Alpine glacier – endangered species? (Pic: I.Quaile)

It was with mixed feelings that I read an article drawn to my attention by a colleague earlier in the week.

“Protecting Ice Memory” is the subject –a description of a new project to create a “global archive of glacial ice for future generations”.

I am generally enthusiastic about all projects concerning ice. The worrying thing is the reason why this project has been deemed necessary.

History melting

“The goal is to build the world’s first library of ice archives extracted from glaciers which are threatened by global warming”. There we have it. Another frightening acknowledgement of the extent and speed of global change.

How sad that our human-induced warming is threatening our ice, especially here in the European Alps, where we do not have as much ice as in some other parts of the globe. How good that we have the technology to save some of it for posterity. How frustrating that while we also have the technology to shift to a zero-carbon economy and stop the ice melting, we are not actually doing it anything like fast enough.

Starting on Monday August 15th and carrying on until early September, an international team of glaciologists and engineers (French, Italian, Russian and American) will be travelling to Mont Blanc, in particular to the “Col du Dome” glacier area, which is 4,300 metres or 14,108 feet up. They will be drilling the first ice cores for the “Protecting Ice Memory” project.

Some glaciers are being covered in summer to stop them melting, this one I saw in Switzerland. Proved ineffective. (I.Quaile)

Saving the cores

The team will be coordinated by Patrick Ginot from the French Research Institute for Development (IRD), working within the UGA-CNRS Laboratory of Glaciology and Environmental Geophysics (LGGE), and Jerome Chappelaz, director of Research at the CMRS and working within ths same laboratory.

The team will be extracting three ice cores each 130 metres long. These will be taken down by helicopter and taken to the LGGE in Grenoble. Clearly they will have to kept very cold during the process.

In 2019 (why only then, I wonder?), one core will be analysed to start a database which is ultimately to be made available to the whole world scientific community.

The other two will be transported by ship to ANTARCTICA. Yes, you read correctly. There, they will be taken on tracked vehicles across the high plateaus to be stored at the Concordia station, which is run by the French Paul-Emile-Victor Polar Institute (IPEV) and its Italian partner, the National Antarctic Research Programme (PNRA)

In the long term, dozens of ice cores are to be stored in a snow cave at -54° Celsius, which the project describes as “the most reliable and natural freezer in the world”.

The Mont Blanc glacier is the first step. The next will be carried out in 2017 on the Illimani glacier in the Bolivian Andes.

“Where’s my ice”? (Swiss Alps, Pic: I.Quaile)

Global operation

It seems other countries with access to glaciers are also hoping to join the project, including Germany, Austria, Switzerland, Brazil, the USA, Russia, China, Nepal and Canada. That sounds like a real mega-project.

I have commented often enough here on the Ice Blog on the dwindling ice in my own favourite hiking territory in the German and Swiss Alps. Last week it was the turn of the New Zealand Alps to be the focus of this rather sadly motivated attention.

Ice just a memory? Iceblogger in her element in Switzerland. (Pic. I.Quaile)

The scientists who came up with the project had the idea after observing a rise in temperatures on several glaciers. At ten year intervals, they say the temperature near the glaciers on the Col du Dome and Illimani in the Andes has risen between 1.5 degrees and 2 degrees (Those figures sound familiar from somewhere…)

“At the current rate, we are forecasting that their surface will undergo systematic melting over the summer in the next few years and decades. Due to this melting and the percolation of meltwater through the underlying layers of snow, these are unique pages in the history of our environment which will be lost forever”, says the project description.

Iceblogger in the Svalbard Seed Vault

The scientists compare their project to the Svalbard Global Seed Vault on the Norwegian Arctic island of Spitsbergen. Before I read that part, this very comparison had already come to my mind. I had a rare opportunity to visit that vault a couple of years ago.

Svalbard to Antarctica

But one of the very worrying things in that connection is that even that “secure coldspot” has in turn been affected by permafrost melt – at least at a level close to the surface, which caused damage to the entrance area in the early stages.

