How to end congestion without giving up the car

Well, this looks healthy: Paris, 2007. Image: Getty.

Cars are spectacularly under-used. This may seem slightly counterintuitive if you were stuck in a traffic jam getting to work this morning, but the cold, naked fact is that an average car drives barely 50 minutes every day. For more than 23 hours it sits idle. When it’s on the road, a car carries an average of only 1.2 to 1.5 passengers.

Put differently, cars do what they were built for only about 3.5 per cent of the time, and then with 25 to 30% of the passengers they could carry. So inevitably lonely drivers find themselves stuck in congestion, breathing polluted air – not to even mention the impact of “individual mobility”, as experts call driving a car, on CO2 emissions and climate change.

That we accept this is a testament to the huge value we attribute to the freedom of movement that having our own car provides. Yet it is indisputably unsustainable, and increasingly so as car travel is increasingly undermined by its own success. Drivers in many world cities spend 25-41 per cent of time stuck in congestion during peak hours, the cost of which has been estimated at 0.8 per cent of GDP across the US, Germany, Britain and France.

How many of these do we really need? Image: International Transport Forum.
 

The same mobility with 10 per cent of today’s cars

Enter the sharing economy, ever on the look-out for under-utilised assets that can be made accessible for use with the help of today’s digital networking possibilities. Countless car sharing and ridesharing operators with a bewildering array of business models promise to make car travel as convenient as with your own car, and without the hassle. Could shared mobility provide the solution for urban mobility?

In fact it seems it can. Researchers at the International Transport Forum used real mobility data to create sophisticated computer model of mobility patterns over a typical 24-hour working day in the city of Lisbon in Portugal. They then replaced all private cars with a fleet of shared vehicles.

The result stunned even the experts: The shared fleets provided all the trips needed with 10 per cent or less of the current number of private cars, in some scenarios with 3 per cent. These results have been confirmed in four studies to date, testing different configurations of services and using data from cities with different density, topography and infrastructure. A shared mobility simulation for Helsinki in Finland was released in October; a study for Auckland, New Zealand, followed in November.

An infographic. Image: International Transport Forum.

Parks, not car parks

Imagine for a moment a world in which 9 of 10 cars have disappeared from your city’s streets. The first thing you’d notice is how much space cars occupy. In the simulation, 95 per cent of the land currently used for on-street car parking was freed for wider sidewalks, more cycling lanes, parks instead of car parks.

Congestion also disappears. The shared vehicles clock many more kilometres, but the overall distance driven falls by more than a third. And with fewer cars driving less overall, CO2 emissions from car traffic would also fall by a third – without any new technology in place. There would be knock-on effects: vehicles drive more, so need to be replaced sooner, so advances in fuel-saving or emissions reduction become relevant more quickly.

One of the most fascinating simulation results is the impact of shared mobility on social equality. Transport services are a means to an end – access to jobs, schools, shops, health services and so on. Private cars provide great access for those who have them. Those who don’t may find themselves having to refuse a better paid job because it’s simply not reachable by public transport.

Lisbon. Image: International Transport Forum.

The dark red areas in the maps of Lisbon above show the points from which 75 per cent or more of health services can be reached within 30 minutes. The light areas indicate that less than 25 per cent of services are within a 30 minute reach.

With on-demand shared mobility, almost all citizens have the highest level of access to health care, no matter where they are. The Gini coefficient, a widely-used indicator for inequality, drops from 0.26 now to 0.08 or almost full equality of access. The improvements for access to jobs and education are in the same order of magnitude.


The end of Public Transport?

So, potentially, on-demand shared mobility could offer cities a way out of traffic gridlock without making people less mobile. Will it happen?

A lot of political will is needed to launch such an urban mobility revolution. Much depends on adroitly setting the right framework in a way that ensures society reaps the benefits. For one thing, it will require regulation on how travel requests and rides are matched. The research suggests that a central dispatcher works best, rather than several. There could be multiple operators for shared taxis, taxi-buses and other services, however.

And what will happen to public transport? It’s hard to imagine traditional bus lines following fixed routes on rigid timetables, much like 19th century steam trains, competing successfully with on-demand services. On the other hand, nothing keeps city-backed public transport operators from offering innovative services themselves – for instance smaller buses that swarm around the city or oscillate along corridors, picking up people along the way based on itineraries constantly optimised by algorithms.

Transport as a service. Image: Shared User Mobility Center.

And the new shared services can even work well in tandem with public transport. The ITF studies show that shared mobility services have the biggest impact in combination with high-capacity public transport – they can provide effective feeder services for metro lines or commuter rail.

Surveys and focus groups conducted in several cities showed that users are attracted by the idea. But the shared mobility service will have to be set up – and promoted – to attract car owners, not people who use public transport.

How do we get there?

The “what if” approach of replacing all private cars with shared vehicles can demonstrate what is possible, but it doesn’t do much to help cities get there. With 100 per cent shared mobility, the price of a journey could be 50 per cent less than today on public transport, even without subsidies.


But there is a risk that such systems will falter during the transition – as happened in Helsinki, where the Kutsuplus on-demand bus service folded in 2015, caught between high costs and limited reach. In Boston, a similar service called Bridj gave up in April of 2017 (but is now planning a comeback in Sydney).

