Prehistoric Planet: TV show asked us to explore what weather the dinosaurs lived through

Apple TV+, CC BY-NC-SA

When conjuring up images of when dinosaurs ruled the planet we often think of hot and humid landscapes in a world very different from our own. However, the new TV series Prehistoric Planet, narrated by Sir David Attenborough, shows dinosaurs living and indeed thriving in many types of environments, including colder regions where snowstorms, freezing fog and sea-ice were commonplace.

When the show’s producers first approached us to help understand the kinds of weather and environment that dinosaurs lived in before being wiped out around 66 million years ago, it prompted us to tackle a problem that has existed in palaeoclimate modelling for decades. That was, when scientists like us used computers to simulate, or “model”, the climate of prehistoric Earth, the models tended to make the poles much colder than evidence from fossils and rocks suggested they had actually been.

For the TV series, not only have we improved our models, but we have run the computer programmes for longer than anybody else has ever done to get the models as close to ancient “reality” as possible.

Prehistoric Planet depicts CGI dinosaurs based on the latest research.
AppleTV+, CC BY-NC-SA

The producers, the BBC’s Natural History Unit, needed to know about the weather so they could film “real world” locations similar to those that existed in the past where dinosaurs lived. But most of what we know about the climate that long ago comes from indirect “proxy” evidence, such as leaf fossils and traces of certain chemicals in rocks, which can only reconstruct the average climate over decades or centuries. This is where the narrative of a much hotter and more humid Cretaceous world comes from.

This narrative isn’t exactly wrong, but it doesn’t tell the whole story since weather and climate behave differently. For instance, even in today’s warming world a place like Texas, largely hot and humid, recently experienced widespread snowfall. Geologists a million years from now will spot the sudden global warming – but not the freak snowstorm. Nonetheless, modelling the the prehistoric equivalent of these snowstorms is important since we know warmer worlds will experience greater weather extremes. And these extremes will have largely determined which regions were completely inhospitable to dinosaurs.

Surface wind speed and precipitation through a typical year 69m years ago. An index of 1 means no visibility beyond 10 metres.

How do we know what the weather was like?

Unfortunately, although fossils give us many clues as to past climate, most cannot directly tell us what the weather was on a day to day basis.

So, for a given place on Earth, how do we know what the weather was on, say, May 27 some 66 million years ago? To do this we need to employ a computer simulation of the climate, similar to the ones used to look at future climate change today. These models are based on fundamental physical and biological processes which remain constant with time. It is therefore possible to adjust them for ancient worlds, even if we don’t know precise details like where or how high the mountains were, or exactly how much carbon dioxide was in the atmosphere.

We can then check these models using some of the ancient climate proxies, such as fossilised leaves, coral or rocks which contain traces of what conditions were like at the time. If our model matches up with the proxies – and it did – then we can be confident it is simulating typical weather at the time.

So what did we learn from modelling the climate of 66m years ago?

Our model found there would have been intense blizzards in Antarctica, for instance, “category six” hurricanes (something we are likely to see in our lifetimes) buffeting the mid and low latitudes and extensive, ever present, fog banks creating murky winters under polar cloud caps.

In a warmer world the water cycle is intensified over the poles. This meant more water in the air, and large parts of the planet would have been very foggy almost all the time (Source: modelling work by the authors)

This doesn’t immediately sound like a dinosaur-friendly environment. However, the old misconception that dinosaurs were cold blooded, thus requiring a warm climate for survival has for the most part already been dismissed. The new paradigm is that dinosaurs were warm blooded, and could to some extent regulate their internal temperature, like mammals do today.

This would be essential to survive large swings in temperature, driven by varied weather patterns, particularly in the polar regions. Our modelling therefore backs up recent fossil discoveries which show that some dinosaur species were cold-adapted, could see in low light conditions (useful in those huge fog banks), and thrived year-round near the poles.

Dinosaur in snow
Pachyrhinosaurus surviving and thriving.
AppleTV+, CC BY-NC-SA

The Prehistoric Planet scenes with the chilly Pachyrhinosaurus were set in Alaska, and demonstrate why the show wanted check its accuracy with climate models. We have an idea what the conditions would have been like there 66m years ago thanks to detailed fossils of plants, dinosaurs and other animals, yet the old models would have predicted intensely-cold and lifeless tundra.

Our model instead matches up with the fossil evidence, and predicts forests right up to the margins of the Arctic Ocean at 82°N – much further north than any trees today. In the summer, dinosaur food would have been abundant, but in the long dark winters it would have been more difficult to find, particularly as both fossils and modelling suggests it was so foggy.

Dinosaurs survived for a remarkable 165 million years. Tyrannosaurus Rex lived much closer to present day humans than it did to Stegosauruses, for instance. They managed to survive so long because they were resilient and adaptable to changeable environmental conditions, much like mammals are today. Our work for Prehistoric Planet shows that they were able to survive through greater extremes in temperature, stormier weather, and more extreme droughts than humans have experienced – so far.The Conversation

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This blog is written by Cabot Institute for the Environment members Dr Alex Farnsworth, Senior Research Associate in Meteorology, and Paul Valdes, Professor of Physical Geography, University of Bristol; and Robert Spicer, Emeritus Professor of Earth Sciences, The Open University

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

Mock COP26: Convincing, Cooperating and Collaborating

 

Glasgow COP26 presentation, preliminary discussion, and negotiation rounds 1 & 2

On 11th November at 10am around 60 A-level students from schools across Bristol gathered to participate in this year’s Mock COP26, hosted by Jack Nicholls, Emilia Melville, and Camille Straatman from the Cabot Institute for the Environment. After a resounding success from the first Mock COP, which took place online in March 2021, there was real excitement and anticipation building for the in-person event which would be held in the Great Hall of the Wills Memorial Building.

