What you will find on this page – definitions and explanations of “carbon” terms and what they mean for climate change response: temperature and CO2 emissions in context (animated video); Global emissions flat 3rd year in row; 43 greenhouse gases driving global warming; carbon budget 2016 (infograph): follow CO2 through atmosphere (video); the rich outsourcing emissions to the poor; carbon dioxide levels continue reaching new highs; understanding the carbon cycles – slow & fast; atmospheric CO2 misconceptions; carbon budget; global carbon emission footprint (interactive graph); carbon map – who’s responsible; 800,000 history of carbon dioxide (video); CO2 keeps rising emissions flat – why?; are we permanently above 400ppm?; CO2 equivalent what is it; GHG emission data; CO2 & CO2 – e measurement analysis; emission reduction not all what it seems; carbon concentration overshoot; climate system lag time; what is carbon neutral/offsetting (video, report & recommendations); carbon capture and storage (video); carbon pricing; how carbon credits work – Narmboolville; also refer to pages “the science“, “Two degree “safe limit” and “mitigation battle” as the issues are closely related
What does “carbon ……” mean?
13 June 2017, The Conversation, There are those who say the climate has always changed, and that carbon dioxide levels have always fluctuated. That’s true. But it’s also true that since the industrial revolution, CO₂ levels in the atmosphere have climbed to levels that are unprecedented over hundreds of millennia. So here’s a short video we made, to put recent climate change and carbon dioxide emissions into the context of the past 800,000 years.
14 June 2017, Carbon Brief, The world added a record amount of energy from renewable sources in 2016 and global coal use fell again, according to the 2017 BP Statistical Review of World Energy, published earlier this week. This helped to keep global CO2 emissions flat for the third year in a row, even as energy demand rose. The record 53 million tonnes of oil equivalent (Mtoe) added by non-hydro renewables met a third of the increase in global energy demand. Global coal use fell by 53Mtoe (1.4%) and is now 4% below the 2014 peak. Meanwhile, coal production fell by a record 231Mtoe (5.9%), as massive output declines continued in the US and China worked to reduce overcapacity and combat air pollution. Carbon Brief runs through BP’s new data and highlights some of the key changes in global energy production and use last year. Record renewables Non-hydro renewable energy sources, such as wind and solar, had a record year in 2016, adding 53Mtoe. They were the fastest-growing source of energy, up 14%, in line with average growth of 16% per year over the decade to 2015. Together with nuclear and hydro, low carbon energy supplied more than half of the net increase in global energy demand between 2015 and 2016. Read More here CLICK ON IMAGE TO ACCESS VIDEO
June 2017, Australia Institute National Energy Emissions Audit. Providing a comprehensive, up-to-date
indication of key greenhouse gas and energy trends in Australia. Access Report here
The most comprehensive collection of atmospheric greenhouse gas measurements, published today, confirms the relentless rise in some of the most important greenhouse gases. The data show that today’s aggregate warming effect of carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O) is higher than at any time over the past 800,000 years, according to ice core records. Building on half a century of atmospheric measurements by the international research community, we compiled and analysed the data as part of a group of international scientists, led by Malte Meinshausen from the University of Melbourne in collaboration with CSIRO. Together, the data provide the most compelling evidence of the unprecedented perturbation of Earth’s atmosphere. They clearly show that the growth of greenhouse gases began with the onset of the industrial era around 1750, took a sharp turn upwards in the 1950s, and still continues today. Research has demonstrated that this observed growth in greenhouse gases is caused by human activities, leading to warming of the climate – and in fact more than the observed warming, because part of the effect is currently masked by atmospheric pollution (aerosols). The new collection of records comes from measurements of current and archived air samples, air trapped in bubbles in ice cores, and firn (compacted snow). The data cover the past 2,000 years without gaps, and are the result of a compilation of measurements analysed by dozens of laboratories around the world, including CSIRO, the Bureau of Meteorology’s Cape Grim Station, NOAA, AGAGE and the Scripps Institution of Oceanography, among others. Read More here
NASA, the US space agency, has released an “eye-popping” three-dimensional animation showing carbon dioxide emissions moving through the Earth’s atmosphere over the course of a year. It says the 3-D visualisation is “one of the most realistic views yet” of the “complex patterns in which carbon dioxide in the atmosphere increases, decreases and moves around the globe”. The data used to produce the visualisation was collected by NASA’s Orbiting Carbon Observatory-2 (OCO-2) satellite from September 2014 to September 2015. The data was then modelled and visualised by the Global Modeling and Assimilation Office at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.
Source: To view more NASA carbon dioxide videos go here
18 April 2017, VOX, For years now, carbon dioxide emissions in the United States and Europe have been steadily falling — an encouraging sign of progress in the fight against global warming. But on the flip side, emissions in developing countries like China and India have been growing at a very rapid clip. So one natural question to ask is just how closely these two things are related. That is, are rich countries just “outsourcing” their climate pollution to poorer countries, by shifting their factories overseas? The answer is basically yes. But as you might guess, there are all sorts of interesting twists and nuances that make this more complicated than it seems. The Global Carbon Project, a major effort to measure CO2 emissions worldwide, tries to measure this outsourcing effect by estimating, for each country, “production emissions” (that is, the CO2 produced within a country’s borders) and “consumption emissions” (the CO2 emitted around the world in the course of manufacturing goods for that country). As you can see on the graph below, wealthy OECD nations “consume” a fair bit more CO2 than they actually emit within their own borders. They have indeed outsourced a big chunk of their climate pollution to the developing world. Read More here
4 April 2017, Climate Central, Current carbon dioxide levels are unprecedented in human history and are on track to climb to even more ominous heights in just a few decades. If carbon emissions continue on their current trajectory, new findings show that by mid-century, the atmosphere could reach a state unseen in 50 million years. Back then, temperatures were up to 18°F (10°C) warmer, ice was almost nowhere to be seen and oceans were dramatically higher than they are now. The implications of the research, published on Tuesday in Nature Communications, are some of the starkest reminders yet that humanity faces a major choice to curtail carbon pollution or risk pushing the climate outside the bounds that have allowed civilization to thrive. Atmospheric levels of carbon dioxide have varied for millennia, fluctuating largely on natural cycles. Humans have added dramatically more carbon dioxide to the atmosphere since the Industrial Revolution, though, raising carbon dioxide from 280 parts per million to nearly 410 parts per million. That has turned the thermostat up about 1.8°F (1°C) and caused a host of other impacts. Read More here
NASA Earth Observatory: This diagram of the fast carbon cycle shows the movement of carbon between land, atmosphere, and oceans. Yellow numbers are natural fluxes, and red are human contributions in gigatons of carbon per year. White numbers indicate stored carbon. (Diagram adapted from U.S. DOE, Biological and Environmental Research Information System.)
