Making decisions in an environmentally uncertain world

Improved decision making in the face of environmental uncertainty is at the heart of the Cabot Institute. Although individuals, businesses and society aspire to make logical decisions, informed by evidence and wisdom, we are also influenced by a complex mixture of emotions, ethics, political opportunism and personal beliefs.  These murky waters become even more challenging to navigate when dealing with the inherent uncertainty in the basic evidence.  And it becomes almost impossible when pre-conceived beliefs and opinions replace evidence.  In such scenarios, uncertainty can be manipulated as a tool to undermine evidence and justify flawed decisions.  This is the particular challenge of decision making in the context of complex environmental, economic and ecological issues.

To a scientist confronted with evidence that human activity is changing our environment at unprecedented rates, it is apparent that environmental uncertainty is rarely appropriately deployed in policy making.  Most perniciously, it is commonly argued that the risk of an action (i.e. loss of biodiversity or increasing CO2 emissions) could be at the low end of the probability distribution – ‘the temperature might not warm that much’, ‘we might not get more hurricanes’.  That is not proper governance; that is hiding behind uncertainty and hoping for the best.  Nor is it appropriate to govern based on the worst-case scenario.  But nor can we govern by solely considering the most likely outcome.  We must recognise the range of possibilities and plan within it – strategically, flexibly, resiliently.  In other words, the uncertainty brought about by ongoing environmental change is itself a profound cause for concern and a challenge for governance.

However, environmental uncertainty is not an opaque label for things ‘we do not understand’ and by an extension it is not a cause for inaction.

Rich Pancost’s old farm, US Midwest

I grew up on a farm in the US Midwest and so environmental uncertainty to me mainly concerns our food and the people who provide it.   Anyone who has ever been involved in farming understands how uncertain our environment can be. And they understand how undermining and economically challenging that uncertainty is, especially with respect to the weather (weather is not the same as climate, but it makes for a useful environmental analogy).

We had about 30 head of cattle on our small Ohio dairy farm , and my brother, parents and I needed to put aside 4000 bales of hay every summer. I loved that job – I remember the smell of drying hay and the fat bumble bees buzzing in the clover. I remember being with my family, the satisfaction of completed work and the closeness that came from achieving things together. But it was hard and uncertain work, my father cutting the grass, raking it and baling it, quickly over successive hot days so that it would dry before a summer rain shower could strip away the nutrients. Or worse: before an extended few days of rain saturated the mowed hay on the ground, causing it to become fungus-ridden and rotting it away in the field.  We could work with a prediction of rain and we could work with a prediction of no rain or even drought.  But we could not work with an overly uncertain prediction.  Even worse were wrong (i.e. overly certain) predictions.  We navigated the probabilistic terrain of the daily weather forecasts somewhat by instinct, but the stakes were high, and just three or four bad decisions in a summer would have been financially catastrophic.  The farm is long gone but my Mom is still addicted to the weather reports.

The barn

But uncertainty does not mean paralysis; it means risk management.  We mitigated the risk of wasted crop by renting and working fields that could yield 4500 bales rather than 4000.  And those 4000 bales of hay were themselves, risk management, exceeding our likely needs.  Gathering the bales and storing them in our barn’s loft was hard, sticky, hot and gritty work.  The hay was delivered to the loft by a metal elevator – metal plates carried by metal chains up a metal chute, all powered by our forty-year old International Harvester tractor’s power take-off shaft.  I loved doing this work on the farm – its physicality and the stimulus of all of your senses – but I do not miss that tremendous rattling, clanging noise!  The loft itself could reach temperatures of 110°F and was filled with clouds of dust and darting, irritated wasps.  Our necks would burn and our forearms would be filled with tiny splinters of hay.

We worked hard and put away 4000 bales each summer even though we would probably only need 3500, because we had to err on the side of caution in case there was an early winter. Or a long winter.

That is environmental uncertainty – and risk management – to me.  Cutting the hay when the forecast predicts a 35% chance of rain and watching 400 bales of alfalfa rot in the field.  Renting more land than we would likely need. Working 20% harder than necessary – just in case.

All of us understand this, whether it be maintaining the garden, managing the allotment or planning a holiday. This is part of human history: sound, profitable, secure decision-making has always required a confrontation with environmental uncertainty; consequently, almost all societies have strived to mitigate risks by understanding the environment, managing essential resources, and building up our own resilience.