The morning kicked off with an engaging presentation by Jack, Emilia, and Camille, outlining the objectives of the upcoming COP26 in Glasgow. There had been much discussion surrounding the COP in the public sphere in the prior weeks, so it was interesting to see a summary of where things stand in the time since the Paris Agreement and what the potential outcomes of this COP may be.

The negotiations began with preliminary intra-group discussions, facilitated by a group of 12 postgraduate students. Each group defined their stance on each of the COP resolutions, ranging from option A, the most radical response, to C, the most conservative. It was evident from the off that these students were highly knowledgeable and passionate about the environmental, sociological, and economic impacts of each resolution, and as a result, each group wasted no time in prioritising the resolutions that would benefit their actor the most. Brazil factored in its current economic and development situation, as well as the Amazon’s critical role in the ecosystem balance, choosing to prioritise climate finance, natural protection and conservation and protecting climate refugees. For the International Indigenous Peoples Forum on Climate Change (IIFPCC), giving protected status to 50% of Earth’s natural areas by 2050 was defined as the most important resolution, whereas Shell chose to focus on phasing out coal, with the understanding that this would take the onus off the oil industry. Each group presented their ideal resolutions in a clear and concise manner.

The atmosphere really started to build in the hall when the first round of negotiations began. China faced Greenpeace in a heated discussion on coal usage while the IIFPCC negotiated with the USA on protecting indigenous populations. The United Nations High Commissioner for Refugees found alignment with Brazil on many of the resolutions, namely achieving net-zero emissions by 2050, natural protection and conservation to 30% of Earth’s natural areas and protecting climate refugees. In round two of negotiations, we saw Shell and the International Monetary Fund categorically disagree on the timeline for transition to Zero Emissions Vehicles, eventually compromising on a B resolution to have all new vehicle sales as zero-emission by 2040. Brazil was happy in supporting the IIPFCC in resolution 7a. (All countries must allow people fleeing from natural disasters, environmental degradation, and sea level rise to enter their countries and make their new homes there). Brazil and IIPFCC made an alliance to encourage USA toward resolution 7a, instead of their preferred 7b (Countries at risk of extinction from sea level rise should be provided with new land to settle and move their people to OR be provided with financial help to buy land in other nations). China and the Alliance of Small Island States (AOSIS) clash on coal usage, with AOSIS pushing back with a suggestion of image control, but ultimately China held strong on their decision.

Negotiation rounds 3 & 4, voting, and deputy mayor’s speech

The UK showed their tactical abilities and their knowledge in the negotiations with Greenpeace, but Greenpeace did not cede to their demands and manage to agree to a deal.  The IIPFCC was determined to protect indigenous land and communities, but their quest was heavily challenged by Shell. There was no common ground in the negotiation with this petrol giant, so the IIPFCC had to ensure an allyship with Brazil if they wanted to ensure the protection of the indigenous. On round four, Shell tried to sway some votes from China and Sweden, but while agreements were found with the former, the latter country was not going to let Shell influence their values. The tête-à-tête became lively as neither Shell nor Sweden were willing to compromise, resulting in a rather unsuccessful attempt of finding complicity.

After four intense rounds of negotiating, the voting began. Were all parties going to remain faithful to the agreements established during the negotiations? Or would some throw a curve ball, changing their minds at the last minute? The pondered tactics of the IIPFCC were successful, as they managed to lock Brazil’s and the USA’s support on their most valued resolutions. All parties pondered thoroughly on how to best use their votes, and it seemed that this meant that some agreements had been silently retracted, when some astonished reactions followed the raise of hands here and there.

The conference was finally over and many parties, including Brazil and Greenpeace, could celebrate the victory of the resolutions agreed upon. Yet, it was clear that a bittersweet aftertaste was left in the mouths of some parties, who did not manage to persuade enough. The heated debate had ended, and what was done was done, but one more surprise was awaiting our participants. Deputy Mayor Asher Craig had been sitting on the sidelines for a few instances already, assisting in the final yet most heated rounds of the conference. She was there, observing our pupils in awe as they got into character and avidly fought for their beliefs. The Deputy Mayor was impressed by the passion of these young minds and how much they are invested in the cause; she was proud to see that young generations care about the environment and our planet, as they came up with ideas for change that they would like to see more in the Bristol. The innovativeness and creativity of the students was remarkable in her eyes, as she proceeded to give an inspiring and uplifting speech on the efforts currently being made by the City Council to respond to the climate emergency. The mock COP26 was a more than a successful event, and as everyone waited for the results of the conference in Glasgow, we all wished that our simulation had been real.

Watch the students in action in this short video created by Particle Productions and funded by Bristol City Council.

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This blog is written by Sonia Pighini and Jennifer Malone, who are students on the Cabot Institute for the Environment Master’s by Research.