Carbon flows between each reservoir in an exchange called the carbon cycle, which has slow and fast components. Any change in the cycle that shifts carbon out of one reservoir puts more carbon in the other reservoirs. Changes that put carbon gases into the atmosphere result in warmer temperatures on Earth. There are both slow and fast carbon cycles. Without human interference, the carbon in fossil fuels would leak slowly into the atmosphere through volcanic activity over millions of years in the slow carbon cycle. By burning coal, oil, and natural gas, we accelerate the process, releasing vast amounts of carbon (carbon that took millions of years to accumulate) into the atmosphere every year. By doing so, we move the carbon from the slow cycle to the fast cycle. In 2009, humans released about 8.4 billion tons of carbon into the atmosphere by burning fossil fuel.
16 December 2010, Yale Climate Connections: Understanding the carbon cycle is a key part of understanding the broader climate change issue. But a number of misconceptions floating around the blogosphere confuse basic concepts to argue that climate change is irrelevant because of the short residence time of carbon molecules in the atmosphere and the large overall carbon stock in the environment.
It turns out that while much of the “pulse” of extra CO2 accumulating in the atmosphere would be absorbed over the next century if emissions miraculously were to end today, about 20 percent of that CO2 would remain for at least tens of thousands of years. The complex global carbon cycle process involves carbon absorption and release by the atmosphere, oceans, soils, and organic matter, and also emissions from anthropogenic fossil fuel combustion and land-use changes. The figure below shows the best estimate of annual carbon fluxes from main sources and sinks. (Figure is from Oak Ridge National Laboratories (Units in gigatons of carbon).
At first glance, it may seem that the narrow black arrows representing anthropogenic sources are relatively insignificant, making up only a few percent of the total carbon released to the atmosphere in any given year. To understand why anthropogenic emissions are of concern, it is important to think of the carbon cycle as a balance of sorts; every year around 230 gigatons of carbon dioxide are released to the atmosphere, and around 230 gigatons of carbon dioxide are absorbed by the world’s oceans and biosphere. This balance forms an equilibrium of sorts, with the level of atmospheric carbon dioxide remaining largely unchanged over time. However, anthropogenic emissions throw this process out of kilter, adding a new source of emissions unmatched by additional sinks.
Read More here
At the 21st Conference of the Parties to the Climate Change Convention, in Paris in December 2015, the international community agreed to “pursue efforts” to limit temperature rise to no more than 1.50 C above the pre-industrial average, in order to prevent the dangerous effects of climate change.The challenge of this task is quite extraordinary. The IPCC has identified a range of ‘carbon budgets’ which define the maximum amount of carbon dioxide that can be emitted for any given likelihood of remaining below a given temperature rise.
This figure shows the number of years it would take to use up those budgets, if the level of annual emissions remained as they are today. The available carbon budget – if we want a two thirds chance of meeting the 1.5°C target – is just 240 Gt CO2 . At the current rate of annual emissions this would be used up in just six years. After that point, there would have to be ‘net zero’ carbon emissions for the rest of the century. Source: Limits Revisited: A Review of the Limits to Growth Debate (April 2016)
Go here for more on carbon budget background or click on image for full report
22 September 2014, Inside Climate News, Climate Primer: Explaining the Global Carbon Budget and Why It Matters: Once the amount of CO2 in the atmosphere tops 3.2 trillion metric tons, chances dim to avoid climate disaster, according to new calculations. For as long as scientists and policymakers have been grappling with climate change, they’ve been up against two critical questions: How much extra carbon has mankind sent into the atmosphere? And how much more can be added before global warming becomes disastrous? Climate researchers have spent decades tracking and quantifying the complex flows of carbon into and out of the atmosphere, but those questions couldn’t be answered convincingly until 2009. That’s when a group of European scientists published a groundbreaking and highly credible global carbon budget that filled the information void. Using a comprehensive climate model, the scientists determined the maximum amount of greenhouse gases mankind could send into the atmosphere without triggering catastrophe—and then found that more than a quarter of that budget had been spent by 2006.
What is a carbon budget?
It’s an estimate of the maximum amount of greenhouse gases that can be released into the atmosphere over time and still keep warming limited to a specified level. In many cases, carbon budgets are pegged to holding the average global temperature increase below 2 degrees C compared with the beginning of the Industrial Age in the 18th Century. Accelerated burning of fossil fuels over the past 2½ centuries has poured billions of tons of carbon into the atmosphere, causing global surface air temperatures to warm already by an average of 0.8 degrees C. Scientists have estimated that 2-degree warming would trigger a host of more drastic changes in the climate, including effects that would be irreversible. Most carbon budgets focus solely on emissions of carbon dioxide, or CO2. That’s because it’s by far the largest contributor to global warming. Others, such as the carbon budget cited by the United Nations-led Intergovernmental Panel on Climate Change, include estimates for other greenhouse gases such as methane. For simplicity and consistency, this discussion refers only to carbon budgets that track CO2 emissions. In 1992, nations participating in climate treaty talks through the UN Framework Convention on Climate Change agreed to hold human-caused global warming below a level that would cause “dangerous” climate change. That led to the 2-degree benchmark and an agreement to consider lowering that goal to 1.5 degrees. Researchers from Germany, the U.K. and Switzerland, led by scientist Malte Meinshausen of the Potsdam Institute for Climate Impact Research, are widely credited with being the first—in 2009—to combine all of those elements into a rigorous, comprehensive scientific model to calculate a 2-degree carbon budget. Since then, carbon budgets have become a staple of climate change analysis.
How big is the budget?