Will the Svalbard vault ultimately have to be moved to the even colder Antarctic at some point in the future, one might wonder?

I remember a visit to the Alfred-Wegener Institute in Bremerhaven, Germany’s polar agency. One of the highlights was a look into the laboratory where ice cores are processed. Clearly, these provide invaluable evidence of how our planet and life on it have developed. Climate and environmental archives of a quite unique nature.

“Our generation of scientists, which bears witness to global warming, has a particular responsibility to future generations. That is why we will be donating these ice samples from the world’s most fragile glaciers to the scientific community of the decades and centuries to come, when these glaciers will have disappeared or lost their data quality”, says Carlo Barbante, the Italian project initiator and Director of the Instutite for the Dynamics of Environmental Processes – CNS, Ca’Foscari University of Venice”. What a sobering thought – and a daunting task.

And what an inspiring campaign to rescue what it seems we will not be able to save in time in the natural world.

Projects like this cost a lot of money. It is relying on private sponsors. The current European project has funding. The Université Grenoble Alpes foundation is now running a campaign to fund the Bolivian expedition.

Here’s hoping the money will be forthcoming.

And here’s hoping the international community will speed up efforts to halt global warming before we have to create archives to try to document all the ecosystems, species and habitats we are losing faster than we can count them.

Arctic phone box – a chilly wind DOWN from the pole! (pic: I.Quaile)

During my first trip to Australia around 25 years ago, I was standing outside a phone box (there are still such things even in this smartphone age) one evening, in a chilly wind.

“That wind’s coming straight up off the pole”, a local told me. Up off the pole? That was a weird image for a visitor from the northern hemisphere. It figures, the wind blows up rather than down from the pole when you’re at the other end of the world.

A few years later, during a visit to New Zealand, I was tickled to find there were “alps” to visit, with glaciers, reminiscent of some of my favourite hiking territory in Switzerland. I haven’t heard much about them since.

There hasn’t been much about New Zealand in the media here in Europe, except when earthquakes strike, or – the latest popular summertime story – the decision to exterminate all “alien” predators like mice, rats and possums.

But this week I came across a story by the New Zealand Herald on Twitter, entitled “warning sounds for vanishing glaciers”.  Needless to say this set the alarm bells ringing with the Iceblogger.

Iceblogger, Iceblocker?

It seems these beautiful icy regions have also been affected considerably by climate warming.

Rapid retreat

The South Island of New Zealand is home to snowy mountains and picturesque glaciers. The article by Jamie Morton describes how the glaciers have been retreating massively since 2011. The pictures, taken by Brian Anderson of Victoria University’s Antarctic Research Centre, show a dramatic change. The latest measurements for Fox Glacier and Franz Josef Glacier, the ones I visited, show they have “shrunk to record levels”, the article quotes Dr. Anderson.

I must delve into my photo archive at home for pics taken when I was there in 2000 and compare them with the latest. I have the feeling the comparison would be a sobering one.

Twice a year, scientists conduct surveys of the snowlines and glacier retreats in New Zealand’s Southern Alps. The measurements take place at the end of winter, and again at the end of summer.

Glaciers – beautiful but highly endangered in our warming age. (Pic. I.Quaile)

The scientist says the snow accumulation on the glaciers was average in winter 2015, but high by the end of the very warm summer in 2016.

In the last five years, it seems the Fox Glacier has retreated 750 meters, the Franz Josef as much as 1.5 kilometres.

The ice volume in the Southern Alps has decreased from 170 cu km in the 1890s to a current 36.1, and is predicted to go down to between 7 and 12 cu km, by 2100. Yikes.

The last dramatic loss of ice was during the summer of 2010/2011, under the influence of a strong La Nina climate system – one of the strongest ever recorded, according to Jamie Morton. The latest ice loss appears to be similar in amount.

