such as psychiatric patients.

And low levels of serotonin are associated with depression, anxiety, impulsivity, aggression and occurrence of violent incidents.

Implications

In the future, heatwaves will be hotter and last longer. Temperature records are likely to be broken ever more frequently as the world continues to warm. In north-west Asia, for example, temperatures could increase by 8.4°C by 2100.

A world that is on average 1.5°C warmer will see many average regional temperatures rise by more than this. This problem is compounded as the population – and therefore the number of people living in cities – increases. By 2050, it is projected that two thirds of the world’s population will live in urban areas.

A city in summer
Cities are often hotter than rural regions, exacerbating negative mental health effects caused by heat.
PedroFigueras/Pixabay

Urban environments are known to be warmer than their rural surroundings, a phenomenon known as the “urban heat island”. Climate projections show not only that cities will warm faster than rural areas, but that this effect is increased at night. This may further exacerbate the effects of heat extremes on our sleep.

Both adaptation to and mitigation of climate change will be necessary to lessen these potentially devastating effects as much as possible.

Options for adapting our lives to a warmer world could include increasing air circulation within buildings and adjusted work hours in times of extreme heat. Paris, for example, has already created a network of “cool islands”: green and blue spaces such as parks, ponds and swimming pools which provide places to seek refuge from the heat.

Most simply, educating people on the potential impacts of heat on mental health, aggression and violence – allowing them to understand exactly why it is so important to support initiatives that help keep our planet cool – could support better mental health at the same time as fighting the climate crisis.

—————————————–The Conversation

This blog is written by Cabot Institute for the Environment members Dr Mary Zhang, Senior Research Associate in Policy Studies, University of Bristol; Professor Dann Mitchell, Associate Professor in Atmospheric Sciences, University of Bristol, and Dr Vikki Thompson, Senior Research Associate in Geographical Sciences, University of Bristol

This article is republished from The Conversation under a Creative Commons license. Read the original article.

Dann Mitchell
Mary Zhang
Vikki Thompson

 

 

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What Europe’s exceptionally low winds mean for the future energy grid

 

Shaggyphoto / shutterstock

Through summer and early autumn 2021, Europe experienced a long period of dry conditions and low wind speeds. The beautifully bright and still weather may have been a welcome reason to hold off reaching for our winter coats, but the lack of wind can be a serious issue when we consider where our electricity might be coming from.

To meet climate mitigation targets, such as those to be discussed at the upcoming COP26 event in Glasgow, power systems are having to rapidly change from relying on fossil fuel generation to renewables such as wind, solar and hydropower. This change makes our energy systems increasingly sensitive to weather and climate variability and the possible effects of climate change.

That period of still weather badly affected wind generation. For instance, UK-based power company SSE stated that its renewable assets produced 32% less power than expected. Although this may appear initially alarming, given the UK government’s plans to become a world leader in wind energy, wind farm developers are aware these low wind “events” are possible, and understanding their impact has become a hot topic in energy-meteorology research.

A new type of extreme weather

So should we be worried about this period of low wind? In short, no. The key thing here is that we’re experiencing an extreme event. It may not be the traditional definition of extreme weather (like a large flood or a hurricane) but these periods, known in energy-meteorology as “wind-droughts”, are becoming critical to understand in order to operate power systems reliably.

Recent research I published with colleagues at the University of Reading highlighted the importance of accounting for the year-to-year variability in wind generation as we continue to invest in it, to make sure we are ready for these events when they do occur. Our team has also shown that periods of stagnant high atmospheric pressure over central Europe, which lead to prolonged low wind conditions, could become the most difficult for power systems in future.

Climate change could play a role

When we think about climate change we tend to focus much more on changes in temperature and rainfall than on possible variations in near-surface wind speed. But it is an important consideration in a power system that will rely more heavily on wind generation.

The latest IPCC report suggests that average wind speeds over Europe will reduce by 8%-10% as a result of climate change. It is important to note that wind speed projections are quite uncertain in climate models compared with those for near-surface temperatures, and it is common for different model simulations to show quite contrasting behaviour.

Colleagues and I recently analysed how wind speeds over Europe would change according to six different climate models. Some showed wind speeds increasing as temperatures warm, and others showed decreases. Understanding this in more detail is an ongoing topic of scientific research. It is important to remember that small changes in wind speed could lead to larger changes in power generation, as the power output by a turbine is related to the cube of the wind speed (a cubic number is a number multiplied by itself three times. They increase very fast: 1, 8, 27, 64 and so on).

World map with dark blue (less wind) in Europe, North America and China
Change in wind speed compared to 1986-2005 if we were to limit global warming to 1.5C. Areas in blue will have less wind; areas in green, more wind.
IPCC Interactive Atlas, CC BY-SA

The reductions in near-surface wind speeds seen in the above map could be due to a phenomenon called “global stilling”. This can be explained by the cold Arctic warming at a faster rate than equatorial regions, which means there is less difference in temperature between hot and cold areas. This temperature difference is what drives large-scale winds around the globe through a phenomenon called thermal wind balance.