Jennifer Malone
Currently studying for a Master’s by Research in Global  Environmental Challenges from the Cabot Institute for the Environment, Jennifer’s research is centred on food system decarbonisation within the scope of UK food policy and community practice.
Sonia Pigini

Sonia is an international student in the MscR programme Global Environmental Challenges. Their research focuses on people-centred sustainable food system transitions in Bristol. They are particularly interested in exploring the potential for a more decentralised food system in the city, which empowers local producers, engages consumers and that keeps aspects such as justice and inclusion at its heart.

Image credit (image at top of blog): Jack Pitts

Digital home working and its sustainability potential: human immobility and the mobilities of stuff

Despite the huge human and economic costs of the COVID pandemic, many commentators have observed that this disruption – or shock – to our resource-intensive daily lives could offer a catalyst for the great societal transformations necessary to meet the climate emergency.

Radical growth of home working is an oft-cited example. According to Office for National Statistics (ONS) figures 50% of those in employment did some work from home in April 2020. This mainstreaming of home working has been facilitated by the rapid appropriation of digital devices and services into our everyday lives. It has been accompanied by equally rapid development of cultural skills and competencies required to (collectively) use those devices and services in a satisfactory way. And has led to major adjustments in how we work but also how we shop, interact, use our homes, engage with our local communities, learn, care for others and so on.

Home working during the pandemic, March 2020 (image: Simon Evans on Flickr)

The question is whether these shifts could lead to systemic environmental gains. Is it an environmental ‘good’ or ‘bad’? As ever with academics, our answer is ‘it’s not straightforward…’, but when viewed from a systemic perspective it does offer an opportunity to re-imagine sustainable ways of life.

When considering the environmental impacts of any technology or practice, understanding will be shaped by the scope of the analysis: what is considered inside the system being studied and what is ignored. A narrow scope, focused only on the technological parts of the system, makes it more straightforward to quantify the results (such as a ‘carbon footprint’ of something) but means missing out the broader implications – such as how any technology interacts with diverse social practices. One approach to this problem is to consider different scopes for analysis that address the direct, indirect and systemic impacts of a technology. We apply this framing to home working to consider some possibilities.

Direct impacts are the environmental costs of constructing, using and disposing of a technology. Engineering methods, such as life cycle assessment (LCA) (or more colloquially, ‘carbon footprinting’) can be used to model the technology’s life cycle, systematically collect the relevant data and then apportion the ‘environmental burden’ to the different applications of that technology. In the case of digital home working, this will include the impacts of manufacturing the equipment used and providing the electricity to keep it operational: both the home laptops and Wi-Fi, but also a share of the networking equipment used to connect workers with their offices and each other, and the data centres used to power the applications they use. Accounting for this ‘hidden materiality’, and the large consumption of energy used by data centres, has led to some fearing that the impacts of digital home working are substantial. Applying University of Bristol models developed for digital services to video conferencing suggests that the truth is somewhere between the two. A ballpark estimate for the climate impact of a one-hour video conference, for example, would be about 50-100g CO2e depending on the setup used – roughly equivalent to driving 400-800m in a typical family car. This suggests that we should not let concerns about the direct environmental impact of digital services put us off a move to home working.

Indirect impacts are the environmental costs of changing social practices related to the digital service. What do people stop doing? What do they start doing? Again, LCA can be used to quantify these – but only if one understands the nature of these changes. Social science insights are essential here, both to identify what changes to practice might occur, and to collect the data to quantify the extent to which they change across diverse populations.

In the case of home working, the most obvious changes to practice are reduction in travel to work and decreases in energy use within workplaces. These two factors will potentially be substantially larger than the direct impacts of technology use – but will be more variable and harder to predict across the population. Reductions in heating and lighting in the workplace were, it would appear, largely offset by rises of domestic energy use (Hook et al., 2020). The most dramatic potential environmental savings are from the sharp reduction in commuting, with the Department for Transport reporting a 60% reduction in private car usage during 2020 and a 90% decline in the use of public transport. But even here we must consider a range of related indirect effects of the apparent immobility of people. During the same period, we witnessed a huge increase in online shopping as people ordered their goods for home delivery. The ONS shows that online retail sales increased from just under 19% of total retail sales in November 2019 to almost 40% within a year. Groceries, clothing, household products and takeaway foods saw the largest growth.

The digital devices and services that allowed us to adapt so quickly to conditions of apparent human immobility also offered the technological affordances and cultural skills necessary for a commensurate growth in the circulation of goods, ordered online and delivered (often as individual items) to the homes of the immobile. Measuring these effects – especially if trying to capture the relative weighting of a trip to the shopping mall to purchase multiple items versus delivery of multiple individual items purchased online – would be necessary to estimate indirect impacts.

Systemic impacts consist of a huge range of elements that shape, and are shaped by, technologies and social practices. In the case of home working, we pick out three core elements: infrastructures, cultures, and modes of provision. To consider the impact and potential of home working we need to recognise the changing home to include the re-purposing of space for home offices and the technologies required, from the high tech (digital devices and networks) to the low tech (desks and storage). Local communities are also changing, and development of local service infrastructures to support mass home working (for example, the re-invention of the local high street) together with a corresponding decline of city-based office infrastructures will be required if home working is to be viable over the longer term. Each of these changes come with their own direct and indirect environmental impacts.