“Based on regional warming projections of 1.5C to 2.5 C, it has been projected by glaciologists Valentina Radic and Regine Hock that just 7 to 12 cu km of ice would remain on the alps by the end of this century, Morton writes.

The snowline has also moved up to “exceptionally high levels”, Morton quotes Dr. Andrew Lorry from the National Institute of Water and Atmosphere (NIWA).

Warming water, melting ice

The article says before last summer, the experts expected the El Nino to have a major impact. But instead, it was unseasonably warm sea surface temperatures in the Tasman Sea, bringing warmer air over land, that caused the damage.

With temperatures higher than average so far this season, it seems likely more ice and snow will be melting.

Are we surprised by all this? Perhaps not. Concerned? Saddened? Definitely. Clearly the cold wind blowing up off the south pole, like the one blowing down from the north, is no longer enough to secure those icy areas of New Zealand.

Of course emissions reductions have to take place across the board. Local melting is not only caused by local actions. Still, countries who profit from their ice and snow, like New Zealand, where the alps are an important tourist attraction, can be expected to set a good example in implementing measures to halt the warming. The “Climate action tracker”, an independent science-based assessment of country’s emissions targets and actual action, rates New Zealand’s INDC 2030 target as “inadequate”. That means its commitment is not in line with a “fair” approach to reach a 2° C maximum temperature rise pathway.

“If most other countries followed the New Zealand approach, global warming would exceed 3–4°C”, the website says.

Maybe I better not wait too long for another visit to those New Zealand glaciers. At this rate, I will hardly even need my snow boots.

Redundant? (Pic: I.Quaile)

Can we halt Arctic ice melt? (Pic: I.Quaile, Greenland)

I had a very interesting high-profile visitor here at Deutsche Welle this week. Bonn, John Le Carré’s “Small Town in Germany” is this country’s UN city nowadays, home to organizations like the climate secretariat UNFCCC and the Convention on Migratory Species, CMS. This year marks 20 years of the former German capital in that new UN role. Fortunately for me and my colleagues, it brings a lot of interesting people to the city.

The University and the City of Bonn have been running a series of lectures by members of the Scientific Advisory Board of the United Nations Secretary-General Ban Ki-Moon this year, under the heading “Global Solutions for Sustainable Development”. This week, it was the turn of Susan Avery, who was President and Director of the Woodshole Oceanographic Institution in the USA until last year. She has been on the advisory board to Ban Ki-Moon for the last three years and she and the other advisors are just finishing their report, so it was great to have the opportunity to talk in length.

Susan Avery enthralls the audience at Bonn University. (Pic: C.Koenig/ City of Bonn)

Sea and sky as dancing partners

Her lecture was about the importance of the ocean with regard to climate, but she also talked to me about a whole range of ocean-related issues in an interview to be broadcast on our Living Planet programme, starting next week.

Susan Avery is an atmospheric scientist, (the first to head a major oceanographic institution, she told me). She has a very attractive image to describe how the atmosphere and the ocean relate to each other:

“In our planetary system we have two major fluids, the ocean and the atmosphere, and think of them as two dance partners… moving along, but in order to get a choreographic dance, they have to talk to each other. They do that through the ocean-atmosphere interface, which is wave motion, spray, all the things that help them communicate. These two create different dances… an El Nino dance, or a hurricane dance, for example. In reality what they do together is transport heat, carbon and water, which are the major global cycles in our planetary system.”

Since the onset of industrialization, we humans have been introducing some different steps to the dance, it seems:

“When you take it to the climate scale, we talk a lot about the temperature of the atmosphere, increases associated with the infusion of carbon, that is human produced. The thing is that the extra carbon dioxide that gets released into the atmosphere through our fossil fuels and deforestation is associated with extra heat. Of the carbon dioxide we release into the atmosphere, half will stay in the atmosphere, 25% will go into the ocean, 25% will be taken up by the land. But if you look at the heating or warming, 93% of the extra warming is actually in the ocean. There are only very small amounts in the atmosphere.”