With all the talk of wind power being the answer to our energy needs, amid spiralling gas prices and the countdown to COP26, the recent wind drought is a clear reminder of how variable this form of generation can be and that it cannot be the sole investment for a reliable future energy grid. Combining wind with other renewable resources such as solar, hydropower and the ability to smartly manage our electricity demand will be critical at times like this summer when the wind is not blowing.The Conversation

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This blog was written the Cabot Institute for the Environment member Dr Hannah Bloomfield, Postdoctoral Researcher in Climate Risk Analytics, University of BristolThis article is republished from The Conversation under a Creative Commons license. Read the original article.

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Ecological decline: an overlooked emergency?

A blue tit landing. Image credit: Adam Hearne, Student at the University of Bristol.
The words ‘Ecological Emergency’ are appearing in an increasing number of environmental declarations, strategies and parliamentary bills. This blog will discuss the need to recognise ecological decline as an emergency in its own right, as well as being an element of the climate emergency. This will be part of an ‘Ecological Emergency’ Cabot Campaign which will run alongside the United Nations Convention on Biological Diversity (COP15), which is happening this week.

Last year, The Cabot Institute for the Environment’s home city Bristol became the first major city to declare an ecological emergency. This declaration came only two years after Bristol became the first European city to declare a climate emergency. Many UK councils and organizations have since declared joint “Climate and Ecological” emergencies, and the Climate and Ecological Emergency Bill has been put forward to replace the ‘outdated’ 2008 Climate Change Act. These declarations show that while climate and ecology are intrinsically linked, there is increasing recognition of ecological decline as an emergency in its own right as well as being a consequence of and contributor to the climate emergency. Climate mitigation is fundamental to safeguarding ecosystems, however, ecological decline could continue alongside decarbonisation and even be exacerbated by the means to get to net-zero, if the ecological emergency is overlooked in sustainability strategies and policy.

The UN Convention on Biodiversity (COP15) is taking place this week and a Cabot Campaign on the ‘Ecological Emergency’ will run alongside it. The campaign will include a series of blogs and posts across our website and social media. Using statements from Cabot researchers in relevant fields, this blog will discuss the ecological emergency and the need for targeted action.

 

Bristol suspension bridge. Image credit: Meg Barstow, Postgraduate Student at the University of Bristol.
 
What is the ecological emergency?

Biodiversity is being lost on a scale not seen since the last mass extinctionDr Chris Clements Caboteer and leader of the experimental conservation group explains. While Dr Andrew Flack, an environmental and animal historian, described the ecological emergency as “among the most profound crises of our time, diminishing not only planetary diversity but also the very experience of being human on our beautiful, rich planet“.

More quantitively, the statistics which drove Bristol’s pioneering ‘Ecological Emergency’ declaration include:

  • 60% of the worlds wild animals have been lost since 1970
  • One in seven UK wildlife species are at risk of extinction
  • More locally in Bristol and the surrounding areas, swift and starling populations have dropped by more than 96% since 1994
  • 41% of insects are threatened with extinction, posing a huge threat to our global food supply due to 75% of our crops being reliant on pollination by insects
  • Three-quarters of land and two-thirds of marine environment have been significantly altered by human actions
 
A honey bee on a flower. Image credit: Callum Mclellan, Student at the University of Bristol.

In their statements, many of our academics highlighted that, as well as the beauty of the natural world and our responsibility to preserve it, our reliance on ecosystems makes their survival essential to our own. Ecosystems provide us with food, oxygen, nutrient cycling, carbon absorption, air and water purification, and protection from erosion, floods and droughts. Many of these services are already under increased pressure due to climate change, which ecological decline is intertwined with. Destruction of ecosystems and exploitation of wildlife can also cause the emergence of infectious disease, as has been demonstrated by the occurrence of the current COVID-19 pandemic. Biodiversity loss and climate action failure both earned their own place in the top five threats to humanity in the next five years, according to the 2020 Global Risks Report from the World Economic Forum. Though these interdependent crises will drastically affect everyone, their consequences will not be felt equally among communities and are sadly already intensifying inequality and poverty.

Intertwined emergencies

 “The climate emergency is certainly exacerbating the ecological emergency” Professor Jane Memmott, a leading restoration ecologist, explained. Under current trends, climate change is projected to drive many ecosystems to collapse. Simultaneously, large-scale destruction of ecological carbon sinks, such as forests, wetlands and mangroves, is contributing to climate change. There are several feedback loops at play: destruction of carbon sinks is increasing atmospheric CO2, which drives climate change and in turn further ecological degradation, which then further debilitates natures ability to store carbon. This forms a vicious cycle, with profound consequences for the planet.

