Beyond Preston: How local wealth building is taking the UK by storm

Preston Bus Station. Image: Getty.

The Preston Model, which has seen the Lancashire town rise from the bottom 20 per cent of the deprivation index to be named the UK’s most improved city, has become the poster child for an insurgent economic approach known as “local wealth building”. This uses the levers of the local state to reorganise the economy away from neoliberalism and towards local economies rooted in social, economic and environmental justice.

While the programme’s success in Preston is obvious from the widespread interest it has received among policy makers, politicians and commentators, local wealth building is also being explored elsewhere to confront economic failure, social hardship, wealth extraction and environmental degradation. 

In Manchester, the programme first began in 2008, pioneered by the Centre for Local Economic Strategies (CLES) and Manchester City Council. Together they grew the number of organisations based in the city that were competing and winning contracts from the city government by 50 per cent. 

From this early work on procurement, local wealth building initiatives began to focus on the idea of “predistribution”, a counterpoint to the redistributive policies, such as ”inclusive growth”, a current zeitgeist among policy makers that advocates a weak form of redistributing wealth through taxes and benefits after the fact of its creation. Local wealth building instead aims to construct an inclusive economy where wealth is generated by and for all citizens. In doing so, it slays the neoliberal dragon of trickle-down economics and rebuilds wealth from the bottom-up rather than the top-down.

To achieve this, local wealth building follows a model based on “anchor institutions”, where local businesses and socially-focused enterprises outside the local area compete for commercial contracts from institutions such as housing organisations, universities, schools and hospitals. These institutions hold a unique position in the local economy, as they employ people, buy things, hold property and assets and are unlikely to relocate from the local area. 

The Preston Model is a welcome indication that this anchor approach can work. But in places beyond Preston, this agenda has taken diverse forms; what unites these places is five central principles. These are:

  • Plural ownership of the economy – deepening the relationship between the production of wealth and those who benefit from it. This means returning public services to direct democratic control by insourcing public goods and services. It’s also about developing cooperatives and locally owned or socially focussed enterprises in the public and commercial economy.
  • Making financial power work for local places – increasing flows of investment within local economies by, for example, directing the funds from local authority pensions away from global markets and towards local schemes and community-owned banks and credit unions.
  • Fair employment and just labour markets – working within large anchor institutions and their human resource departments to pay the living wage, adopt inclusive employment practices, recruit from lower income areas, build secure progression routes for workers and ensure union recognition.
  • Progressive procurement of goods and services – developing a dense local supply chain of local enterprises, employee-owned businesses, social enterprises, cooperatives and other forms of social ownership that can provide goods and services to large local anchor organisations.
  • Socially productive use of land and property – ensuring that local assets including those held by anchor organisations are owned, managed and developed equitably, so that local communities can harness any financial gain from these assets.

This movement is growing rapidly; CLES is working with Gateshead, Sunderland, Darlington, Hartlepool, Wakefield, Leeds, Calderdale, Kirklees, Oldham, Wigan, Salford, Birmingham, Lewisham, Wirral and Southampton to adopt local wealth building initiatives involving a range of anchors.


In London, Islington is deepening its progressive procurement practices and examining ways to tackle the rentier economy and speculative land and property ownership. In Gateshead, the council has a longstanding process of insourcing. In Wales the first Minister has made a commitment to ensure a programme of local wealth building, and in Scotland, local government is establishing a pilot linking local wealth building to a growth deal. Elsewhere, the NHS has adopted the anchor approach as part of its long term plan.

In the coming years as this movement becomes more embedded in regions across the UK, the “Gateshead model” or the “Wirral model” should achieve as much attention as the pioneers of Preston. The Labour Party has established a community wealth building unit and the ongoing work of the government’s inclusive economic partnership magnifies the local wealth building agenda. In the age of experiments, the lessons of Preston, Gateshead, Islington and elsewhere must become a new mainstream for all forms of local economic development.

Jonty Leibowitz is a researcher and Neil McInroy is the chief executive at the Centre for Local Economic Strategies (CLES), the think and do tank working on progressive economics for people and places. 

 
 
 
 

The IPPC report on the melting ice caps makes for terrifying reading

A Greeland iceberg, 2007. Image: Getty.

Earlier this year, the Intergovernmental Panel on Climate Change (IPCC) – the UN body responsible for communicating the science of climate breakdown – released its long-awaited Special Report on the Ocean and Cryosphere in a Changing Climate.

Based on almost 7,000 peer-reviewed research articles, the report is a cutting-edge crash course in how human-caused climate breakdown is changing our ice and oceans and what it means for humanity and the living planet. In a nutshell, the news isn’t good.