How much heat is stored under that icy ocean?  (Pic: I.Quaile, Greenland)

Centuries of warming pre-programmed

That means a huge amount of heat is actually being stored in our seas:

“And you can understand why, because the atmosphere is a gas, the ocean is a mass of liquid, which covers two thirds of our planet, and it has a huge heat capacity to store that, but that heat doesn’t just stay at the surface. So (..) when you only talk about heat and temperatures at the surface, you’re ignoring what’s happening below the surface in the ocean, and once the ocean gets heated it’s not going to stay there, because there is this fluid motion. So we’re getting to see greater and greater temperature increases at greater and greater depths. And once that heat gets into the ocean, it can stay there for centuries. Whereas in the upper ocean, it might stay 40 or 50 years, when you get into the deeper parts, because of the density and capacity, it stays there for a long time.”

So, she explained, the carbon dioxide we’ve put into the atmosphere already – and the heating associated with that – means that “we’re already pre-destined for a certain amount of global temperature increase. Many people say we have already pre-destined at least one and a half degree, some will say almost two degrees.”

Now if that is not a sobering thought.

And on top of that comes the acidification of the oceans caused by the extra carbon dioxide, which is playing havoc with coral reef systems and shell-based ocean life forms.

“This is really critical, because it attacks a lot of the base of the food chain for a lot of these eco-systems”.

Scientists measure ocean acidification off the coast of Spitsbergen. (Pic: I.Quaile)

“What’s in the Arctic is not staying in the Arctic”

Susan Avery’s work has included research on the Arctic and Antarctic, so of course I took the opportunity to ask how she sees all this affecting the polar regions.

She explained how the rapid increase in ice melt in the Arctic – both sea-ice and land ice – caused by atmospheric warming above and warmer ocean waters below, is of great concern for two reasons. The more obvious one is the contribution of land ice melt to sea-level-rise. The other, she explained, is that the melting of the land-based ice results in “a freshening of certain parts of the ocean, so particularly the sub-polar north Atlantic, so you have a potential for interfacing with our normal thermohaline circulation systems which could dramatically change that.” The changes in salinity currently being observed, are a “signal that the water cycle is becoming more vigorous”. This, of course, has major implications for ocean circulation and, in turn, the climate, not just in the region where the ice has been melting:

“What’s in the Arctic is not staying in the Arctic. What’s in the Antarctic is not staying in the Antarctic. I would say the polar regions are regions where we don’t have a lot of time before we see major, massive changes”.

What I find particularly worrying is that Susan Avery confirmed there is still so much we do not know about what is happening in the polar regions and in the ocean in general.

“We really need to get our observations and science and models working together”, she told me. “The new knowledge we have created on processes in the Arctic has to be incorporated into climate system models”.

Satellite data ( KSAT site in in Tromso) helps, but cannot penetrate deep ocean, Avery says.  (Pic. I Quaile)

Paris and the poles

So, given that temperature rise of 1,5 to two degrees Celsius could already be a “given”, and the Arctic is being affected much faster and more strongly than the planet on average, is there any real hope that we can hold up these developments and halt the melting of ice in the Arctic? This was clearly a very difficult question for my guest. She told me she had been very relieved that the Paris Climate Agreement was signed and was sure humankind could still “make things better”. But when I asked whether we will really be able to reverse what is happening in the Arctic or halt climate change in the Antarctic, this was what she replied:

“I don’t have an answer, to be honest. I think we’re still learning a lot about the Arctic and its interface with lower latitudes, how that water basically changes circulation systems, and on what scale. But I think what’s really critically needed right now to get a better sense of the evolution of the Arctic, and of sea level rise, is a real concerted observing network. We know so little, about the Arctic, the life forms underneath the ice. We have the technology. What I really see now is a confluence of new technologies, new analytical approaches, new ways to do ocean science, and all it takes is money to really get those robots there, get the genomic studies that you need, the analysis. We are at the stage where we can do so much, to further our understanding, and I would really put a lot into the Arctic right now, if I had the money to do so.”