The interdependent emergencies share similar causes, consequences and solutions, however, Dr Tommaso Jucker, whose research is on forests and their responses to rapid global change, explains “it is not only climate change that threatens biodiversity, and the effects of biodiversity loss on people will not just be a subset of those brought on by climate change”. As well as climate change, threats to ecosystems include species over-exploitation, habitat destruction, pesticides and pollution of land, air and water. These could all continue simultaneously to our efforts to decarbonise, and even be exacerbated by the means to get to net-zero, if the ecological emergency is overlooked in sustainability strategies.
 
A forest. Image credit: Dr. Stephen Montgomery, Senior Research Fellow at the University of Bristol

A coordinated approach to climate and ecology

The climate emergency is becoming mainstream conversation and it is now widely accepted that huge changes in policy, infrastructure and behaviour are needed. However, while the climate emergency is gaining recognition, the ecological emergency is comparatively overlooked. If we are to avoid ecological collapse, a co-ordinated approach to the crises is essential; focusing purely on technological advancement and decarbonisation runs the risk of allowing and even exacerbating further ecosystem destruction.

Natural climate solutions, such as strategic management of forests, grasslands and wetlands, can offer around a third of the climate mitigation required by 2030 to keep warming below 2 °C. These environments are not only carbon sinks, but biodiversity havens, making them effective solutions for ecological decline as well as climate change. Protecting ecosystems is also often significantly more cost-effective than human-made climate interventions. However, due to our often unnatural lifestyles and a fast-growing population, nature alone will not be enough to mitigate human impact on the environment.  

A peacock butterfly. Image credit: Sam J. England, PhD Student at the University of Bristol.

The need for targeted action 

As well as the intrinsic links and coordinated solutions to the climate and ecological emergencies, there is a lot that can be done to specifically alleviate the ecological emergency. This is exemplified by Bristol’s ‘One City Ecological Emergency Strategy‘ which predominantly focuses on land management, pesticide use, water quality and consumption of products that undermine global ecosystems. This is in addition to climate mitigation, already covered in the Climate Emergency Action Plan.

Last year’s UN Summit for Biological Diversity saw leaders from all regions of the world take the ‘Leader’s Pledge for Nature’, which commits to reversing alarming global biodiversity loss trends by 2030. To achieve this ambitious but necessary goal, both climate action and targeted conservation and restoration strategies will be needed on both a local and global level. For these crises to be mitigated, some uncomfortable truths surrounding lifestyles many have become accustomed to will have to be faced.

The word ‘emergency’ from a scientific perspective 

Despite widespread agreement on the obvious threats posed by biodiversity loss and the need for action, the word ‘emergency’ can be controversial, especially amongst the scientific community. Professor Richard Wallexplained “As a research scientist, my view is that the sound-bite ‘ecological emergency’ is not sufficiently nuanced to be useful in scientific discourse and is best left to journalists and campaigners; it has no scale or quantification and what constitutes an ‘emergency’ is highly subjective.”

Public awareness surrounding our changing climate and declining ecosystems are important, however, if action doesn’t follow declarations, then they run the risk of being no more than empty PR stunt and can increase public immunity to the word as well as the impacts of the crisis itself. COP15, which is happening this week, will be pivotal in deciding the future of our own species, as well as all the other species that share our planet.

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This blog was written by Hilary McCarthy, a University of Bristol PhD Student and part of the Cabot Communicators group.

Thank you to University of Bristol students and staff for wildlife photography submissions used in this blog and across the campaign: Adam Hearne (UoB student and wildlife photographer, www.adamhearnewildlife.co.uk, Instagram: @adamhearnewildlife) Meg Barstow (UoB student, wildlife photographer, Instagram: @cardboard.rocket)
Dr Stephen Montgomery (Senior Research Fellow, Neurobiology and Behaviour, School of Biological Sciences) Sam J. England (PhD student researching aerial electroreception in insects and wildlife photographer, Instagram @sam.j.england, https://www.samjengland.com)

 

Time for policymakers to make policies (and to learn from those who are)

From a social scientist’s point of view, the recent IPCC report and the reception it has received are a bit odd. The report certainly reflects a huge amount of work, its message is vital, and it’s great so many people are hearing it. But not much in the report updates how we think about climate change. We’ve known for a while that people are changing the climate, and that how much more the climate changes will depend on the decisions we make.

What decisions? The Summary for Policymakers— the scientists’ memo to the people who will make the really important choices—doesn’t say. The words “fossil fuel”, “oil”, and “coal” never even appear. Nor “regulation”, “ban”, “subsidy”, or “tax”. The last five pages of the 42-page Summary are entitled “Limiting Future Climate Change”; but while “policymakers” appear, “policies” do not.