Cultural shifts must also be considered. Workplace cultures of presenteeism, long working hours, the status of private offices, and daily meetings are all challenged by home-working regimes. In addition, the rising use of digital platforms shows signs of fostering modes of provision through informal networks (such as familial and community based) that have, in recent history, been marginalised by the dominance of market modes of provision. Community sharing initiatives (such as food box schemes, local delivery hubs, community stores) coupled with the accumulating practical challenges of privately owned goods (as symbolised by the increasing percentage of domestic space devoted to storing seldomly used consumer goods and the decreasing use of expensive private cars) have been argued to indicate a shift towards collaborative consumption: the rejection of privately owned goods in favour of sharing (Southerton and Warde, forthcoming). While the direct and indirect environmental impacts of such systemic shifts are unknown, the potential to reduce the material flows of goods and reduce the impacts of human mobility are clear.

Thinking in terms of the systemic implications of home working – symbolised by the immobility of people and rising mobility of goods during COVID – is more important than only measuring direct and indirect impacts. As things stand, we are moving in the direction of ‘hybrid’ working, presumably on the grounds of a ‘best of both worlds’ assumption. From a systems level perspective there is a huge risk that we end up with two systems: workplaces and home working. Whether this ends up being the worst of both worlds, layering new resource-efficient systems over old resource-intensive systems, will largely depend on whether debates regarding the post-COVID world takes the opportunity to re-imagine and re-configure the systemic impacts of technology and human practice on the environment (Geels et al., 2015).

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This blog is written by Chris Preist, Professor of Sustainability and Computer Systems at the University of Bristol. His research focuses on the environmental impact of digital technology and consumer electronic goods; and Dale Southerton, Professor in Sociology of Consumption and Organisation at the University of Bristol. He studies consumption, its role in organising everyday lives and its significance in processes of societal change.

Teaching sustainability in computer science?

The Faculty of Engineering at the University of Bristol ran a discussion panel on if and how should (environmental) sustainability be taught to the Engineering students. Here are my 2 pence on teaching sustainability to Computer Science students.

Why should our students engage with Environmental Sustainability in their formal education?

Well because the ICT/Software impacts and drives every activity in the present society – from the day to day business to entertainment, education, and policy. This impact is felt in two ways:

  1. through production and use of ICT equipment and software, and
  2. through changing the way that the society itself operates.

I will only mention some brief points about the impact of production and use of ICT:

  • Energy Consumption of the ICT systems seems to be growing unstoppably, e.g.,
    • In 2018 the data centres were accountable for  about 1 % of the global electricity use
    • The energy consumption of the ICT is projected (in worst case) to account for 20% of the world electricity consumption in 2030 [1].
  • Materials, including rare earth metals are also increasingly depleted for use of ICT hardware production. Even worth, as much of the hardware is quickly outdates and distracted, it creates the problem of e-waste.
  • Waste form ICT hardware is either put into landfill or damped at the developing countries.

So yes, to point out a few issues that we, as computer scientists and engineers we need to learn to think about:  how about teaching and learning about how to minimise energy and material consumption, how to design modular and long-living hardware and software solutions, how to make our software maintainable and hardware bio-degradable?

But, even more importantly, Software Engineers must learn about the impact that their software solutions have within their situated environments.

Let’s look at the problem of traffic congestion: we all know that when too many vehicles are trying to get through a given road, they create a traffic jam; as the vehicles use (fossil) fuels while sitting in a traffic jam, they ends up generating excessive CO2. So what can a software engineer do to help? How about we some ride sharing software solutions, like Uber or Lyft?

Figure 1: Ride sharing software to reduce CO2 emissions.

We know that, as shown in Figure 1, this software will reduce the need for car ownership and as lesser number of people own and drive their cars, it will also reduce traffic congestion problem!

We already teach our students how to develop such applications. They already learn about platform development for data collection, and data analytics, distributed systems development and could computing and user interface design: all that they need to develop a ride sharing application is well covered in the current Computer Science curriculum.

But what happens once this application goes out to be used by people? It turns out that car ownership does decrease, so great. But, as studies into ride sharing show, these also increase the distance travelled by the shared cars. Even worse, as ride sharers become accustomed to the Uber/Lyft services, which are convenient and cheap compared to “normal” taxies, they start to substitute the journeys previously taken by public transport (i.e., bus or train) for ride sharing services.

In short, traffic congestion and respective CO2 emissions do not improve at all, as shown in Figure 2.

Figure 2: Longer term environmental impact from use of ride sharing.

I suggest this is because, while the software developers for the ride sharing solutions may have wished to reduce environmental impact, they did not know  how to account for such an impact. As and education providers, we do not teach our Software Engineering students about:

  • Systems Thinking,
  • Environmental Life Cycle Assessment,
  • Responsible Innovation and Software Impact Assessment, about
  • Human Behaviour and Rationality, or
  • Sustainable Living.

What should be offered to students within our faculty with regards to Environmental Sustainability?

Well, all of the above. Unless we teach our students to account for the human behaviour and longer term software use, software impact assessment and responsible decision making in what, how, and why is integrated into software solutions, we are not likely to see such solutions having any positive impact in addressing the challenges of the environmental degradation and climate change.

So how can we integrate Sustainability into our programs?

I suggest that each module taught to our students must cover content of how it relates to sustainability and sustainable development. So each module needs to be reviewed. As stated in the Karlskrona Manifesto for Sustainability Design [2,3]:

There is a perception that sustainability is a distinct discipline of research and practice with a few defined connections to software.

Whereas sustainability is a pervasive concern that translates into discipline- specific questions in each area.

So, we really do need to teach students about which questions does sustainability translate in each of our modules, and how to address these questions, some examples of these are shown in Fig 3.