Cryosphere in decline

Most of us rarely come into contact with the cryosphere, but it is a critical part of our climate system. The term refers to the frozen parts of our planet – the great ice sheets of Greenland and Antarctica, the icebergs that break off and drift in the oceans, the glaciers on our high mountain ranges, our winter snow, the ice on lakes and the polar oceans, and the frozen ground in much of the Arctic landscape called permafrost.

The cryosphere is shrinking. Snow cover is reducing, glaciers and ice sheets are melting and permafrost is thawing. We’ve known this for most of my 25-year career, but the report highlights that melting is accelerating, with potentially disastrous consequences for humanity and marine and high mountain ecosystems.

At the moment, we’re on track to lose more than half of all the permafrost by the end of the century. Thousands of roads and buildings sit on this frozen soil – and their foundations are slowly transitioning to mud. Permafrost also stores almost twice the amount of carbon as is present in the atmosphere. While increased plant growth may be able to offset some of the release of carbon from newly thawed soils, much will be released to the atmosphere, significantly accelerating the pace of global heating.

Sea ice is declining rapidly, and an ice-free Arctic ocean will become a regular summer occurrence as things stand. Indigenous peoples who live in the Arctic are already having to change how they hunt and travel, and some coastal communities are already planning for relocation. Populations of seals, walruses, polar bears, whales and other mammals and sea birds who depend on the ice may crash if sea ice is regularly absent. And as water in its bright-white solid form is much more effective at reflecting heat from the sun, its rapid loss is also accelerating global heating.

Glaciers are also melting. If emissions continue on their current trajectory, smaller glaciers will shrink by more than 80 per cent by the end of the century. This retreat will place increasing strain on the hundreds of millions of people globally who rely on glaciers for water, agriculture, and power. Dangerous landslides, avalanches, rockfalls and floods will become increasingly normal in mountain areas.


Rising oceans, rising problems

All this melting ice means that sea levels are rising. While seas rose globally by around 15cm during the 20th century, they’re now rising more than twice as fast –- and this rate is accelerating.

Thanks to research from myself and others, we now better understand how Antarctica and Greenland’s ice sheets interact with the oceans. As a result, the latest report has upgraded its long-term estimates for how much sea level is expected to rise. Uncertainties still remain, but we’re headed for a rise of between 60 and 110cm by 2100.

Of course, sea level isn’t static. Intense rainfall and cyclones – themselves exacerbated by climate breakdown – can cause water to surge metres above the normal level. The IPCC’s report is very clear: these extreme storm surges we used to expect once per century will now be expected every year by mid-century. In addition to rapidly curbing emissions, we must invest millions to protect at-risk coastal and low-lying areas from flooding and loss of life.

Ocean ecosystems

Up to now, the ocean has taken up more than 90 per cent of the excess heat in the global climate system. Warming to date has already reduced the mixing between water layers and, as a consequence, has reduced the supply of oxygen and nutrients for marine life. By 2100 the ocean will take up five to seven times more heat than it has done in the past 50 years if we don’t change our emissions trajectory. Marine heatwaves are also projected to be more intense, last longer and occur 50 times more often. To top it off, the ocean is becoming more acidic as it continues to absorb a proportion of the carbon dioxide we emit.

Collectively, these pressures place marine life across the globe under unprecedented threat. Some species may move to new waters, but others less able to adapt will decline or even die out. This could cause major problems for communities that depend on local seafood. As it stands, coral reefs – beautiful ecosystems that support thousands of species – will be nearly totally wiped out by the end of the century.

Between the lines

While the document makes some striking statements, it is actually relatively conservative with its conclusions – perhaps because it had to be approved by the 195 nations that ratify the IPCC’s reports. Right now, I would expect that sea level rise and ice melt will occur faster than the report predicts. Ten years ago, I might have said the opposite. But the latest science is painting an increasingly grave picture for the future of our oceans and cryosphere – particularly if we carry on with “business as usual”.

The difference between 1.5°C and 2°C of heating is especially important for the icy poles, which warm much faster than the global average. At 1.5°C of warming, the probability of an ice-free September in the Arctic ocean is one in 100. But at 2°C, we’d expect to see this happening about one-third of the time. Rising sea levels, ocean warming and acidification, melting glaciers, and permafrost also will also happen faster – and with it, the risks to humanity and the living planet increase. It’s up to us and the leaders we choose to stem the rising tide of climate and ecological breakdown.

Mark Brandon, Professor of Polar Oceanography, The Open University.

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