From IPCC 2013, Working Group 1

What is disturbing and unique about the 21st century is that we are no longing mitigating environmental uncertainty but instead, we are very rapidly increasing it. We are changing our planet and where and how we live upon it.  Increasing carbon dioxide emissions might warm the planet by 1.5°C.  Or 3°C.  Or 5°C.   Such warming will probably cause the Southwest of England to have wetter summers and the great food-supplying regions of the American Midwest to become drier.  But there is a probability that the opposite will happen.  How does the small farmer plan?  For that matter, how does the huge international agritech firm plan? I would argue that the greatest challenge posed by our changing environment is not how much the Earth warms but the uncertainty in how much it will warm and the uncertainty associated with the consequences of that warming. Planning for our future – perhaps for the first time in human history – is actually becoming more uncertain every year.

But we are also learning much more about ourselves and our environment, and this perhaps makes the future a bit more certain than it might otherwise be.  Currently the Met Office is improving our prediction tools and tailoring specific advice to farmers; engineers are learning how we might mitigate or even adapt to this uncertainty; and we are developing methods to limit our dependence on fossil fuel and thus the associated climate change.  And we are learning how to make sound decisions in the face of it. To achieve these objectives, the Cabot Institute and similar entities are bringing together a wide variety of scientists, social scientists, managers and engineers, all of whom share expertise with the community and industry.  That expertise includes those who deal specifically with quantifying uncertainty, the underlying psychology and sociology of decision making, and the clash of ethical and pragmatic ideas that inform policy making.  The world’s population is growing and with it our basic food, water and energy needs; to provide for those needs, we must make our future more certain but also more resilient and adaptable.

This blog was written by Professor Rich PancostCabot Institute Director, University of Bristol

Prof Rich Pancost

 

Measuring our world: Notes from the V.M. Goldschmidt Conference

Galileo Galilee
Measure what is measurable, and make measurable what is not so.’ – Galileo Galilee

Science is measuring.

Of course, it is about much more than measuring.  The scientific approach includes deduction, induction, lateral thinking and all of the other creative and logistical mechanisms by which we arrive at ideas. But what distinguishes the ideas of science from those of religion, philosophy or art is that they are expressed as testable hypotheses – and by testable hypotheses, scientists mean ideas that can be examined by observations or experiments that yield outcomes that can be measured.

Earth scientists use astonishingly diverse approaches to measure our world, from the submolecular to the planetary, from bacterial syntrophic interactions to the movement of continental plates. A particularly important aspect of observing the Earth system involves chemical reactions – the underlying processes that form rocks, fill the oceans and sustain life. The Goldschmidt Conference, held this year in Florence, is the annual highlight of innovations in geochemical methodologies and the new knowledge emerging from them.

Geochemists reported advances in measuring the movement of electrons across nanowires, laid down by bacteria in soil like electricians lay down cables; the transitory release of toxic metals by microorganisms, daily emissions of methane from bogs, and annual emissions of carbon dioxide from the whole of the Earth; the history of life on Earth as recorded by the isotopes of rare metals archived in marine sediments; the chemical signatures in meteorites and the wavelengths of light emitted from distant solar nebulae, both helping us infer the building blocks from which our own planet was formed.

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The Goldschmidt Conference is often held in cities with profound cultural legacies, like that of Florence.  And although Florence’s legacy that is perhaps dominated by Michelangelo and Botticelli, Tuscany was also home to Galileo Galilee, and he and the Scientific Revolution are similarly linked to the Renaissance and Florence. Wandering through the
Galileo Museum is a stunning reminder of how challenging it is to measure the world around us, how casually we take for granted many of these measurements and the ingenuity of those who first cracked the challenges of quantifying time or temperature or pressure.

And it is also exhilarating to imagine the thrill of those scientists as they developed new tools and turned them to the stars above us or the Earth beneath us.  Galileo’s own words tell  us how he felt when he pointed his telescope at Jupiter and discovered the satellites orbiting around it; and how those observations unlocked other insights and emboldened new hypotheses:

‘But what exceeds all wonders, I have discovered four new planets and observed their proper and particular motions, different among themselves and from the motions of all the other stars; and these new planets move about [Jupiter] like Venus and Mercury… move about the sun.’

The discoveries of the 21st century are no less exciting, if perhaps somewhat more nuanced.

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The University of Bristol is one of the world leaders in the field of geochemistry.  Laura Robinson co-chaired several sessions, while also presenting a new approach to estimating water discharge from rivers, based on the ratio of uranium isotopes in coral; the technique has great potential for studying flood and drought events over the past 100,000 years, helping us to better understand, for example, the behaviour of monsoon systems on which the lives of nearly one billion people depend.  Heather Buss chaired a session and presented research quantifying the nature and consequences of reactions occurring at the bedrock-soil interface – and by extension, the processes by which rock becomes soil and nutrients are liberated, utilised by plants or flushed to the oceans. Kate Hendry, arriving at the University of Bristol in October, presented her latest work employing the distribution of zinc in sponges (trapped in their opal hard parts) to examine how organic matter is formed in surface oceans, then transported to the deep ocean and ultimately buried in sediments; this is a key aspect to understanding how carbon dioxide is ultimately removed from the atmosphere.  The Conference is not entirely about measuring these processes – it is also about how those measurements are interpreted. This is exemplified by Andy Ridgwell who presented two keynote lectures on his integrated physical, chemical and biological model, with which he evaluated the evidence for how and when oceans become more acidic or devoid of oxygen.