This is not the fault of the authors; Working Group I’s remit does not include policy recommendations. Even Working Group III (focused on mitigation) is not allowed to advocate for specific choices. Yet every IPCC contributor knows the most important question is which emission pathway we take, and that will depend on what policies we choose.

Which is why it’s so odd that big policy issues and announcements get comparatively little airtime (and research funding). For example, in June, the European Union codified in law the goal of reducing its greenhouse gas emissions 55% by 2030 (relative to 1990), and last month the European Commission presented a set of ambitious proposals for hitting that target. As a continent, Europe is already leading the world in emission reductions (albeit starting from a high level, with large cumulative historical emissions), and showing the rest of the world how to organize high-income societies in low-carbon ways. But the Commission’s proposals—called “Fit for 55”—have gone largely under the radar, not only outside of the EU but even within it.

The proposals are worth examining. At least according to the Commission, they will make the EU’s greenhouse gas emissions consistent with its commitments under the Paris Agreement. (Independent assessments generally agree that while a 55% reduction by 2030 won’t hit the Paris Agreement’s 1.5˚ target, it would be a proportionate contribution to the goal of limiting global heating to no more than 2˚.) And they will build on the EU’s prior reduction of its territorial emissions by 24% between 1990 and 2019.

A change of -24% over that period, and -18% for consumption emissions, is in one sense disappointing, given that climate scientists were warning about the need for action even before 1990. But this achievement, inadequate though it may be, far exceeds those of other high per-capita emitters, like the U.S. (+14%), Canada (+21%), or Australia (+54%).

The most notable reductions have been in the areas of electricity generation and heavy industry—sectors covered by the EU’s emissions trading system (ETS). Emissions from buildings have not declined as much, and those from transportation (land, air, and marine) have risen. Several of the Fit for 55 proposals therefore focus on these sectors. Maritime transport is to be incorporated into the ETS; free permits for aviation are to be eliminated; and a new, separate ETS for fuels used in buildings and land transport is to be established. Sales of new cars and trucks with internal combustion engines will end as of 2035, and increased taxes will apply to fuels for transport, heat, and electricity.

The Commission also proposes to cut emissions under the ETS by 4.2% each year (rather than 2.2% currently); expand the share of electricity sourced from renewables; and set a stricter (lower) target for the total amount of energy the EU will use by 2030—for the sake of greater energy efficiency.

All of this is going to be hugely contentious, and it will take a year or two at least for the Commission, the member-states, and the European Parliament to negotiate a final version. Corporate lobbying will shape the outcome, as will public opinion (paywall).

Two of the most interesting proposals are meant to head off opposition from industry and voters. A carbon border adjustment mechanism will put a price on greenhouse gases emitted by the production abroad of selected imports into the EU (provisionally cement, fertiliser, iron, steel, electricity, and aluminium). This will protect European producers from competitors subject to weaker rules. A social climate fund, paid for out of the new ETS, will compensate low-income consumers and small businesses for the increased costs of fossil fuels—thereby preventing any rise in fuel poverty.

No country is doing enough to mitigate emissions. But Fit for 55 represents the broadest, most detailed emissions reductions plan in the world—and, in some form, it will be implemented. Decision-makers everywhere should be studying, and making, policies like this.

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This guest blog is by friend of Cabot Insitute for the Environment and PLOS Climate Academic Editor Malcolm Fairbrother. Malcolm is a Professor of Sociology at Umeå University (Sweden), the Institute for Futures Studies (Stockholm), and University of Graz (Austria). Twitter: @malcolmfair. This blog has been reposted with kind permission from Malcolm Fairbrother. View the original blog.

Top image credit: Cold Dawn, Warm World by Mark McNestry, CC BY 2.0

 

The COP26 Goals and Small Island Developing States

Small Island Developing States (SIDS) have had a giant impact on international climate negotiations. As part of the Alliance of Small Island States and the High Ambition Coalition, SIDS have pushed for the 1.5°C Paris Agreement target through their tagline “1.5°C to stay alive” as well as their advocacy for loss and damage and climate adaptation finance. Without them, the Paris Agreement would not be nearly as ambitious [1], and there would not be the focus on the 1.5°C temperature goal to the extent there is today. SIDS are amongst the countries on the frontline of the climate emergency, whilst being some of the least responsible for greenhouse gases causing anthropogenic climate change.

But SIDS have not sat back quietly whilst their future becomes more uncertain. They are fighting for the assurances of climate mitigation from the rest of the world to help ensure their habitable future.

As part of this year’s United Nations Climate Conference COP26, four goals have been set to drive forward ambition to tackle the climate emergency. Here are four reasons why achieving these goals is not only crucial for the future of humanity, but especially for SIDS.