The answer depends on several variables and it’s constantly being adjusted. The September 2014 carbon budget from the Global Carbon Project, a consortium of university and government scientists and researchers, put the latest 2-degree limit at 3.2 trillion metric tons of CO2. According to the budget, if emissions stay below that mark, there is roughly a 66 percent chance that the world would not trigger the most destructive forces of climate change.
Where do we stand now?
From 1870 to 2013, human activity added about 2 trillion metric tons of CO2 to the atmosphere, according to the Global Carbon Project. That means almost two thirds of the budget already has been used. The emissions came from burning fossil fuels for heat, electricity, factories, ships, planes, trains and automobiles, as well as from cement production, agriculture and land use changes. Because fossil fuel emissions have accelerated over time, humanity is on track to use up the remainder of the budget in the next three decades—or perhaps as early as 2031. Read More here Access Global Carbon Project here
There are many in the scientific circles of climate change that are expressing the concern that there is NO carbon budget left. For the latest report concerning this access “Recount do the math again” by David Spratt, from Break Through site. Also access Two degree “safe limit” on The Science page of this site.
May 2016, An interactive guide from British Gas about the world’s carbon emissions. Explore the Carbon Emissions of different countries and how nations across the globe are working to reduce their CO2 emissions. Access guide here
Source: NOAA Global Monitoring Division
10 March 2016, Washington Post: Atmospheric carbon dioxide concentrations have spiked more in the period from February 2015 to February 2016 than in any other comparable period dating back to 1959, according to a scientist with the National Oceanic and Atmospheric Administration’s Earth System Research Laboratory. The change in average concentrations from February of last year to February of this year was 3.76 parts per million at the storied Mauna Loa Observatory in Hawaii, leaving the concentration at 404.02 parts per million for February, based on preliminary data. Pieter Tans, lead scientist of NOAA’s Global Greenhouse Gas Reference Network, confirmed that the increase, reported previously by New Scientist, represented a record year-over-year growth for Mauna Loa. He also said that in addition to the stark rise in carbon dioxide levels over the past year, researchers have now observed four straight years of increases of more than 2 parts per million in the atmosphere. “We’ve never seen that,” Tans said. “That’s unprecedented.” Read More here
25 February 2016, Climate News Network, Fossil fuel use will have to fall twice as fast as predicted if global warming is to be kept within the 2°C limit agreed internationally as being the point of no return, researchers say.
Climate scientists have bad news for governments, energy companies, motorists, passengers and citizens everywhere in the world: to contain global warming to the limits agreed by 195 nations in Paris last December, they will have to cut fossil fuel combustion at an even faster rate than anybody had predicted. Joeri Rogelj, research scholar at the International Institute for Applied Systems Analysis in Austria, and European and Canadian colleagues propose in Nature Climate Change that all previous estimates of the quantities of carbon dioxide that can be released into the atmosphere before the thermometer rises to potentially catastrophic levels are too generous. Instead of a range of permissible emissions estimates that ranged up to 2,390 billion tons from 2015 onwards, the very most humans could release would be 1,240 billion tons. Available levels In effect, that halves the levels of diesel and petrol available for petrol tanks, coal for power stations, and natural gas for central heating and cooking available to humankind before the global average temperature – already 1°C higher than it was at the start of the Industrial Revolution – reaches the notional 2°C mark long agreed internationally as being the point of no return for the planet. In fact, the UN Framework Convention on Climate Change summit in Paris agreed a target “well below” 2°C, in recognition of ominous projections − one of which was that, at such planetary temperatures, sea levels would rise high enough to submerge several small island states. The Nature Climate Change paper is a restatement of a problem that has been clear for decades. Carbon dioxide proportions in the atmosphere are linked to planetary surface temperatures and, as they rise, so does average temperature. For most of human history, these proportions oscillated around 280 parts per million. Read More here
Avoiding catastrophic warming requires stabilizing CO2 concentrations (or levels) in the atmosphere, not annual emissions. Studies find that many, if not most, people are confused about this, including highly informed people, mistakenly believing that if we stop increasing emissions, then global warming will stop. In fact, very deep reductions in greenhouse gas emissions are needed to stop global warming.
One study by MIT grad students found that “most subjects believe atmospheric GHG concentrations can be stabilized while emissions into the atmosphere continuously exceed the removal of GHGs from it.” The author, Dr. John Sterman from MIT’s Sloan School of Management, notes that these beliefs “support wait-and-see policies but violate conservation of matter” and are “analogous to arguing a bathtub filled faster than it drains will never overflow.”
While atmospheric concentrations (the total stock of CO2 already in the air) might be thought of as the water level in the bathtub, emissions (the yearly new flow into the air) are the rate of water flowing into a bathtub from the faucet. There is also a bathtub drain, which is analogous to the so-called carbon “sinks” such as the oceans and the soils. The water level won’t drop until the flow through the faucet is less than the flow through the drain. Similarly, carbon dioxide levels won’t stabilize until human-caused emissions are so low that the carbon sinks can essentially absorb them all. Under many scenarios, that requires more than an 80 percent drop in CO2 emissions. And if the goal is stabilization of temperature near or below the 2°C (3.6 °F) threshold for dangerous climate change that scientists and governments have identified, then CO2 emissions need to approach zero by 2100. So the first key point is that CO2 levels will continue rising if we merely keep annual CO2 emissions flat. In fact, they will keep rising at a faster and faster rate because the land and ocean carbon sinks are weakening (see below).
The Temporary Impact Of El Niño
NOAA reported two weeks ago that the CO2 concentrations “measured at NOAA’s Mauna Loa Observatory in Hawaii jumped by 3.05 parts per million during 2015, the largest year-to-year increase in 56 years of research.” That is a big jump compared to the average annual rise at Mauna Loa from 2005 to 2014 of 2.11 ppm per year. But the second-highest single-year growth rate for CO2 levels was back in 1998, which saw a jump of 2.93 ppm (whereas the average annual rise from 1995 to 2004 was 1.87 ppm per year). You may notice a pattern here — big jumps during big El Niño years. “El Niño years tend to be bad years for plant growth, due to things like widespread drought or other extreme weather,” Stefan Rahmstorf, co-chair of Earth System Analysis at the Potsdam Institute for Climate Impact Research, explained in an email. “So the biosphere loses some carbon. You see that happening in 1998 as well. Below is a diagram from the AR5, you see from the squiggly line how variable the land sink is, it dominates interannual variability in the carbon budget.”