Figure 3: Additional issues to consider in Computer Science Curricula.

References

[1] https://ictfootprint.eu/en/news/decreasing-ict-energy-consumption-%E2%80%93-power-data-centres-and-people%E2%80%99s-will-ictfootprinteu-webinar 

[2] The Karlskrona Manifesto for Sustainability Design, url: https://www.sustainabilitydesign.org/karlskrona-manifesto/

[3] Becker, C., Chitchyan, R., Duboc, L., Easterbrook, S., Penzenstadler, B., Seyff, N., Venters, C. C. (2015). Sustainability design and software: The Karlskrona manifesto. ICSE’15: 37th International Conference on Software Engineering. http://dx.doi.org/10.1109/ICSE.2015.179

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This blog is written by Cabot Institute for the Environment member Dr Ruzanna Chitchyan, from the Department of Computer Science at the University of Bristol.

India heatwave: why the region should prepare for even more extreme heat in the near future

An extreme heatwave in India and Pakistan has left more than a billion people in one of the most densely populated parts of the world facing temperatures well above 40℃. Although this has not broken all-time records for the regions, the hottest part of the year is yet to come.

Though the heatwave is already testing people’s ability to survive, and has led to crop failures and power blackouts, the really scary thing is that it could be worse: based on what has happened elsewhere at some point India is “due” an even more intense heatwave.

Together with a few other climate scientists, we recently looked for the most extreme heatwaves globally over the past 60 years – based on the greatest difference from expected temperature variability in that area, rather than by maximum heat alone. India and Pakistan do not feature in our results, now published in the journal Science Advances. Despite regularly having extremely high temperatures and levels of heat stress in absolute terms, when defined in terms of deviation from the local normal, heatwaves in India and Pakistan to date have not been all that extreme.

In fact, we highlighted India as a region with a particularly low greatest historical extreme. In the data we assessed, we didn’t find any heatwaves in India or Pakistan outside three standard deviations from the mean, when statistically such an event would be expected once every 30 or so years. The most severe heatwave we identified, in southeast Asia in 1998, was five standard deviations from the mean. An equivalent outlier heatwave in India today would mean temperatures of over 50℃ across large swaths of the country – such temperatures have only been seen at localised points so far.

Our work therefore suggests India may experience even more extreme heat. Assuming the statistical distribution of daily maximum temperatures is broadly the same across the world, statistically a record-breaking heatwave is likely to occur in India at some point. The region has not yet had reason to adapt to such temperatures, so may be particularly vulnerable.

Harvests and health

Although the current heatwave has not broken any all-time records, it is still exceptional. Many parts of India have experienced their hottest April on record. Such heat this early in the year will have devastating impacts on crops in a region where many rely on the wheat harvest both to eat and to earn a living. Usually, extreme heat in this area is closely followed by cooling monsoons – but these are still months away.

It is not just crop harvests that will bear the brunt, as heatwaves affect infrastructure, ecosystems and human health. The impacts on human health are complex as both meteorological factors (how hot and humid it is) and socioeconomic factors (how people live and how they are able to adapt) come into play. We do know that heat stress can lead to long-term health issues such as cardiovascular diseases, kidney failure, respiratory distress and liver failure, though we will be unable to know exactly how many people will die in this heatwave due to the lack of necessary health data from India and Pakistan.

What the future holds

To consider the impact of extreme heat over the next few decades, we have to look at both climate change and population growth, since it is a combination of the two that will amplify the human-health impacts of heat extremes in the Indian subcontinent.

world map with some countries shaded yellow
Hotspots of population increases over the next 50 years (red circles), all coincide with locations where no daily mortality data exists (yellow).
Mitchell, Nature Climate Change (2021), CC BY-SA

In our new study, we investigated how extremes are projected to increase in the future. We used a large ensemble of climate model simulations, which gave us many times more data than is available for the real world. We found that the statistical distribution of extremes, relative to a shift in the underlying climate as it generally gets warmer, does not change. In the climate models the daily temperature extremes increase at the same rate as the shift in the mean climate. The IPCC’s latest report stated that heat waves will become more intense and more frequent in south Asia this century. Our results support this.

The current heatwave is affecting over 1.5 billion people and over the next 50 years the population of the Indian subcontinent is projected to increase by a further 30%. That means hundreds of millions more people will be born into a region that is likely to experience more frequent and more severe heatwaves. With even larger numbers of people being affected by even greater heat extremes in the future, measures to adapt to climate change must be accelerated – urgently.The Conversation

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This blog is written by Cabot Institute for the Environment members Dr Vikki Thompson, Senior Research Associate in Geographical Sciences, University of Bristol and Dr Alan Thomas Kennedy-Asser, Research Associate in Climate Science, University of Bristol.

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

Climate change isn’t just making cyclones worse, it’s making the floods they cause worse too – new research

People take refuge on a sports ground following flooding caused by Cyclone Idai in Mozambique.
DFID/Flickr, CC BY-SA

Laurence Hawker, University of Bristol; Dann Mitchell, University of Bristol, and Natalie Lord, University of Bristol

Super cyclones, known as hurricanes or typhoons in different parts of the world, are among the most destructive weather events on our planet.

Although wind speeds within these storms can reach 270 km/h, the largest loss of life comes from the flooding they cause – known as a “storm surge” – when sea water is pushed onto the coast. Climate change is predicted to worsen these floods, swelling cyclone clouds with more water and driving rising sea levels that allow storm surges to be blown further inland.

