Demand for urban office space is changing: cities need more flexibility

A co-working space. Image: StartupHub/Wikimedia Commons.

What does a good office look like? When cities are thinking about intervening in their city centre office market, the temptation will be to simply build more office space. This will be the right call in some cities, but others may already have a plentiful supply of offices. In these places, the quality of the existing city centre office space will be more important, as well as the extent to which it supports the growing trends for co-working and flexible space.

But before deciding how and when to intervene, cities need to first figure out the specific gaps in their local office market where private developers aren’t responding to existing demand. There’s no single national office market, and the quality of offices on offer varies a lot across the country.

The map below – using data from the Centre for Cities’ recent report Building Blocks: the role of commercial space in Local Industrial Strategies – shows that while 39 per cent of offices in Southampton city centre is of a high quality, this drops to only 9 per cent in Coventry and Leicester.

Source: Non-Domestic Energy Performance Register 2018.

But while this data shows the quality of office buildings, it doesn’t tell us much about what occupiers want from offices. The value of offices is determined by the location, condition, and the amenities they are able to offer to occupiers, and understanding the services occupiers are demanding is key for any office market.

One growing trend in office space is the rise of co-working. Collaborative spaces such as WeWork have recently expanded in London and Manchester and in other large cities around the world.

These have two main advantages for businesses – knowledge spillovers and more efficient use of commercial space. Freelancers can rent desks in these offices, devour free snacks and coffee, and meet and do business with other enterprises who have sat down right across from them. Start-ups and larger firms also use the flexibility to easily acquire (or reduce) desks as their needs change, squeezing as much value as possible out of city centre locations by not paying for excess commercial space.

But it’s not just the big cities which are seeing office space change. In our research for the Building Blocks report, we were struck by how many other cities across England and Wales are already responding to occupier demand by providing features such as co-working or ‘easy in, easy out’ flexible leases. Warrington, Bradford, and Bristol are all embarking on co-working spaces of their own.


Demand for these innovations in office space is therefore widespread across the country. For instance, the non-profit IndyCube provides co-working office space in London, but also in cities like Wakefield, Cardiff, Swansea, Newport and over a dozen towns in Wales. Even in urban areas with very small economies such as Rhyl and Abertillery, it is possible to rent a desk, just as you can in the most up-to-date offices in large cities.

Each city should identify any weaknesses in their office market, and justify whether they should respond to them through their Local Industrial Strategy. In some places, this might be providing more high-quality buildings, and in others, it might just be more co-working and innovative space.

Crawley, for example, has a city centre which lacks large offices of 5,00m2 or more, while the average city has roughly a quarter of its office space in buildings in such large offices. Based on the evidence Centre for Cities laid out in our report on the Economy of the Gatwick Diamond, this suggests Crawley could perhaps justify intervening to supply more office space. Other cities such as Preston, by contrast, may have plenty of large offices – but have a shortage of high-quality buildings or innovations like co-working.

When it comes to interventions, cities should only act when it’s clear there is a market failure and the private sector is not responding to existing demand. Huddersfield and Derby have both supplied small amounts of new office space with features such as co-working, one step at a time so as not to swamp local demand, in response to a shortage of office space in the city centre and a lack of new private sector supply.

This is not to say that “build and the jobs will come” justifications for risky speculative office schemes will work – they won’t, as cities should be intervening in commercial property to respond to demand, rather than trying to create new demand. Improving skills and transport provision will be more important than shiny new skyscrapers in most cities.

But in cities where there is an existing kernel of high-skilled work, making sure this activity has the office space it needs in the city centre is an important step for improving local productivity. As work changes, cities should recognise that their commercial space will need to evolve too.

You can explore city-by-city data on office space with the Centre for Cities’ commercial property dashboard.

Anthony Breach is an economic analyst at the Centre for Cities, on whose blog this post first appeared.

 
 
 
 

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.