Me too, Susan.

Ice: the final frontier?

Investigating the undersea secrets of the Arctic night from the research vessel Helmer Hanssen (Pic: I.Quaile)

This brings us back to a key problem I have worried about ever since I started to work on how climate change is affecting the Arctic. That change is speeding up so fast, it is virtually impossible for our research to keep pace. As Susan Avery put it:

“The Arctic will be a major economic zone, we’ve already seen the North-West Passage through the Arctic waters, we’re going to see migration of certain fisheries around the world – and we don’t even know completely what kind of biological life we have below that ice. We have the ability to get underneath the ice now. I call these the frontiers, of the ocean, and that includes looking under ice.”

I am reminded of my trip on board the Helmer Hanssen last year, accompanying a research mission to find out what happens under that ice and down in the deep ocean during the cold, dark season.

(Listen to the audio feature here). There is still so much we do not know about life in the ocean – and it might disappear before we even knew it was there.

Melting ice off Greenland (Pic: I.Quaile)

My attention was caught this week by a study that ascertained that thermal expansion accounts for a much greater share of sea level rise than previously thought. In fact, quite a few journalists got the message wrong. They thought the researchers had found that climate change was causing sea level rise twice as high as previously thought, which would have been quite a sensation. In fact, what the scientists actually found was that the amount of sea level rise that comes from the oceans warming and expanding has been underestimated and is probably about twice as much as previously calculated. There is a clear difference, which does not make the research – using the latest available satellite data – any less interesting.

Since two of the authors of the study are based here in Bonn, I was able to drop in on them and get them to explain their findings and the implications for our Living Planet programme. That will be broadcast in the near future. I also talked to Professor Anders Levermann from the Potsdam Institute for Climate Impact research on the phone, to get the research findings into context.

While physicists understand the workings of thermal expansion in the oceans in general, Levermann told me there is still a lot to learn about how the heat from excess warming is transported in the ocean, which is of key importance to understanding sea level rise, amongst other things. He says the new research will help make models of future sea level rise more accurate.

Roelof Riebroek and Jürgen Kusche, University of Bonn (Pic: I.Quaile)

The Bonn researchers explained to me how satellite technology has made huge improvements in the collection of data, especially relating to the very deep areas of the ocean, which are very difficult to reach with conventional measuring gauges. Professor Kusche told me he would like to see the results of the study, published in the Proceedings of the National Academy of Sciences, being used by governments and coastal planners, as sea level rise will affect a large number of people living in coastal areas in the not-too-distant future. Warming seas are also linked to the occurence of storms, making the findings doubly relevant to those involved in protecting coastal areas.

From an Iceblogger point of view, I was keen to know whether the knowledge about the amount of sea level rise ascribed to  thermal expansion had any implications for the role played by melting ice in raising sea level. If thermal expansion is accounting for a higher share of the sea level rise, is melting ice from Greenland and Antarctica accounting for less? I put that question first to Professor Kusche.

“We think that less of the sea level rise is coming from melting ice and glaciers, that’s actually true,” he answered. He said he and his colleagues had done a very thorough re-analysis of all the measurements available over the last 12 or 13 years, “and we are pretty sure that our numbers are correct”.

Rietbroek came in that that point: “Less, but not that much less. If you look at pubished literature and estimates of glacier melting, and try to add those up, you won’t be that far away from what we get. So the melting of glaciers is not that different from what’s been found previously”, he added.