1. Secure global net zero by mid-century and keep 1.5°C within reach

SIDS have long been champions of the 1.5°C goal, underlining the science that demonstrates that limiting warming to 2°C would be inadequate to ensure a habitable future for some small island states. Following the 2018 IPCC report looking at the impacts of a world at 1.5°C and 2°C, a 1.5°C global temperature rise in SIDS would already lead to [2]:

    ↑ More intense rainfall events

    ↑ More extreme heat

    ↑ Longer and more extreme drought

    ↑ Increased flooding

    ↑ Freshwater stress

    ↑ Significant loss of coral reefs

    ↑ Sea level rise

Any increase greater than 1.5°C would compound and exacerbate these risks further and could lead to the loss of ancestral homelands for thousands of people in low-lying islands such as the Maldives or Kiribati. For other islands, there would be severe impacts on lives and livelihoods. To highlight just one example, communities in small islands often rely on coral reefs for food, storm protection and tourism (to name but a few of the many reasons coral reefs are critical to coastal communities all over the world). But at 2°C warming, 99% of coral reefs are likely to perish [2]. For some small islands it really is “1.5°C to stay alive”.

2. Adapt to protect communities and natural habitats

Adaptation will be required in SIDS to help communities adjust to the consequences of a more extreme climate. From coral reef and mangrove restoration in the Caribbean, to early warning systems in the Pacific, adaptation strategies in SIDS are accelerating, but this must be aided by appropriate finance and support. The United Nations proposes that at least 50% of climate finance should be spent on building resilience and adaptation, but financial capital is currently the key limiting factor for adaptation in SIDS. Mobilising finance to boost adaptation projects would be the first step up a long ladder in assisting SIDS facing the steep cost of adapting to a climate they did not create.

3. Mobilise finance

Developing nations such as those in SIDS need financial assistance from developed economies to fund adaptation and the transition to a greener future. This is entirely reasonable considering that developed nations have built their economies using fossil fuels, of which the consequences are a) already impacting SIDS today and b) not an option to fuel sustainable development. Developed countries pledged to raise at least $100billion annually by 2020 to support developing countries with adaptation and mitigation, but in 2018 just $78.9billion had been mobilised [3]. Even if this $100billion is attained it would still be vastly insufficient, considering estimated costs of adaptation in developing countries will be $280-500billion in 2050 [4].

But what about the communities or entire islands who cannot adapt? SIDS have also been key advocates for loss and damage reparations, seeking compensation for their inequitable experience of climate-related disasters and for the loss and damages that cannot be recovered or adapted against. Broadly speaking, this refers to climate-related loss and damages – such as those from weather and hazard events we know are being made more likely and more severe by climate change – as well as helping to avoid future loss and damage through adequate risk reduction and adaptation.

In whichever form these reparations come, it is vital that they come faster and with bolder ambition.

4. Work together to deliver ambition into action

Small Island Developing States cannot combat the climate emergency alone. After all, the very reason for the extreme injustice of climate change in SIDS is that they have done little to cause the problem that they are bearing the consequences of. To put this in context, SIDS are responsible collectively for less than 1% of global greenhouse emissions [5]. This is where governments, business, and civil society from all over the world come in. SIDS (and the entire planet, frankly) need all countries to come forward with robust plans and targets for slashing emissions by at least 50% by 2030 and reaching net zero by 2050, as well as agreeing to mobilise finance to support adaptation against the damage we have already locked in.

Time is ticking. Let’s ensure these goals are achieved at COP26 to help speed up our race against the clock, so that we can safeguard a habitable future for SIDS, for ourselves and the planet.

References

[1] Ourbak, T. & Magnan, A. K. The Paris Agreement and climate change negotiations: Small Islands, big players. Regional Environmental Change vol. 18 2201–2207 (2018).

[2] Hoegh-Guldberg, O. et al. Chapter 3: Impacts of 1.5oC global warming on natural and human systems. in Global warming of 1.5°C. An IPCC Special Report on the impacts of global warming of 1.5°C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, (ed. Intergovernmental Panel on Climate Change) 175–311 (Intergovernmental Panel on Climate Change, 2018).

[3] OECD. Climate Finance Provided and Mobilised by Developed Countries in 2013-18. OECD https://www.oecd-ilibrary.org/finance-and-investment/climate-finance-provided-and-mobilised-by-developed-countries-in-2013-18_f0773d55-en (2020) doi:10.1787/F0773D55-EN.

[4] United Nations Environment Programme. Adaptation Gap Report 2020. https://www.unep.org/resources/adaptation-gap-report-2020 (2020).

[5] Thomas, A. et al. Climate Change and Small Island Developing States. Annual Review of Environment and Resources 45, (2020).

