Why do flood defences fail?

More than 40,000 people were forced to leave their homes after Storm Desmond caused devastating floods and wreaked havoc in north-west England. Initial indications were that the storm may have caused the heaviest local daily rainfall on record in the UK. As much as £45m has been spent on flood defences in the region in the previous ten years and yet the rainfall still proved overwhelming. So what should we actually expect from flood defence measures in this kind of situation? And why do they sometimes fail?

We know that floods can and will happen. Yet we live and work and put our crucial societal infrastructure in places that could get flooded. Instead of keeping our entire society away from rivers and their floodplains, we accept flood risks because living in lowlands has benefits for society that outweigh the costs of flood damage. But knowing how much risk to take is a tricky business. And even when there is an overall benefit for society, the consequences for individuals can be devastating.

We also need to calculate risks when we build flood defences. We usually protect ourselves from some flood damage by building structures like flood walls and river or tidal barriers to keep rising waters away from populated areas, and storage reservoirs and canals to capture excess water and channel it away. But these structures are only designed to keep out waters from typical-sized floods. Bigger defences that could protect us from the largest possible floods, which may only happen once every 100 years, would be much more expensive to build and so we choose to accept this risk as less than the costs.

Balancing the costs and benefits

In the UK, the Environment Agency works with local communities to assess the trade off between the costs of flood protection measures, and the benefits of avoiding flood damage. We can estimate the lifetime benefits of different proposed flood protection structures in the face of typical-sized floods, as well as the results of doing nothing. On the other side of the ledger, we can also estimate the structures’ construction and maintenance costs.

In some cases, flood protection measures can be designed so that if they fail, they do the least damage possible, or at least avoid catastrophic damage. For example, a flood protection wall can be built so that if flood waters run over it they run into a park rather than residential streets or commercial premises. And secondary flood walls outside the main wall can redirect some of the overflow back towards the river channel.

 

Thames Barrier: big costs but bigger benefits.
Ross Angus/Flickr, CC BY-SA

The Environment Agency puts the highest priority on the projects with the largest benefits for the smallest costs. Deciding where that threshold should be set is a very important social decision, because it provides protection to some but not all parts of our communities. Communities and businesses need to be well-informed about the reasons for those thresholds, and their likely consequences.

We also protect ourselves from flood damage in other ways. Zoning rules prevent valuable assets such as houses and businesses being built where there is an exceptionally high flood risk. Through land management, we can choose to increase the amount of wooded land, which can reduce the impact of smaller floods. And flood forecasting alerts emergency services and helps communities rapidly move people and their portable valuables out of the way.

Always some risk

It’s important to realise that since flood protection measures never eliminate all the risks, there are always extra costs on some in society from exceptional events such as Storm Desmond, which produce very large floods that overwhelm protection measures. The costs of damage from these exceptional floods are difficult to estimate. Since these large floods have been rare in the past, our records of them are very limited, and we are not sure how often they will occur in the future or how much damage will they cause. We also know that the climate is changing, as are the risks of severe floods, and we are still quite uncertain about how this will affect extreme rainfall.

 

At the same time we know that it’s very hard to judge the risk from catastrophic events. For example, we are more likely to be afraid of catastrophic events such as nuclear radiation accidents or terrorist attacks, but do not worry so much about much larger total losses from smaller events that occur more often, such as floods.

Although the process of balancing costs against benefits seems clear and rational, choosing the best flood protection structure is not straightforward. Social attitudes to risk are complicated, and it’s difficult not to be emotionally involved if your home or livelihood are at risk.
The Conversation

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This blog is written by Cabot Institute member Dr Ross Woods, a Senior Lecturer in Water and Environmental Engineering, University of Bristol.  This article was originally published on The Conversation. Read the original article.

Ross Woods

COP21 daily report: While the politicians negotiate, the science does not stop

Cabot Institute Director Professor Rich Pancost will be attending COP21 in Paris as part of the Bristol city-wide team, including the Mayor of Bristol, representatives from Bristol City Council and the Bristol Green Capital Partnership. He and other Cabot Institute members will be writing blogs during COP21, reflecting on what is happening in Paris, especially in the Paris and Bristol co-hosted Cities and Regions Pavilion, and also on the conclusion to Bristol’s year as the European Green Capital.  Follow #UoBGreen and #COP21 for live updates from the University of Bristol.  All blogs in the series are linked to at the bottom of this blog.