A crucial point is that, based on actual observations and measurements, the world’s top carbon cycle experts have determined that the land and oceans are becoming steadily less effective at removing excess CO2 from the atmosphere, as I reported last year. This makes it more urgent for us to start cutting carbon pollution ASAP, since it will become progressively harder and harder for us to do so effectively in the coming decades. In particular, the defrosting permafrost and the resultant release of CO2 and methane turns part of the land sink into a source of airborne greenhouse gases. Similarly, as global warming increases forest and peatland fires — burning trees and vegetation — that also turns one part of the land carbon sink into a source of atmospheric CO2. So does ever-worsening droughts that scientists are observing in the United States southwest and other parts of the world. We are destroying nature’s ability to help us stave off catastrophic climate change. “Clearly nature is helping us” deal with atmospheric CO2 right now much more than it will be decades to come, as Dr. Josep (Pep) Canadell, executive director of the Global Carbon Project, told me last year. Ultimately this is one more reason why delaying action to cut carbon pollution is a costly and dangerous mistake. Source: Think Progress
20 May 2016, Renew Economy, Just three years ago this month, the carbon dioxide monitoring station atop Hawaii’s Mauna Loa reached a significant milestone: the first measurement of CO2 concentrations that exceeded the benchmark of 400 parts per million (ppm). Now, they may never again dip below it. As CO2 levels once again approach their annual apex, they have reached astonishing heights. Concentrations in recent weeks have edged close to 410 ppm, thanks in part to a push from an exceptionally strong El Niño.
But it is the emissions from human activities that are by far the main driver of the inexorable climb of CO2 concentrations in the atmosphere. That trend, in turn, is driving the steady rise of global temperatures, which have set record after record in recent months. Those CO2 levels will soon begin to drop toward their annual minimum as spring triggers the collective inhale of trees and other plant life. But because of the remarkable heights reached this year, the fall minimum, unlike recent years, may not dip below the 400-ppm mark at Mauna Loa. “I think we’re essentially over for good,” Ralph Keeling, the director of the Mauna Loa CO2 program at the Scripps Institution of Oceanography, said. And before too long, that will be the case the world over. Steady Rise Atmospheric carbon dioxide levels are monitored at stations around the world, providing records of the mark humans are leaving on the planet. Keeling’s father, Charles Keeling, began the recordings at Mauna Loa in 1958, revealing not only the annual wiggles created by the seasonal growth and death of vegetation, but the steady rise in CO2 from year to year. The resulting graph, dubbed the Keeling Curve in his honor, became an icon of climate science…..Mauna Loa isn’t the only spot poised to move permanently above 400 ppm, though. The Cape Grim station in remote northwestern Tasmania saw its first measurements above 400 ppm on May 10. Now that it has reached that level, it will not dip below again, the scientists who maintain the site told the Sydney Morning Herald. This is particularly significant because Cape Grim had yet to reach that mark, in part because the Southern Hemisphere has a less pronounced seasonal cycle than the Northern Hemisphere because it has more landmass and plant life. The majority of carbon dioxide emissions also come from the Northern Hemisphere and take about a year to spread across the equator……Keeling suspects that the only places on the globe that may see levels dip below 400 ppm this summer will be at the highest latitudes (which have higher seasonal swings). They could perhaps do so again next summer, but then the planet as a whole will be above 400 ppm for the foreseeable future. And while that benchmark is somewhat symbolic — the excess heat trapped by 400 ppm versus 399 is small — it serves as an important psychological milestone, Keeling said, a way to mark just how much humans have emitted into the atmosphere. And with levels this year already nearing 410 ppm, “you realize how fast this is all going,” he said. Keeling is hopeful, though, that with the signing of the Paris agreement and signs of action to limit emissions by various national governments, the iconic rise of the Keeling Curve will start to plateau. “If Paris is successful, this curve will look very different in a matter of five or 10 years because it will start to change,” he said “And I hope we see that.” To read full report access here For more data go to Climate Central’s “Flirting with the 1.5°C Threshold”
The following is taken from the Climate Change Connection website: Charts and tables in this emissions section of their website convert all greenhouse gas (GHG) emissions into CO2equivalents so they can be compared. Each greenhouse gas (GHG) has a different global warming potential (GWP) and persists for a different length of time in the atmosphere. The three main greenhouse gases (along with water vapour) and their 100-year global warming potential (GWP) compared to carbon dioxide are:
- carbon dioxide (CO2) – 1 x
- methane (CH4) – 25 x more powerful
- nitrous oxide (N2O) – 298 x more powerful
Water vapour is not considered to be a cause of man-made global warming because it does not persist in the atmosphere for more than a few days.
There are other greenhouse gases which have far greater global warming potential (GWP)but are much less prevalent. These are sulphur hexafluoride (SF6), hydrofluorocarbons (HFCs), and perfluorocarbons (PFCs). There are a wide variety of uses for SF6, HFCs, and PFCs but they have been most commonly used as refrigerants and for fire suppression. Many of these compounds also have a depleting effect on ozone in the upper atmosphere.