Header image: Leigh Blackall (CC BY 2.0)

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This blog is written by Cabot Institute for the Environment member Leanne Archer, School of Geographical Science, University of Bristol. Leanne is a NERC GW4+ PhD student interested in disaster risk in Small Island Developing States, investigating how flood inundation estimates could be improved in small islands under current and future climate change. You can follow Leanne on Twitter @leanne_archer_

Airport towns like Luton and Hounslow are suffering as people fly less often – here’s how to help them

Thousands of aircraft were grounded during the pandemic. Now research is showing people might fly less.
JetKat/Shutterstock

Tens of thousands of aircraft have been grounded for well over a year due to the pandemic. In April 2020 air travel around the world was cut by 94% from April 2019. By June 2021 it was still 60% down on June 2019 thanks to holidays being cancelled, work trips shelved, and long-planned journeys to see family and friends moved to another time.

Never has any global industry collapsed with such speed. In climate terms, this has been a cause for celebration. It has represented a chance for reducing emissions that contribute significantly to climate change and pollute our air.

Some people who live close to an airport may also have welcomed the drop in noise. But many others will be worrying about the effect the long-term reduction in air travel may have on their community’s economy.

Will the industry bounce back?

Industrial bodies estimate that it might take five years for passenger demand to return to pre-pandemic levels. That’s a longer expected recovery than any other mode of transport. Globally, an estimated 46 million jobs have been deemed at risk. This isn’t just pilots or cabin crew; it’s also those who screen your baggage or make your lunch.

But will the air industry even bounce back in five years? Research our team conducted in early 2021 in Bristol, an English city with an airport and a century-old aviation industry, found that close to 60% of those surveyed expect to fly less in the future. Many of our respondents gave climate change and the pandemic as equally important reasons. Other polling has shown that many elsewhere remain wary of flying in the future too.

Businesses may also operate differently. Polling has found that four in ten business travellers are likely to fly less in the future. Business-class seats are an important part of airline income – on some flights corporate travel can represent 75% of revenue.

Setting aside ideas about electric planes for now, it seems obvious that we will need to fly less to move to a zero-carbon economy. Two-thirds of people want a post-pandemic economic recovery to prioritise climate change. This means fewer planes, and fewer jobs for crew and baggage handlers and so on.

Rebuilding communities

The decline of older industries such as mining, textiles or pottery resulted in high unemployment in towns which were massively dependent on one of them. We are all familiar with how the closure of a local pit or car plant caused the decline of once vibrant towns, leaving a generation to struggle with unemployment and the need to retrain.

Steel mills were nestled deep in the fabric of nearby communities. Their closure removed the pivot around which lives, work and leisure were based. So with the pandemic, whole communities are at risk of a similar economic decline.

In summer 2020 the rate of those jobless (be it unemployed or on furlough) was higher in areas near UK airports. In Hounslow (near London Heathrow) this was 40% of the population – with an estimated £1 billion loss to the borough’s economy. At Gatwick airport in 2020, there were job losses for 40% of its workforce, many of whom live in nearby towns such as Crawley.

Hounslow in west London
Towns like Hounslow are highly dependent on the nearby airport for employment.
BasPhoto/Shutterstock

Many towns and communities are economically dependent on nearby airports. Luton Airport is estimated to have sustained over 27,000 jobs (directly and indirectly) and is a major employer in the region. The decline of the sector has broader effects on subsidiary industries too, such as taxis, maintenance, catering and hotels.

So what is to be done? The Green Jobs Taskforce, an industry and government initiative set up in 2020 to look at future employment, has called on the UK government to invest in jobs related to wind turbines, electric trains and replacing gas boilers.

Any version of a green new deal is necessarily a job-heavy economy, with a great deal of work needed to alter the infrastructure that powers our current lifestyle. The UK government’s Ten Point Plan for Green Industrial Revolution pledges 250,000 green jobs. The political question here is whether politicians and policymakers will be brave enough to resist a bounce back for aviation and invest in a longer term future for these airport towns, to avoid them suffering a decade of decline.

This is likely to see aviation jobs lost, and will require very targeted support for cities or regions reliant on airport employment. To build back better, a green recovery must seek to support these communities and provide them with new opportunities and livelihoods.The Conversation

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This blog was written by Cabot Institute for the Environment members Dr Ed Atkins, Lecturer, School of Geographical Sciences, University of Bristol and Professor Martin Parker, Professor of Organisation Studies, University of BristolThis article is republished from The Conversation under a Creative Commons license. Read the original article.

Martin Parker
Ed Atkins

Sit down and wake up! On Buddhist theory and planetary crisis

Mention Buddhism and you’ll often get a response shaped by its recent commodification into a self-care trend. Mindfulness apps, cheerful Buddha incense holders and the Life Changing Magic of Tidying Up have led many to assume that Buddhism, like deep breathing and scented candles is primarily a technique for managing stress. Do I even need to tell you that these assumptions are wide off the mark? Probably not, yet even those who are aware ‘Buddhism’ goes deeper than these stereotypes may be surprised to hear it paired in the same sentence with ‘post-humanism’ ‘decoloniality’ ‘deconstruction’ and even ‘anarchism’.