Climate change melts ice – from above and below(Pic:I.Quaile)

I put the same question to Professor Levermann from PIK, who runs an ice sheet model for the Antarctic and was lead author of the IPCC chapter on sea level change. He explained to me that the various contributions to sea level rise are measured and modelled separately by different teams of experts in particular fields. The models all have a wide range of possible variation. He told me there is still some uncertainty in the distribution of the “sea level rise budget” between thermal expansion, ice sheet melt, mountain glacier melt and groundwater mining. While the latest findings on thermal expansion could potentially shift the relative contributions and are important for improving models to project future sea level rise more accurately, they do not change the validity of predictions relating to the amount of ice going into the ocean.

Ultimately, Levermann says, one of the IPCC statements with the highest certainty is that sea level will continue to rise for centuries to come. He was one of the authors of yet another study  published in Nature Climate Change this past week, led by Peter Clark from the Oregon State University. It affirms that our greenhouse gas emissions today produce climate change commitments for many centuries to millenia. Unless the Paris climate agreement is put into practice asap and we reach zero or negative emissions, up to 20 percent of the world’s population will find itself living in areas that may have to be abandoned.

We are, indeed, living in the Anthropocene. Recently, I interviewed a scientist who found that we have already postponed the next ice age by 50,000 years through our fossil fuel emissions. The latest sea level study indicates that the next few decades offer a brief window of opportunity to avoid increased ice loss from Antarctica and “large-scale and potentially catastrophic climate change that will extend longer than the entire history of human civilization thus far”.

Heavy snow – not all fun (Pic: I.Quaile)

If you are sitting somewhere on the East Coast of the USA, struggling to cope with 30 inches of snow, you might be forgiven for reacting with relief to a report released by the Potsdam Institute for Climate Impact Research (PIK) indicating human-made climate change is suppressing the next ice age. With a wink in your eye, you might be very grateful that these extreme conditions are only going to last for a few days and not become the everyday normality of a new ice age.

There are those (but increasingly few of them) who might even thank the fossil fuels industries for averting a scenario like “The Day after Tomorrow” and ensuring that the relatively comfortable interglacial in which we live is likely to continue for the next 100,000 years. That is the conclusion of the study published in the scientific journal Nature.

The problem is that postponing an ice-age illustrates that human interference with natural climate cycles over a relatively short time has the potential to change the world for a hundred thousand years to come, with all the problems that come with it. And given that the increase in extreme weather events like the US snowstorm is highly probably related to anthropogenic climate change, perhaps an ice age in 50,000 years would be the lesser evil.

Burn fossil fuels, suppress the ice age

Using complex models to try to find out which factors influenced the last eight glacial cycles in earth history and what is likely to lie ahead of us, the scientists found that as well as astronomical factors like the earth’s position in relation to the sun in different stages of its orbit, the CO2 concentration in the atmosphere is a key factor.

I talked to physicist and earth systems modeler Andrey Ganopolski, lead author of the study to find out more about the research and the background.

Listen to the interview.

Ganopolski is a physicist and climate modeler. (Pic: PIK)

According to Milankovich’s theory, a new ice age should occur when the earth is far away from the sun and summer is colder than usual in the northern hemisphere, at high latitudes in Canada and northern Europe. These are the areas where big ice sheets can grow. At the moment, Ganopolski explained, we have a situation where our summer occurs when the earth is far from the sun. So in principle, we have the conditions when a new ice age can potentially start. He and his colleagues wanted to understand why we are not living in an ice age when astronomically, the conditions are just right to move towards a new ice age.

Meddling with the planet

They come to the conclusion that naturally, without any anthropogenic influence, we would expect the new ice age to start around 50,000 years from now. That would mean that this interglacial, the Holocene, in which we live now, would already be unusually long. In the past, an interglacial lasted only 10 or 20,000 years, but this one is expected to last for 60,000 years.

Greenhouse gas emissions are transforming all areas of the planet. (Pic: I.Quaile)

But our emissions of greenhouse gases are postponing this even further. Relatively large anthropogenic greenhouse gas emissions – say two to three times what we already emitted – would, according to the scientists’ model, additionally postpone the next ice age, so that it would only start 100, 000 years from now, so we would completely skip one glacial cycle, which never happened in the last three million years.