To succeed, shared mobility would probably need at least about 20 per cent market share to have sufficient scale to keep costs low enough and significantly reduce traffic (and emissions). When surveyed, users made it clear that while they love the idea in principle, the two things that matter to them are service quality and price.

Yet city planners can take courage from another answer. Asked whether they would be less likely to use a shared vehicle if it had many riders on board, the opposite turned out to be the case. People don’t mind full cars but are not keen on sharing a ride with just one other person – for fear they might be engaged in conversation.

If that turned out to be true, it would at least help improve capacity utilisation.

Hans Michael Kloth, a former journalist with news magazine Der Spiegel, now works at the International Transport forum, a policy think thank linked to the OECD in Paris.

 
 
 
 

Here’s why we’re using a car wash to drill into the world’s highest glacier on Everest

Everest. Image: Getty.

For nearly 100 years, Mount Everest has been a source of fascination for explorers and researchers alike. While the former have been determined to conquer “goddess mother of the world” – as it is known in Tibet – the latter have worked to uncover the secrets that lie beneath its surface.

Our research team is no different. We are the first group trying to develop understanding of the glaciers on the flanks of Everest by drilling deep into their interior.

We are particularly interested in Khumbu Glacier, the highest glacier in the world and one of the largest in the region. Its source is the Western Cwm of Mount Everest, and the glacier flows down the mountain’s southern flanks, from an elevation of around 7,000 metres down to 4,900 metres above sea level at its terminus (the “end”).

Though we know a lot about its surface, at present we know just about nothing about the inside of Khumbu. Nothing is known about the temperature of the ice deeper than around 20 metres beneath the surface, for example, nor about how the ice moves (“deforms”) at depth.

Khumbu is covered with a debris layer (which varies in thickness by up to four metres) that affects how the surface melts, and produces a complex topography hosting large ponds and steep ice cliffs. Satellite observations have helped us to understand the surface of high-elevation debris-covered glaciers like Khumbu, but the difficult terrain makes it very hard to investigate anything below that surface. Yet this is where the processes of glacier movement originate.

Satellite image of Khumbu glacier in September 2013. Image: NASA.

Scientists have done plenty of ice drilling in the past, notably into the Antarctic and Greenland ice sheets. However this is a very different kind of investigation. The glaciers of the Himalayas and Andes are physically distinctive, and supply water to millions of people. It is important to learn from Greenland and Antarctica, – where we are finding out how melting ice sheets will contribute to rising sea levels, for example – but there we are answering different questions that relate to things such as rapid ice motion and the disintegration of floating ice shelves. With the glaciers we are still working on obtaining fairly basic information which has the capacity to make substantial improvements to model accuracy, and our understanding of how these glaciers are being, and will be, affected by climate change.

Under pressure

So how does one break into a glacier? To drill a hole into rock you break it up mechanically. But because ice has a far lower melting point, it is possible to melt boreholes through it. To do this, we use hot, pressurised water.

Conveniently, there is a pre-existing assembly to supply hot water under pressure – in car washes. We’ve been using these for over two decades now to drill into ice, but our latest collaboration with manufacturer Kärcher – which we are now testing at Khumbu – involves a few minor alterations to enable sufficient hot water to be pressurised for drilling higher (up to 6,000 metres above sea level is envisioned) and possibly deeper than before. Indeed, we are very pleased to reveal that our recent fieldwork at Khumbu has resulted in a borehole being drilled to a depth of about 190 metres below the surface.

Drilling into the glacier. Image: author provided.

Even without installing experiments, just drilling the borehole tells us something about the glacier. For example, if the water jet progresses smoothly to its base then we know the ice is uniform and largely debris-free. If drilling is interrupted, then we have hit an obstacle – likely rocks being transported within the ice. In 2017, we hit a layer like this some 12 times at one particular location and eventually had to give up drilling at that site. Yet this spatially-extensive blockage usefully revealed that the site was carrying a thick layer of debris deep within the ice.

Once the hole has been opened up, we take a video image – using an optical televiewer adapted from oil industry use by Robertson Geologging – of its interior to investigate the glacier’s internal structure. We then install various probes that provide data for several months to years. These include ice temperature, internal deformation, water presence measurements, and ice-bed contact pressure.


All of this information is crucial to determine and model how these kinds of glaciers move and melt. Recent studies have found that the melt rate and water contribution of high-elevation glaciers are currently increasing, because atmospheric warming is even stronger in mountain regions. However, a threshold will be reached where there is too little glacial mass remaining, and the glacial contribution to rivers will decrease rapidly – possibly within the next few decades for a large number of glaciers. This is particularly significant in the Himalayas because meltwater from glaciers such as Khumbu contributes to rivers such as the Brahmaputra and the Ganges, which provide water to billions of people in the foothills of the Himalaya.

Once we have all the temperature and tilt data, we will be able to tell how fast, and the processes by which, the glacier is moving. Then we can feed this information into state-of-the-art computer models of glacier behaviour to predict more accurately how these societally critical glaciers will respond as air temperatures continue to rise.

The ConversationThis is a big and difficult issue to address and it will take time. Even once drilled and imaged, our borehole experiments take several months to settle and run. However, we are confident that these data, when available, will change how the world sees its highest glacier.

Katie Miles, PhD Researcher, Aberystwyth University and Bryn Hubbard, Professor of Glaciology, Aberystwyth University.

This article was originally published on The Conversation. Read the original article.