GLOBAL WARMING POTENTIAL (GWP) TABLE: The following table shows the 100-year global warming potential for greenhouse gases reported by the United Nations Framework Convention on Climate Change (UNFCCC). Click here to download an expanded PDF table: GHG Lifetimes and GWPs (144 kB)
How to read this table: The column on the right shows how much that chemical would warm the earth over a 100 year period as compared to carbon dioxide. For example, sulphur hexafluoride is used to fill tennis balls. The table shows that a release on1 kg of this gas is equivalent to 22,800 kg or 22.8 tonnes of CO2. Therefore, releasing ONE KILOGRAM of sulphur hexafluoride is about equivalent to driving 5 cars for a year! (2)
100-year GWP (AR4)
NOTE: The GWP values were changed in 2007. The values in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) in 2007 were refined from the IPCC Second Assessment Report (SAR) values used previously and are still in much of the literature. Refer also to sub page, “Other sources of GHGs”
5 December 2016, The Conversation, Nitrogen pollution: the forgotten element of climate change. While carbon pollution gets all the headlines for its role in climate change, nitrogen pollution is arguably a more challenging problem. Somehow we need to grow more food to feed an expanding population while minimising the problems associated with nitrogen fertiliser use. In Europe alone, the environmental and human health costs of nitrogen pollution are estimated to be €70-320 billion per year. Nitrogen emissions such as ammonia, nitrogen oxide and nitrous oxides contribute to particulate matter and acid rain. These cause respiratory problems and cancers for people and damage to forests and buildings. Nitrogenous gases also play an important role in global climate change. Nitrous oxide is a particularly potent greenhouse gas as it is over 300 times more effective at trapping heat in the atmosphere than carbon dioxide. Nitrogen from fertiliser, effluent from livestock and human sewage boost the growth of algae and cause water pollution. The estimated A$8.2 billion damage bill to the Great Barrier Reef is a reminder that our choices on land have big impacts on land, water and the air downstream. Read More here
4 August 2015, The Conversation, Reducing emissions alone won’t stop climate change: new research. Based on current greenhouse gas emissions, the world is on track for 4C warming by 2100 – well beyond the internationally agreed guardrail of 2C. To keep warming below 2C, we need to either reduce our emissions, or take carbon dioxide out of the atmosphere. Two papers published today investigate our ability to limit global warming and reverse the impacts of climate change. The first, published in Nature Communications, shows that to limit warming below 2C we will have to remove some carbon from the atmosphere, no matter how strongly we reduce emissions. The second, in Nature Climate Change, shows that even if we can remove enough CO2 to keep warming below 2C, it would not restore the oceans to the state they were in before we began altering the atmosphere.
How we’re tracking? Currently, we’re at 400 parts per million – rising from 280 ppm before the industrial revolution. To project future climate change the Intergovernmental Panel on Climate Change (IPCC) uses a range of emissions scenarios called Representative Concentration Pathways (RCPs), based on different economic and energy use assumptions. In the high scenario, RCP8.5, emissions continue to grow from our present rate of 37 billion tonnes of CO2 per year to about 100 billion tonnes of CO2 in 2100, when atmospheric CO2 levels are projected to be 950 ppm. This scenario assumes little mitigation of our carbon emissions.In the low scenario, RCP2.6, emissions rise slowly till the end of this decade to about 40 billion tonnes CO2 each year and then start to decline. Amongst the IPCC emission scenarios, only the RCP 2.6 appears capable of limiting warming to below 2C. With RCP 2.6 at the end of the century atmospheric concentrations is about 420 ppm, and only 20 ppm above the present value. Present emissions are tracking close to the highest scenario (RCP8.5). If we want to keep warming below 2C it requires a substantial reduction in the amount of CO2 released into the atmosphere. Read More here
From Guardian story on China.…. The problem for those fighting to keep global warming within 2C though, is that Chinese demand has expanded so fast that anything short of a dramatic cut in coal use – something no one is even advocating – leaves terrifying amounts of carbon dioxide pumping into the atmosphere. Read More here
19 February 2015, European Environment Agency: Atmospheric greenhouse gas concentrations (CSI 013/CLIM 052) – Assessment: Key policy question: Will the atmospheric concentration of all greenhouse gases remain below 450 ppm CO2-equivalent, giving a 50% probability that the global temperature rise will not exceed 2 degrees Celsius above pre-industrial levels?
- The global average concentrations of various greenhouse gases (GHGs) in the atmosphere continue to increase. The combustion of fossil fuels from human activities and land-use changes are largely responsible for this increase.
- The concentration of all GHGs, including cooling aerosols that are relevant in the context of the 2oC temperature target, reached a value of 435 parts per million (ppm) CO2 equivalents in 2012, an increase of about 3 ppm compared to 2011. As such the concentration continued to close on the threshold of 450 ppm.
- In 2012, the concentration of the six GHGs included in the Kyoto Protocol had reached 449 ppm CO2 equivalent, an increase of 171 ppm (around +62%) compared to pre-industrial levels.
- The concentration of CO2, the most important GHG, reached a level of 393 ppm by 2012, and further increased to 396 ppm in 2013. This is an increase of approximately 118 ppm (around +42%) compared to pre-industrial levels.
Excerpts key assessment
The various greenhouse gases each affect the climate system differently (see rationale). To evaluate the GHG concentration in the atmosphere in relation to temperature change, it is important to consider all greenhouse gases, i.e. the long-living GHGs under the Kyoto Protocol, those under the Montreal Protocol (direct and indirect), as well as ozone, water vapour and aerosols (IPCC, 2013). Considering these gases, the total CO2-equivalent concentration reached a level of 435 ppm CO2 equivalent. in 2012 ; an increase of 3.3 ppm compared to 2011. The increase is slightly higher than the average increase of the annual concentration over the past decade (i.e. is now 2.9 eq.yr-1).
Overall, assuming a concentration threshold of 450 ppm CO2 equivalent could result in a 2oC temperature change (see rationale), this means concentrations can only increase by about a further 15 ppm before this threshold value is exceeded. Assuming the 2000-2012 trend of annual increase of total GHG concentrations will also continue in the coming years, the threshold value may be exceeded in about 5-10 years. The lower band of the uncertainty range has been exceeded already around the millennium change, whereas it may take 20-25 years before the upper uncertainty band is exceeded.
1 June 2015, The Conversation, Climate targets are letting ‘outsourced emissions’ slip through the cracks: Just because a country meets its emissions-reduction targets doesn’t mean it isn’t responsible for increased emissions elsewhere. This isn’t as weird as it sounds. The way national targets are calculated means some countries effectively “outsource” their emissions to other regions. If countries such as the UK don’t include the global emissions impact of their economy they run the risk of believing they are staving off climate change when they are not….Greenhouse gas emissions are usually considered in terms of those emitted within national boundaries; for example by cars and industries. These “territorial emissions” are the basis of national commitments and governments can influence them through taxes or regulations on emissions.
In the UK, the general trend is towards a reduction in these territorial emissions, though it’s tough to say exactly what has happened over the past three years as there is a bit of a lag before annual statistics can be reported.
However, it is instructive to take a wider perspective. Rather than considering the emissions that occur within the UK’s borders, we could think in terms of the emissions that are given off in the process of providing the goods and services enjoyed by its citizens.