In May 2020, Super Cyclone Amphan hit the India-Bangladesh border, bringing heavy rainfall and strong winds and affecting more than 13 million citizens. The cyclone also caused storm surges of 2-4 metres, flooding coastal regions in the Bay of Bengal.

While over the ocean, this category five storm – that’s a storm’s highest possible rating – became the strongest cyclone to have formed in the Bay of Bengal since 1999, reaching wind speeds of up to 260 km/h. Although it weakened to a category two storm following landfall, it remained the strongest cyclone to hit the Ganges Delta since 2007.

Amphan had severe consequences for people, agriculture, the local economy and the environment. It tragically resulted in more than 120 deaths, as well as damaging or destroying homes and power grids: leaving millions without electricity or communication in the midst of an ongoing pandemic.

Relief and aid efforts were hampered by flood damage to roads and bridges, as well as by coronavirus restrictions. Large areas of crops including rice, sesame and mangos were damaged, and fertile soils were either washed away or contaminated by saline sea water. Overall, Super Cyclone Amphan was the costliest event ever recorded in the North Indian Ocean, resulting in over $13 billion (£10 billion) of damage.

Two people assess a tree that has fallen across a road
In Kolkata, India, Super Cyclone Amphan caused widespread damage.
Indrajit Das/Wikimedia

In a recent study led by the University of Bristol and drawing on research from Bangladesh and France, we’ve investigated how the effects of storm surges like that caused by Amphan on the populations of India and Bangladesh might change under different future climate and population scenarios.

Amphan: Mark II

Rising sea levels – thanks largely to melting glaciers and ice sheets – appear to be behind the greatest uptick in future risk from cyclone flooding, since they allow storm surges to reach further inland. It’s therefore key to understand and predict how higher sea levels might exacerbate storm-driven flooding, in order to minimise loss and damage in coastal regions.

Our research used climate models from CMIP6, the latest in a series of projects aiming to improve our understanding of climate by comparing simulations produced by different modelling groups around the world. First we modelled future sea-level rise according to different future emissions scenarios, then we added that data to storm surge estimates taken from a model of Super Cyclone Amphan.

We ran three scenarios: a low emission scenario, a business-as-usual scenario and a high emission scenario. And in addition to modelling sea-level rise, we also estimated future populations across India and Bangladesh to assess how many more people storm surges could affect. In most cases, we found that populations are likely to rise: especially in urban areas.

Our findings were clear: exposure to flooding from cyclone storm surges is extremely likely to increase. In India, exposure increase ranged from 50-90% for the lowest emission scenario, to a 250% increase for the highest emission scenario. In Bangladesh, we found a 0-20% exposure increase for the lowest emission scenario and a 60-70% increase for the highest emission scenario. The difference in exposure between the two countries is mostly due to declining coastal populations as a result of urban migration inland.

Imagine we’re now in 2100. Even in a scenario where we’ve managed to keep global emissions relatively low, the local population exposed to storm surge flooding from an event like Amphan will have jumped by ~350,000. Compare this to a high emission scenario, where an extra 1.35 million people will now be exposed to flooding. And for flood depths of over one metre – a depth that poses immediate danger to life – almost half a million more people will be exposed to storm surge flooding in a high emission scenario, compared to a low emission scenario.

A composite satellite image of a large white cyclone
A satellite image shows Amphan approaching the coasts of India and Bangladesh.
Pierre Markuse/Wikimedia

This research provides yet more support for rapidly and permanently reducing our greenhouse gas emissions to keep global warming at 1.5°C above pre-industrial levels.

Although we’ve focused on storm surge flooding, other cyclone-related hazards are also projected to worsen, including deadly heatwaves following cyclones hitting land. And in the case of Amphan, interplay between climate change and coronavirus likely made the situation for people on the ground far worse. As the world warms, we mustn’t avoid the reality that pandemics and other climate-related crises are only forecast to increase.

Urgent action on emissions is vital to protect highly climate-vulnerable countries from the fatal effects of extreme weather. Amphan Mark II need not be as destructive as we’ve projected if the world’s governments act now to meet Paris agreement climate goals.The Conversation

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This blog is written by Cabot Institute for the Environment members Dr Laurence Hawker, Senior Research Associate in Geography, University of Bristol; Professor Dann Mitchell, Professor of Climate Science, University of Bristol, and Dr Natalie Lord, Honorary Research Associate in Climate Science, University of Bristol

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

Migration, mobilities and the ecological context

In this special blog series, Migration Mobilities Bristol (MMB) and the Cabot Institute for the Environment bring together researchers from across the University of Bristol to explore connections between movement and the environment from a multi-disciplinary perspective. Their diverse approaches highlight the importance of developing frames that incorporate both migration and environment, and in so doing benefit our understandings of both. 

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Migration can make you happy. When I see the first swifts arrive in the spring, I stop in my tracks and smile broadly at all and everyone. I have to restrain myself from telling people walking down the street that ‘they’ are back. Swifts are one of the wonders of the world – they make Concorde look clunky, they hurtle down streets in towns screaming wildly at dusk seemingly just for the fun of it, and scientists have calculated that the distance they fly over their lifetime is equivalent to flying to the moon and back seven times!