Yet I’m about to embark on research linking just these streams of thought. This October I’ll be studying for the MSc Society & Space with plans to continue to PhD study through the ESRC 3+1 route in 2021. My research will ask how Buddhism can help us reconceive the politics of the more-than-human world in an age of planetary crisis. Buddhist thought has a unique contribution to make here, yet it’s frequently overlooked as a source of theory for approaching these questions (and other social science questions more generally).

A statue of Jizo (Kṣitigarbha) or the Earth-Womb boddhisattva glimpsed through a doorway at the Koya-san temple complex in Kansai region, Japan.

Just like other non-Western philosophies, perceptions of Buddhism have been framed through the colonial encounter. Whilst nineteenth century explorers to Tibet, China, India and Japan, did much to inspire fascination with ‘Oriental religions’, early translations of Buddhist texts often understood Buddhism through a Christian lens, equating the Buddha with Jesus. This, and the general imperial refusal to take other ways of thought and life seriously have ensured that Buddhism is yet to receive much serious academic attention outside of religious studies and history departments.

For this reason alone, Buddhist perspectives can and should be mobilised as a source of decolonising critique. But it’s not just valuable as a perspective from which to criticise.  Contemporary Buddhisms brought to the West by Tibetan refugees and modern Japanese scholars such as D.T. Suzuki from the 1950s onwards have demonstrated the breadth, diversity and originality of Buddhist scholarship and practice. And more recently, excellent work has been carried out demonstrating historical Buddhism’s clear pertinence to contemporary philosophical and political concerns more broadly.

In fact many of most disruptive (and productive) concepts shaping contemporary humanities study today were anticipated by Buddhist thought by literally thousands of years. Put it this way – if names like Derrida, Deleuze, Whitehead, Latour, and Stengers are more familiar to social scientists today than Nagarjuna, Dogen, and Candrakirti this is not because the latter have nothing relevant to say on topics such as deconstruction, non-representational theory, subjectivity and self, embodiment, the symbolic order or the production of knowledge (although of course the way they mobilise and describe these concepts is completely different.)

Post-human concepts of relational networks and assemblages, which have so radically re-shaped geographical approaches to understanding human/environment relations, find close resonance in pratitya samutpada, or the doctrine of mutual causality, an ontology of radical relation. Pratitya samutpada sees reality as process – patterns of self-organising physical and psychological events which have no fixed structure or semiotics. This interdependence logically implies an ethic of care and kind-heartedness (towards all sentient beings), a cornerstone of Buddhist practice common to all traditions.

A moment of contemplation at the D.T. Suzuki centre in Kanazawa, Japan.

In an age of climate crisis the ethical imperative to try to relieve suffering is being interpreted increasingly to include ecological care for the more-than-human world (including heterogenous and complex ‘sentient beings’ such as watersheds, bio-regions and radioactive waste) and the resulting politics of this ‘Eco-dharma’ have many similarities to activisms inspired by deep ecology, indigenous, ecofeminist and anarchist philosophies. This global wave of ecologically-informed Buddhist practice is the starting point for my research, but I’m hoping to use it as a springboard for bringing Buddhist critique into geography more generally – applying Buddhist ideas to questions of political ecology, inter-species relationships, care-giving, and environmental governance.

Hopefully, I’ll be able to disrupt some assumptions along the way – including the idea that Zen is primarily concerned with minimalist interior design and esoteric catchphrases. For me, it offers something much more radical and ultimately subversive – a philosophical commitment to experiment with risky ideas and relentlessly question the foundations of your knowledge (as well as a strong suggestion to not take yourself too seriously, and to always be prepared for absurdity and impossibility!) I hope that these will be useful qualities for a new postgraduate researcher to bring into their academic practice and I’m sure that both Deleuze and Nagarjuna would agree.

And of course, Buddhist psychology and meditative practice do offer highly effective methods for understanding the mind, cultivating equanimity and un-learning habitual patterns of thought. It’s exactly this refusal to sit neatly in disciplinary boxes that makes Buddhism such a fascinating area of study – a philosophy of the mind and world which is simultaneously theory and practice. Buddhism asks us to move beyond dualisms of self/world, human/non-human and thought/reality which is exactly why its perspectives are essential to understanding our entangled, inter-dependent and precarious life in the age of the Anthropocene. It offers us an injunction to both sit down (learn to change your mind through meditation) and wake up (liberate yourself through taking ethical action), demonstrating beautifully Marx’s dictum that the true purpose of philosophy is not just to interpret the world, but to change it.