Global problems need global targets
This “consumption-based” perspective looks at the whole life cycle of products consumed in a nation and reveals that supporting British lifestyles actually causes the emission of far more greenhouse gases than those emitted in the UK alone. This is because the UK’s imported goods require, on average, more greenhouse gases to be emitted during their production than the goods it exports. While goods and services are imported, emissions are effectively “outsourced” to other nations. This matters because greenhouse gas emissions have a global impact – the UK will be affected just as much by one tonne of carbon emitted in Shanghai as Sheffield. The UK has developed and signed up to a number of strategies and targets to reduce emissions, most notably the Climate Change Act which legally obliges an 80% reduction in greenhouse gas emissions by 2050. However unless emissions are addressed on a global scale, we run the risk of frustrating the purpose of these strategies by shifting the burden from our shores to others. Looking at emissions based on consumption also gives us a clearer picture of which goods and services actually “drive” greenhouse gas pollution. It’s often not the processes directly responsible for the emissions….
OVERSHOOT: The overshoot scenario is an emissions scenario in which atmospheric CO2 concentrations temporarily exceed predefined “dangerous” thresholds before reducing again and stabilizing to the “safe” level that would itself allow global warming to be stabilized at 2°C above pre-industrial levels.
Atmospheric concentrations in baseline scenarios collected for this assessment (scenarios without additional efforts to constrain emissions beyond those of today) all exceed 450 parts per million (ppm) carbon dioxide-equivalent (CO2eq) by 2030 and lie above the RCP 6.0 representative concentration pathway in 2100 (770ppm CO2eq in 2100); the majority lie below the RCP 8.5 concentration pathway in 2100 (1330ppm CO2eq in 2100) (high confidence). The scenario literature does not systematically explore the full range of uncertainty surrounding development pathways and the possible evolution of key drivers such as population, technology, and resources. However, the baseline scenarios do nonetheless strongly suggest that absent explicit efforts at mitigation, cumulative CO2 emissions since 2010 will exceed 700 GtCO2 by 2030, exceed 1500 GtCO2 by 2050, and potentially be well over 4000 GtCO2 by 2100. [Section 6.3.1] Scenarios can be distinguished by the long-term concentration level they reach by 2100; however, the degree to which concentrations exceed (overshoot) this level before 2100 is also important (high confidence). The large majority of scenarios produced in the literature that reach about 450 ppm CO2eq by 2100 are characterized by concentration overshoot facilitated by the deployment of carbon dioxide removal (CDR) technologies at a large scale. Many scenarios have been constructed to reach about 550 ppm CO2eq by 2100 without overshoot. This assessment found that the likelihood of exceeding temperature goals this century increases with peak concentration levels, which are higher in overshoot scenarios. [6.3.2]
Determining limits over time on global emissions involves striking a balance between the benefits associated with smaller and slower climate change and the costs associated with greater and faster mitigation. The appropriate extent of mitigation is defined by the point at which the additional gains from mitigation are similar to the additional costs. In the end, judgment is required on the level of climate change that corresponds to this balancing point. Targeted limits on climate change can be defined at three levels:
- At the highest level they can be defined in terms of impact or global temperature increase.
- At the next level they can be defined in terms of the profile for concentration of greenhouse gases in the atmosphere, which drives temperature increases.
- And at the third level, they can be defined in terms of emissions of greenhouse gases, which drive atmospheric concentrations.
Targets for global mean temperature compress the multiplicity of possible impacts (ranging from glacial melting to increased weather-related calamities) into a single variable. The European Union, for example, has argued that global mean warming should not be allowed to exceed 2°C from pre-industrial levels (Council of the European Union 2007) (NOTE: This has now been accepted as the international target through UNFCCC 2014). Endorsement of a temperature threshold (and therefore of any target derived from it, for example, greenhouse gas concentration) cannot imply indifference to other factors. There may be tipping points associated with particular temperature thresholds, but the thresholds are not known with certainty.
Figure 9.1 Different concentration goals: stabilisation, overshooting and peaking
Global warming increases temperature with a long lag. It might take more than a century after stabilisation of greenhouse gas concentrations for a new equilibrium temperature to be reached (see below). Any goals in terms of temperature need to be translated into goals for the atmospheric concentration of greenhouse gases….
Most attention has focused on stabilisation scenarios, and the UNFCCC goal of the ‘stabilization of greenhouse gas concentrations in the atmosphere’ (Article 2). However, special challenges are introduced by the need to reduce greenhouse gas concentrations to low levels. There is great difficulty in moving directly to that outcome from where the world is now. Whether the ultimate aim is stabilisation or prolonged decline after an initial rise (peaking), there is a good chance that the optimal response to climate change will need to involve a period (of uncertain duration) during which concentrations fall. This assumes that emissions can be brought below the natural level of sequestration. Reducing emissions below this level would probably require the development and deployment of technologies for carbon capture, such as new approaches to biosequestration….The 550 scenario is a stabilisation scenario at which the concentration of greenhouse gases in the atmosphere approaches 550 ppm carbon dioxide equivalent (CO2-e) and stabilises at around that level thereafter. The 450 scenario is an overshoot scenario under which concentrations peak at around 500 ppm CO2-e and then stabilise at around 450 ppm CO2-e. Any lower stabilisation objective, for example at 400 ppm CO2-e, would need to involve a longer period of overshooting. Any concentration profile has an associated emissions trajectory. (An emissions trajectory defines the flow of greenhouse gases that converts, through various physical and chemical processes, into a stock of greenhouse gases in the atmosphere. There are different ways in which goals for emissions can be expressed:
- End-period emissions—This is the most common way of announcing targets (for example, that emissions will be reduced by 50 per cent by 2050). The advantage of this approach is simplicity. The disadvantage is that a target at one point of time says nothing about the rate at which emissions should approach that target level, and so does not constrain cumulative emissions or the concentration profile at that point of time.
- Annual emissions—Since a concentration profile implies annual values for emissions, annual targets for emissions can be articulated. The disadvantages of this approach are complexity and inflexibility. There may be little difference in the environmental impact of two trajectories that end with similar concentrations but that have different annual emissions levels. However, the two paths could have quite different costs.