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I am on the train from Bristol Temple Meads to Paddington and then on to Paris. It seems appropriate leaving from a station that was built by Brunel, a symbol of the industrial revolution but also innovation. Tomorrow, I will be joining George Ferguson, Stephen Hilton of Bristol City Council, Amy Robinson of Low Carbon Southwest and others at the Sustainable Innovation Forum. I appreciate that addressing climate change means changing some aspects of how we live, but it also requires some fundamentally new technology; I am excited to see where the cutting edge thinking is.  Meanwhile, over a relatively calm weekend, the draft accord has been made public – there have been some significant advances but also a ways to go.  Negotiations will be continuing in earnest!  More on all of that tomorrow (I hope – it will be a long day).  



Today, however, my attention is elsewhere as our postgrads, research fellows and academic staff make their final preparations for the Annual Meeting of the American Geophysical Union (AGU).  The science goes on – as it must and will, regardless of the Paris negotiations. We still know far too little about the complexity of this magnificent planet, how to best live on it sustainably, and the imminent and the longer-term impacts of climate and wider environmental change.  
In my own research group (the OGU), my colleagues will be talking about increases in extreme rainfall during a past global warming event that is potentially analogous to the warming of today (see Matthew Carmichael’s research); the latest reconstructions of how carbon dioxide concentrations have changed over the past 3 million years (see Marcus Badger’s research); and the long-term controls on the hydrological cycle of the Mediterranean region (see Jan Peter Mayser’s research). All of them are collaborating with climate modellers in BRIDGE. Others in BRIDGE will be discussing how to improve the next generation of Earth System models, how to forecast land use impacts on the atmosphere, and examining the biological consequences of past ocean acidification events.  Anita Ganesan and Matt Rigby are both presenting talks on methane cycling and monitoring – a reminder that CO2 is not the only greenhouse gas and that cars and cities are not the only cause of global warming.  Our glaciologists are exploring the future of the ice sheets and glaciers. Our civil engineers and geographers are presenting the latest research on all aspects of the hydrological cycle: improved models of catchments; better flood and drought forecasting; and better understanding how land use change has affected the chemistry of our rivers.  


Through all of this, there is a persistent and recurring theme of constraining uncertainty as well as understanding uncertainty in the context of decision-making. Scientists, industry and leaders must develop better tools for navigating environmental uncertainty, a focus of the Cabot Institute in 2015 and for which the need has been aptly demonstrated by Storm Desmond’s impact on Cumbria.
It is a remarkable variety of research – and that is just a sample from the University of Bristol.  
I’m never apologetic about promoting Bristol achievements and activity – it is what I know best, it is world-leading and it is my job!  Here, however, singling out these Bristol-centric contributions makes a stronger point; the above are just a few examples of the research conducted in just one institution.  Some 20,000 scientists will attend AGU!  There is profound and diverse effort devoted to understanding our planet and improving how we live upon it.


A fantastic example of some research being led by our colleagues will be on display in London on Monday as part of a Royal Society Discussion Meeting on the Biological and Climatic Impacts of Ocean Trace Element Chemistry. The event is co-convened by our Oxford friend, colleague and frequent collaborator, Gideon Henderson. Chatting to Gideon a few days ago, he emphasised the importance of the ocean in regulating our climate: ‘The oceans consume 27% of the carbon we emit, after all, and the ocean biosphere naturally consumes 11 Gtonnes of C per year.’ This is a huge issue. Currently, the ocean buffers the atmosphere against human action – but it is unclear how long this will continue.  Moreover, the ocean does so at a cost:

 

  • As the ocean absorbs energy, it warms. 
  • As the ocean absorbs this carbon, its pH declines. 
  • As marine phytoplankton assimilate this carbon and sink, they change the chemical state of the ocean, from top to bottom, creating oxygen dead zones and transforming the redox state of trace but biologically vital elements.   

 

This research is an important reminder that the issues associated with rising greenhouse gas concentrations encompass more than just the weather – greenhouse gases are changing the chemistry, physics and biology of our planet, with unclear consequences.  Their full synergistic effects, through these complex biogeochemical systems, remain difficult to anticipate. Their consequences difficult to predict. 
 
And so, as the negotiations continue, we continue our research.  On the oceans and the tropical rain forests; the deserts of the Sahara and the Arctic; the peatlands and permafrost; the soils and the bedrock beneath; the atmosphere and the cryosphere.  On the plants, animals and microorganisms that coexist with and co-regulate these ecosystems.  And of course, the people dependent on them.
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This blog is by Prof Rich Pancost, Director of the Cabot Institute at the University of Bristol.  For more information about the University of Bristol at COP21, please visit bristol.ac.uk/green-capital

Prof Rich Pancost

 

This blog is part of a COP21 daily report series. View other blogs in the series below:
 
Monday 30 November: COP21 daily report