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This blog is written by Cabot Institute for the Environment member Courtenay Crawford who is undertaking a new MSc and PhD project, funded by an ESRC 1+3 grant through the South West Doctoral Training Partnership. This blog was reposted with kind permission from the Bristol Centre for Environmental Humanities. Read the original blog.

Courtenay Crawford

Five satellite images that show how fast our planet is changing

 

Stocktrek Images, Inc. / Alamy

You have probably seen satellite images of the planet through applications like Google Earth. These provide a fascinating view of the surface of the planet from a unique vantage point and can be both beautiful to look at and useful aids for planning. But satellite observations can provide far more insights than that. In fact, they are essential for understanding how our planet is changing and responding to global heating and can do so much more than just “taking pictures”.

It really is rocket science and the kind of information we can now obtain from what are called Earth observation satellites is revolutionising our ability to carry out a comprehensive and timely health check on the planetary systems we rely on for our survival. We can measure changes in sea level down to a single millimetre, changes in how much water is stored in underground rocks, the temperature of the land and ocean and the spread of atmospheric pollutants and greenhouse gases, all from space.

Here I have selected five striking images that illustrate how Earth observation data is informing climate scientists about the changing characteristics of the planet we call home.

1. The sea level is rising – but where?

Map showing global sea level rise
The sea is rising quickly – but not evenly.
ESA/CLS/LEGOS, CC BY-SA

Sea level rise is predicted to be one of the most serious consequences of global heating: under the more extreme “business-as-usual” scenario, a two-metre rise would flood 600 million people by the end of this century. The pattern of sea surface height change, however, is not uniform across the oceans.

This image shows mean sea level trends over 13 years in which the global average rise was about 3.2mm a year. But the rate was three or four times faster in some places, like the south western Pacific to the east of Indonesia and New Zealand, where there are numerous small islands and atolls that are already very vulnerable to sea level rise. Meanwhile in other parts of the ocean the sea level has barely changed, such as in the Pacific to the west of North America.

2. Permafrost is thawing

Source: ESA

Permafrost is permanently frozen ground and the vast majority of it lies in the Arctic. It stores huge quantities of carbon but when it thaws, that carbon is released as CO₂ and an even more potent greenhouse gas: methane. Permafrost stores about 1,500 billion tonnes of carbon – twice as much as in the whole of the atmosphere – and it is incredibly important that carbon stays in the ground.

This animation combines satellite, ground-based measurements of soil temperature and computer modelling to map the permafrost temperature at depth across the Arctic and how it is changing with time, giving an indication of where it is thawing.

3. Lockdown cleans Europe’s skies

Source: ESA

Nitrogen dioxide is an atmospheric pollutant that can have serious health impacts, especially for those who are asthmatic or have weakened lung function, and it can increase the acidity of rainfall with damaging effects on sensitive ecosystems and plant health. A major source is from internal combustion engines found in cars and other vehicles.

This animation shows the difference in NO₂ concentrations over Europe before national pandemic-related lockdowns began in March 2020 and just after. The latter shows a dramatic reduction in concentration over major conurbations such as Madrid, Milan and Paris.

4. Deforestation in the Amazon

Credits: ESA/USGS/Deimos Imaging

Tropical forests have been described as the lungs of the planet, breathing in CO₂ and storing it in woody biomass while exhaling oxygen. Deforestation in Amazonia has been in the news recently because of deregulation and increased forest clearing in Brazil but it had been taking place, perhaps not so rapidly, for decades. This animation shows dramatic loss of rainforest in the western Brazilian state of Rondonia between 1986 and 2010, as observed by satellites.

5. A megacity-sized iceberg

Source: ESA

The Antarctic Ice Sheet contains enough frozen water to raise global sea level by 58 metres if it all ended up in the ocean. The floating ice shelves that fringe the continent act as a buffer and barrier between the warm ocean and inland ice but they are vulnerable to both oceanic and atmospheric warming.

This animation shows the break-off of a huge iceberg dubbed A-74, captured by satellite radar images that have the advantage they can “see” through clouds and operate day or night and are thus unaffected by the 24 hours of darkness that occurs during the Antarctic winter. The iceberg that forms is 1,270 km² in area which is about the same size as Greater London.

These examples illustrate just a few ways in which satellite data are providing unique, global observations of key components of the climate system and biosphere that are essential for our understanding of how the planet is changing. We can use this data to monitor those changes and improve models used to predict future change. In the run up to the vitally important UN climate conference, COP26 in Glasgow this November, colleagues and I have produced a briefing paper to highlight the role Earth observation satellites will play in safeguarding the climate and other systems that we rely on to make this beautiful, fragile planet habitable.The Conversation

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This blog is written by Cabot Institute for the Environment member Jonathan Bamber, Professor of Physical Geography, University of Bristol.

This article is republished from The Conversation under a Creative Commons license. Read the original article.

Jonathan Bamber