- Cumulative emissions—This is the budget approach, by which the total emissions determined by a target concentration profile over a number of years are summed up into a single target budget. In this approach, year-to-year variation from the target profile is allowed; what matters is to the total emissions over a number of years. The benefit of the budget approach is its flexibility: it allows intertemporal trade-offs and smoothing. Variations in timing would have to be large to have material environmental impacts.
There is increasing recognition in both science and policy communities that stabilising at low levels of CO2-e (around or below 450 ppm) requires ‘overshooting’ the concentration target (den Elzen et al. 2007; Meinshausen 2006; IPCC 2007a: 827). The climate change impacts of the higher levels of greenhouse gas concentrations reached in an overshoot profile are dependent on the length of time the concentrations stay above the desired target, and how far carbon dioxide overshoots…..Some scientists have also expressed the view that stabilisation at 450 ppm is too high (Hansen et al. 2008). For any such scenarios to be feasible, there would need to be a considerable period of overshooting.
Figure 2.9 shows the different temperature outcomes for a range of cases of overshooting. All three cases show stabilisation at the same level in a similar time frame, but with varying amounts of overshooting. The temperature output demonstrates that while the ‘small overshooting’ case remains under the target temperature, the other cases do not. Hence, due to inertia in the climate system, a large and lengthy overshooting will influence the transient temperature response, while a small, short one will not (den Elzen & van Vuuren 2007).
Figure 2.9 Temperature outcomes of varying levels of overshooting
Source: Concentration and temperature pathways developed using SIMCAP (Meinshausen et al. 2006).
An overshooting profile requires a period in which emissions are below the natural level of sequestration before they are stabilised. Another mitigation option is to follow a ‘peaking profile’. Under a peaking profile, the goal is to cap concentrations at a particular level (the peak) and then to start reducing them indefinitely, without aiming for any explicit stabilisation level. Stabilisation is therefore not conceived as a policy objective for the foreseeable future.
The key benefit of a peaking profile is that it allows concentrations to increase to or above the level associated with a given long-term temperature outcome, but reduces the likelihood of reaching or exceeding that temperature outcome. The higher level of peak concentrations means that current trends in emissions growth do not need to be reversed as quickly to achieve any given temperature goal. This decreases the costs of meeting a given temperature target (den Elzen & van Vuuren 2007).
Following a peaking profile could be a disadvantage if the climate is found to be more sensitive to increases in greenhouse gases than anticipated. Due to the higher concentrations reached under a peaking profile, there is less flexibility to adjust to a lower concentration target at a later point in time, so there is greater risk that a threshold may be crossed.
Designing a mitigation pathway—whether an overshooting or a peaking profile—that requires a decrease in the concentration of greenhouse gases assumes that emissions can be brought below the natural level of sequestration. Figure 2.10 shows the emissions pathways required to achieve a low concentration target following an overshoot. A lower concentration target following an initial overshoot will require negative emissions net of natural sequestration for a longer period.
Figure 2.10 Emissions pathways required to achieve a low concentration target following an overshoot
Source: Based on CASPI (2008).
The costs of reducing emissions below natural sequestration levels would be lower if controls on gross emissions were supported by cost-effective means of removing carbon dioxide from the atmosphere. Bringing emissions below the natural rate of sequestration would require rigorous reduction of emissions from all sources, but might also require extraction of carbon dioxide from the air. Possible methods include:
- increasing absorption and storage in terrestrial ecosystems by reforestation and conservation and carbon-sensitive soil management
- the harvest and burial of terrestrial biomass in locations such as deep ocean sediments where carbon cycling is slow (Metzger et al. 2002)
- capture and storage of carbon dioxide from the air or from biomass used for fuel
- the production of biochar from agricultural and forestry residues and waste (Hansen et al. 2008).
The simplest way to remove carbon dioxide from the air is to use the natural process of photosynthesis in plants and algae. Over the last few centuries, clearing of vegetation by humans is estimated to have led to an increase in carbon dioxide concentration in the atmosphere of 60 ± 30 ppm, with around 20 ppm still remaining in the atmosphere (Hansen et al. 2008). This suggests that there is considerable capacity to increase the level of absorption of carbon dioxide through afforestation activities. The natural sequestration capacities of algae were crucial to the decarbonisation of the atmosphere that created the conditions for human life on earth, and offer promising avenues for research and development. Technologies for capture and storage of carbon from the combustion of fossils fuels currently exist, and the same process could be applied to the burning of biomass.
As yet, there are no large-scale commercial technologies that capture carbon from the air. Some argue, however, that it will be possible to develop air capture technologies at costs and on timescales relevant to climate policy (Keith et al. 2006). Research and development in Australia on the use of algae is of global importance. Captured carbon dioxide could be stored underground or used as an input in biofuel production.
Figure 2.6 shows estimates of the time it takes for different parts of the climate system to respond to a situation where emissions are reduced to equal the rate of natural removal. While greenhouse gas concentrations stabilise in around a hundred years, the temperature and sea-level rise due to thermal expansion of the oceans takes much longer to stabilise. The melting of ice sheets is still increasing the sea level even after a thousand years.
Figure 2.6 Inertia in the climate system
Source: IPCC (2001b: Figure 5.2), reformatted for this publication.
Global Carbon Project
The Global Carbon Project has published the report “Carbon Reductions and Offsets” with a number of recommendations for individuals and institutions who want to participate in this voluntary market.
Recommendations from the report are below:
- Carbon offsets are an important early step
- Choose comprehensive carbon calculators
- Set meaningful limits of responsibility
- Put efficiency first
- Purchase 100 per cent truly new renewable energy
- The voluntary market has developed many credible offset projects
- Offset projects that avoid emissions are best for the long-term
- Carbon sequestration in plants and soils can be vulnerable but has additional benefits
- Tropical reforestation and avoided deforestation are efficient, cost effective land based strategies
- Choose offset projects with stringent standards
- Integrate expenses for offsetting into the cost of activities
- Make a carbon emissions inventory
- Aim for zero net carbon emissions
Source: Global Carbon Project (2008) Carbon reductions and offsets. Coulter L, Canadell J, Dhakal S. Global Carbon Project Report No. 6, ESSP Report No. 5, Canberra.