Dahlia (Bishop of Llandaff). Image credit: Jane Memmott

Migratory species like swifts have two homes and they are generally well regarded in both places. It’s a bit more touch and go whether alien species are welcome or not, and highly context dependent. For example, we deliberately introduce species from all around the world into our gardens without qualm – looking out the window onto my front garden, I’ve got honey bush and pineapple lilies from South Africa, Dahlias from Mexico, a Hebe from New Zealand, devil’s tobacco from Chile and foxgloves from seed collected down the road! In contrast, my local nature reserves are doing their best to remove Rhododendron, Cotoneaster and Himalayan balsam.

Context really is key here. Thus, gardens are grown for colour, relaxation, fruit, vegetables, and art (and I consider gardening as much of an art as a science) and they are highly managed and artificial habitats. In fact, they are increasingly considered as outdoor rooms in the media, and no one worries what countries their botanical furniture is from. In contrast, nature reserves are usually more natural settings where we want to capture natural patterns and processes, so there is an expectation that the species present should be native. And there is good evidence that while most alien species are harmless, some species (approximately 1%) can be very damaging to the environment and the economy.

Honey bush leaves (Melianthus major). Image credit: Jane Memmott

Migration is about mobility, and mobility is a key part of the scientific process. Thus, universities are ecosystems which provide intellectual homes to academics from all over the world. My own department is home to scientists from Africa, Germany, Brazil, Switzerland, Brazil, Italy and China and those are just the people I’ve bumped into over the last few days. COVID has put a bit of a spanner in the works on the mobility front, but mobility is so key to business that academics have quickly found other ways to be mobile. For example, in my own research group, we have been running a large project in a remote part of Nepal entirely by Zoom for the last two years. But, by dint of the internet and some incredible UK staff and amazing project partners in Nepal, we have trained field staff in ten remote villages in the Himalayas to collect diet data for both bees and villagers, using protocols that would have been very new to them. The data is then uploaded by the field staff to the internet and arrives on the computers the other side of the world as if by magic.

Mobility is such a large part of a scientist’s life that when it goes wrong it can feel shocking. I’ve had two encounters with mobility of scientists being blocked, one involving myself, another a visiting scientist. Mine was, I suspect, a straightforward random immigration check, but it did leave me rather shaken. I was travelling to Canada for the first time and got taken out of the queue and then grilled for 30 minutes on the nature of my visit. I was giving a plenary talk at a conference and had fortunately remembered to print out my letter of invitation. Unfortunately, I hadn’t actually read it for six months and so I probably did sound a bit suspicious. They did eventually let me in and it was an excellent trip thereafter. The second time was when a restoration ecologist from Latin America, who was visiting my research group for six months, went to Spain with his family for a weekend and upon return his whole family was issued with deportation papers. There is something deeply shocking about seeing the hostile environment process in action, especially when mobility is simply part of normal academic interchange. After some high-level work by an international lawyer this too was fixed. Restoration ecology is much more of a long-term process, but the restoration of mobility was much faster in this instance, if a lot more stressful.

Swift (Apus apus). Image credit: Wikimedia Commons.

Migration and mobility are everyday events in the environment. They can be natural such as the return of swifts each year, or they can be assisted such as the reintroduction programmes for species that have become extinct in the UK. One of the biggest reintroduction success stories is the red kite, a bird that you are almost guaranteed to see now if you drive down the M4 motorway or look out of the train window from Didcot to London. These are big and very beautiful predatory birds – imagine a paprika coloured swallow with a 6ft wingspan! My last few Saturdays have been spent driving from Bristol to a hospital in Hampshire to visit a sick relative and one of the things that has made this less stressful is counting the red kites along the motorway. Last Saturday was a 12-kite day, my highest count yet.

To end, migration, mobility and the environment are inextricably linked. There is both natural and human assisted movement of species in the environment. Species can be both welcome and unwelcome depending on the context. It’s complicated, but it’s the everyday bread and butter of ecologists around the world. With alien plants bringing colour and bizazz to our gardens and swifts bringing happiness as they return to their second homes in the UK, there is a lot to like about migration and mobility in the environment.

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This blog is written by Cabot Institute for the Environment member, Jane Memmott, Professor of Community Ecology in the School of Biological Sciences, University of Bristol. Her research interests include pollination ecology, invasion ecology, biological control and restoration ecology. In each case she considers how ecological networks can be used as a tool to answer environmental questions.

Professor Jane Memmott

How water stress impacts on migration

In this special blog series, Migration Mobilities Bristol (MMB) and the Cabot Institute for the Environment bring together researchers from across the University of Bristol to explore connections between movement and the environment from a multi-disciplinary perspective. Their diverse approaches highlight the importance of developing frames that incorporate both migration and environment, and in so doing benefit our understandings of both. 

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In 2015, Ioane Teitiota and his family were deported from New Zealand to the Pacific island nation of Kiribati. His asylum application had been based on the grounds that water, due to sea level rise, had made the island uninhabitable in various ways: there was a shortage of clean drinking water; the available habitable land had decreased, which had led to increased insecurity because of violent land disputes; and the main activity, subsistence farming, was impeded.

Water has always had a major influence on where we live. Whether drawing us to new locations or forcing us from existing ones, water has always been intricately connected to the movement of people. As soon as it was possible to navigate the wide-open sea, water facilitated exploration to new lands. Later, being on these wide, open seas offered hope to millions fleeing world wars, presenting a somewhat invincible fortress protecting them from persecution, suffering and premature demise. More recently, the drowning of at least 27 men, women and children attempting to make the crossing from France to England brought into sharp focus how some things have not changed since those world wars: many are still crossing seas to flee persecution, suffering and premature demise.