Humankind as a geological force

Now regardless of whether you are a fan of ice and snow or one of those who say they can happily live without any more ice ages, the study’s findings illustrate just how long anthropogenic influence on climate will continue. Humanity, it seems, has become a geological force that is able to suppress the beginning of the next ice age, according to the PIK experts. Human behavior is changing the natural cycles that have shaped the global environment and human evolution.

Over the last 3 million years, glacial cycles were more or less regular. Most of the evolution of humans occurred during those last three million years. Ganopolski says humans can be seen as a kind of product of glacial cycles, because the conditions were probably right to increase the size of our brain, because we had to be clever to survive in such a variable climate.

Melting ice, north and south? (Photo: I Quaile)

Who cares?

But given that it is easier and pleasanter to live in non ice-age conditions, there is still an understandable tendency to respond to the ice-age-postponement announcement with: “so what?”

Ganopolski argues one reason the study is significant is that it does away with the arguments of some climate skeptics who have argued that warming the atmosphere by burning fossil fuels is not a bad thing, because it could avert an “imminent” ice age (a theory first made popular around thirty years ago, he says). Since the research indicates there is none on the horizon for more than 50,000 years anyway, this is nonsense, says Ganopolski.

But the main reason the research findings deserve attention, he says, is that they show we can affect the climate for up to a hundred thousand years. He believes a lot of people think if we stop using fossil fuels tomorrow or the day after, everything will be fine. In fact, anthropogenic carbon dioxide will stay in the atmosphere for an extremely long time. “That means we are affecting earth’s future on a geological time scale”, he says.

Whether the next ice age comes in 50,000 or 100,000 years may seem irrelevant to a lot of people, faced with the concerns of life today. But the effects of our warming the globe are already being felt and will have considerable implications well before that, Ganopolski reminds us. He says the new study just shows how massive our interference with the earth’s systems is, and backs up the need to take action now to cut greenhouse gas emissions.

Rising CO2 emissions are influencing glacial patterns (Measuring station on Svalbard, Pic. I. Quaile)

Greenland and Antarctic in the Anthropocene

He mentions the research also deals with Greenland and Antarctica:

“What we show is that even with the CO2 concentration we have already, we can expect that a substantial fraction of these ice sheets will melt. So obviously, in this respect, any further increase of CO2 will have even more negative effects”.

Sea level rise, ocean acidification, changing food supplies, floods, droughts…and, yes, even more of those extreme blizzards, fuelled, paradoxically, by warming seas…maybe there is more to this delaying the ice age business than first seemed.

So are we living in the “Anthropocene”, i.e. an era in which not nature but humankind is determining the shape of the world we live in now and for centuries to come? Ganopolski and his colleagues say yes. He stresses what we are doing to the climate and the speed at which it is happening represent unprecedented, substantial deviation from the natural course of things.

“So if you continue to emit a substantial amount of carbon dioxide, the Anthropocene will last for hundreds of thousands of years, before systems return to anything like “normal” conditions”, he says.

Another  study published in Nature  today provides further evidence that human intervention is responsible for the annual heat records that have been in the news so often recently they run the risk of losing their news value. Ganopolski’s PIK colleague Stefan Rahmstorf, one of the authors, says the heat records, with 13 of the last 15 years the warmest since records began, can no longer be explained by natural climate variation. But they can be explained by human-induced climate change.

But is there any point in making potentially uncomfortable changes to the way we live today if we have already changed the atmosphere so massively, for such a long time to come? Ganopolski stresses the extent and speed of the changes and impacts are no grounds for resignation:

“There is no justification for making the climate even warmer than it is. It is a matter of how much CO2 we will emit into the atmosphere. Basically, it will affect all generations, and if we care about them, we should stop using fossil fuel as soon as possible.”

Sounds sensible to me.