What next?  Every few years, a major innovation opens up new insights.  Until about 20 years ago, organic carbon isotope measurements (carbon occurs as two stable isotopes – ~99% as the isotope with 12 nuclear particles and ~1% as the isotope with 13) were conducted almost exclusively on whole rock samples. These values were useful in studying ancient life and the global carbon cycle, but somewhat limited because the organic matter in a rock derives from numerous organisms including plants, algae and bacteria. But in the late 1980s, new methods allowed us to measure carbon isotope values on individual compounds within those rocks, including compounds derived from specific biological sources.  Now, John Eiler and his team at Caltech are developing methods for measuring the values in specific parts or even at a single position in those individual compounds within those rocks.  This isotope mapping of molecules could open up new avenues for determining the temperatures at which ancient animals grew or elide what microorganisms are doing deep in the Earth’s subsurface.

Scientists are going to continue to measure the world around us.  And while that might sound cold and calculating, it is not!  We do this out of our fascination and wonder for nature and our planet.  Just like Galileo’s discovery of Jovian satellites excited our imagination of the cosmos, these new tools are helping us unravel the astonishingly beautiful interactions between our world and the life upon it.

This blog was written by Professor Rich Pancost, Cabot Institute Director, University of Bristol

Prof Rich Pancost

Welcome from the new Director

Left to right: Rich Pancost, Sir John Beddington, Paul Bates

I became the second Director of the Cabot Institute on the 28th of July, taking over from Paul Bates and planning to continue making Cabot one of the world’s premier environmental institutes. The past month has been rather exhilarating in terms of the breadth and quality of my interactions. My experiences have cemented my reasons for assuming this role – the Cabot Institute represents hundreds of brilliant people, working together and working with equally brilliant government, NGO and industry partners to better understand our environment, our relationship to it and the challenges of our co-dependent future. The central aspect of my job as Director is to continue to support those individuals and especially those collaborations.

My first month also confirmed that we have vital, illuminating and challenging ideas to share and we will all benefit from improved communications. Hence, this blog post and the many to follow it.  There are many buried treasures, both clever insights and mature wisdom, on the Cabot Blog, and I encourage new visitors to explore those past posts.  For example, see recent posts on Food Security by Boo Lewis and Energy Markets by Neeraj Oak.  As for me, I’ll be bringing in a combination of personal observations and insights arising from discussions with Cabot partners, as well as ideas emerging in my own discipline.

Penn State University

As a bit of an introduction, I grew up in on a dairy farm in Ohio, and attended Case Western Reserve University, where I dithered back and forth between majors in political science and astrophysics before realising my heart was in Geology…. life decisions are complicated for all of us. I obtained my PhD from Penn State University , using geochemical tools to study past climates, and then continued that work as a post-doctoral researcher at the Royal Netherlands Institute for Sea Research. And in 2000 I joined the Organic Geochemistry Unit  in the School of Chemistry here at Bristol.  Along the way, I played a fair bit of Ultimate (Frisbee ).

I examine organic compounds in a wide range of materials, from soils and plants to microbial mats to ancient rocks. Those organic compounds can be exceptionally well preserved for long periods of time, allowing us to investigate aspects of how the Earth’s biological and chemical systems interact on time scales from tens to millions of years. The topics of my research range from understanding the formation and fate of methane to reconstructing the climate history of the planet (especially during times when carbon dioxide levels and temperatures were higher than those of today). It requires working with a diverse group of people, including climate modellers, mathematicians, social scientists and petroleum geologists.  Those themes will become more prominent in this blog over the coming months, especially as I report back from a few conferences and around the release in late September of the Fifth Report from IPCC Working Group 1: The Physical Basis of Climate Change. But I will also be discussing Environmental Uncertainty and Decision Making: what it means, my personal perspectives on it, and why it is at the heart of the Cabot Institute’s mission.

Finally, this is meant to be an interactive forum.  Do use the comments section and do suggest future topics.  We especially welcome suggestions from our fellow Bristolians for potential visitors and events we could organise in our home town.

Cheers,
Rich

This blog was written by Professor Rich Pancost, Cabot Institute Director, University of Bristol

Rich Pancost