In recent times, it is increasingly recognised that climate change will be a significant driver of migration. Island states such as Tonga and Micronesia already have negative net migration rates and projections are that stressed freshwater resources and water-related extreme events (such as floods) will drive more migration from island states because of food insecurity and habitat loss. Some states are already purchasing land to relocate citizens, as this is considered the only reliable adaptive response. By 2014, Kiribati had purchased 6,000 acres of forest land from Fiji: ahead of the UN climate summit that year, Anote Tong, Kiribati’s president at the time, said that buying land abroad was the way to ensure ‘migration with dignity’. Meanwhile, 6,000 km to the east, the world’s ‘first environmental refugees’ were already setting up new homes in Bougainville, an autonomous island of Papua New Guinea. They had left islands that were becoming increasingly uninhabitable as sea water ingress led to shortages in arable land and clean drinking water.

It is debatable, however, whether the islanders migrating to Bougainville are indeed the world’s first group of people forced to leave their ancestral lands due to climatic changes. Lake Chad, in west Africa was once the sixth largest inland water body, with an open water area of 25,000 km2 in the 1960s. By the 1980s, over 90% of the lake had been lost due to decreased precipitation, sparking significant internal and international migration. By 2015, more than 71,000 people from Nigeria and North Cameroon had moved towards the lake’s receding shores. As the ever-growing numbers scrambled for a portion of the limited water resources to farm, water their livestock and maintain their livelihoods, violence erupted that led to further migration out of the region. With limited non-agricultural skills and no source of capital to engage in alternative livelihood strategies the situation for these people is extremely precarious.

These two case studies challenge the narrative that climate change will drive migration in the future. They show that it already does. The situation is only likely to get worse as more regions of the world are affected, and yet, the impact of water crises on migration is not well documented.

Environmental migrants

No legal definition exists to date, for people on the move due to environmental drivers. However, the International Organisation for Migration put forward the following definition in 2007:

… persons or groups of persons who, predominantly for reasons of sudden or progressive change in the environment that adversely affect their lives or living conditions, are obliged to leave their habitual homes or choose to do so, either temporarily or permanently, and who move either within their country or abroad.

(IOM, 2007:1)

Water scarcity is bound to be a major driver of migration given that 17 countries, home to 25% of the global population, are already experiencing water stress (see Figure 1). The poorest of the global population will be the most adversely affected, but, without the necessary resources, they are also the least able to leave their homelands to seek livelihoods elsewhere. It is therefore unlikely that the world will see waves of impoverished ‘water refugees’ crossing oceans and landing on the shores of wealthy nations. The World Bank estimates that residents of poor countries are four times less likely to move than residents of middle-income countries. But their inability to move will severely impact their chances of survival.

Figure 1: Predicted global water stress between 2030 and 2040 (Image: OpenStreetMap)

 

Conceptualising water as a driver of migration

Water has always been both a push and pull factor for migration: places with adequate sources will attract migrants while diminishing reserves have the opposite effect. To assess the interconnection between water and migration, a 3D model encompassing water quantity, water quality and water-related extremes has been suggested (see Figure 2). Deterioration of water quality – for example, resulting from chemical contamination or increased salinity – will push people away from habitats due to adverse health impacts. Increased salinity can also significantly impact food security, leading to out-migration. The third factor, water extremes – such as floods or droughts – impact both quality and quantity, but their impact on the nature of migration (whether it is temporary or permanent) depends on how frequently these events occur.

Figure 2: Three-dimensional framework conceptualising the links between water and migration (Image: Nagabhatla et al., 2020).

Which way forward?

It is important to acknowledge the ways in which water migration results in unfair outcomes both for those with means to escape water-scarce areas and those without. In developing countries, wages of workers who move from rural to urban areas due to drier climates may be up to 3.4% lower than that of a typical immigrant – a significant amount for those already on a very low income. For those unable to leave their water-scarce homes, diminished food security and loss of income from agriculture present significant blows to already disadvantaged communities.

In urban areas water supplies are also under threat from climate change. Doing nothing could prove extremely costly to local and global economies, both increasing involuntary migration and severely impacting on communities without resources to fund migration. It is therefore crucial to invest in infrastructure and policies that enhance resilience within cities as well as rural areas. Water recycling, rainwater harvesting and incentives for efficient water use are tools that can be employed to this end. Evidence shows that while people may initially be resistant to using recycled water, their willingness increases when all available options are weighed up.

Finally, protecting livelihoods at the place of origin needs to be a key strategy for addressing water-induced population movement. In rural areas climate-smart agriculture can help towards reducing the vulnerability of communities and their livelihoods to diminished water resources. In Senegal, for example, high yielding, early maturing and drought resistant varieties of sorghum, millet, cowpeas and groundnuts are being developed as an adjustment to the shorter rain seasons. Traditional varieties required at least 120 days and plenty of rain to harvest, but new varieties require less than 110 days and can withstand two to three week stretches without rain. Instead of giving up farming therefore, farmers can stay on their lands and farm in ways that are adaptable to water scarcity and a variable climate.

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This blog is written by Dr Anita Etale, a Research Associate at the Department of Aerospace Engineering at the University of Bristol. Her research focuses on finding sustainable materials for water treatment using sustainable resources as well as the environmental and social implications of water stress on communities. Anita is MMB’s Early Career Representative.