“Modern-day indulgences, sold to an increasingly carbon-conscious public to absolve their climate sins” – James Hansen
Source: Seuss Wikia (click on graphic for full report)
December 2014, Carbon Trade Watch Report: A TREE FOR A FISH – The (il)logic behind selling biodiversity: Putting a price on ecological systems has been around for several decades, although it was especially heightened during the UN climate negotiations with the introduction of the carbon market, a system which places a monetary value on the carbon-cycle capacity of nature for trade in financial markets.
The carbon market quickly became “the only game in town” that policy-makers and multilateral agencies would discuss and implement regarding climate change policy. Following this logic, the 2010 UN Convention on Biological Diversity (CBD) called for “innovative financial mechanisms’” to deal with biodiversity loss, making biodiversity offsets the standard buzzword within conservation debates. At the same time, people have been resisting projects that claim to compensate for biodiversity destruction and continue to demonstrate how this concept fails to address the drivers of environmental and social damage.
Biodiversity offsets entail projects that cause destruction to biodiversity such as housing, highways or open-pit mines. These destructive projects are allowed to ‘compensate’ for any destruction of habitats or ecosystems, by implementing a project somewhere else which would theoretically protect or (re)create another habitat or ecosystem. To measure the economic ‘value’ of biodiversity, proponents affirm that accounting units are necessary, and hence, different biodiversity types, locations, times, and contexts are turned into apparent ‘equivalent’ numbers. The argument goes that the destruction in one place is ‘equivalent’ to the supposed protection, or re-creation, of another place.
The Economics of Ecosystems and Biodiversity (TEEB) project, led by Pavan Sukhdev, a former economist from the Deutsche Bank, advanced the idea of incorporating an economic ‘value’ of biodiversity into governmental and corporate decision-making. Hosted by the UN Environmental Program and funded by the EU Commission, Germany, the UK, the Netherlands, Norway, Sweden, Japan, and other governmental agencies, TEEB also received support from consultancy firms like Pricewaterhouse Coopers, NGOs like Conservation International, the Institute for European Environmental Policy (IIEP), among others. TEEB claims that the economic value of nature would make ‘nature’ visible to financial markets and consequently, loss of biodiversity would be stopped………
How are offset developers planning to inform the birds of their ‘new home’? The idea of ‘(re)creating’ a ‘new habitat’ elsewhere will almost certainly not be able to compensate for the loss of their ancient habitat. Ecological systems are linked with each other. One cannot ‘preserve nature’ on one part of a country while destroying another part, and claim that this is ‘balancing’ the loss. Whole ecosystems, animals’ behaviours like hunting and migration, plants, waterways, wind cycles, biodiversity, among many other ‘capacities’ of the ‘natural world’ are carefully and harmoniously linked. Offsets enable the colonization – and thus destruction – of the ‘natural world’ in search of economic gains.
…….Reports concluding remarks: Reducing complex and interconnected ecosystems to a single monetary value reduces the ‘natural world’ into tradeable ‘units’ largely for corporate interests. Proponents claim that biodiversity offsetting is “the only option” to get business on board. But we have heard that argument before with the adoption of the carbon market. After over ten years, we can conclude that framing the market and the financialisation of nature as the “only possible option” is a lucrative method for destructive industries and practices to continue expanding their businesses. The idea that “price will solve biodiversity loss or pollution” has colonised peoples’ imaginations and forcibly ignored the many other positions and knowledges. Offsets impose a hegemonic view on how to perceive the world. A world where nature, biodiversity, forests, and rivers, can be separated, and quantified into homogenous units that can be ‘re-created’, ‘replaced’, ‘moved’ or ‘restored’ according to economic and costrelated ‘values’.
In this world, extractive industries, largescale infrastructure and monoculture tree plantations can continue their social, environmental and climatic destruction while selling themselves as ‘green’ and ‘sustainable’. People defending territories, biodiversities, forests, lakes, rivers and all the interconnected ecosystems with which they have co-existed for centuries are the ones ‘preserving’ and promoting real options for environmental protection and social change. The offsets (il)logic subjugates nature and its people, and forces them to become providers of ‘services’ that ‘work’ towards the accumulation of capital for a few pockets. Read full report here
Click on above image to access Climate Institute’s carbon removal animation for an understanding about what is carbon capture and storage.
IPCC Special Report Chapter 3 – Capture of CO2 The purpose of CO2 capture is to produce a concentrated stream that can be readily transported to a CO2 storage site. CO2 capture and storage is most applicable to large, centralized sources like power plants and large industries. Capture technologies also open the way for large-scale production of low-carbon or carbon-free electricity and fuels for transportation, as well as for small-scale or distributed applications.There are four basic systems for capturing CO2 from use of fossil fuels and/or biomass:
- Capture from industrial process streams (described in Section 3.2): CO2 has been captured from industrial process streams for 80 years (Kohl and Nielsen, 1997), although most of the CO2 that is captured is vented to the atmosphere because there is no incentive or requirement to store it.
- Post-combustion capture (described in Section 3.3): Capture of CO2 from flue gases produced by combustion of fossil fuels and biomass in air is referred to as post-combustion capture. Instead of being discharged directly to the atmosphere, flue gas is passed through equipment which separates most of the CO2 . The CO2 is fed to a storage reservoir and the remaining flue gas is discharged to the atmosphere
- Oxy-fuel combustion capture (described in Section 3.4): In oxy-fuel combustion, nearly pure oxygen is used for combustion instead of air, resulting in a flue gas that is mainly CO2 and H2 O. If fuel is burnt in pure oxygen, the flame temperature is excessively high, but CO2 and/or H2 O-rich flue gas can be recycled to the combustor to moderate this.
- Pre-combustion capture (described in Section 3.5). Pre-combustion capture involves reacting a fuel with oxygen or air and/or steam to give mainly a ‘synthesis gas (syngas)’ or ‘fuel gas’ composed of carbon monoxide and hydrogen.
Other Ways of Carbon Capture
- Chemical scrubbers using certain chemical reactions to remove CO2 that’s already in the atmosphere such as this plan for artificial trees.
- Reducing ocean acidification by adding crushed limestone to the oceans.
- Fertilizing the oceans with iron or urea to promote plankton growth.
- Reducing the CO2 from decomposing plant matter by either burring it or turning it into biochar, to be burnt like coal.
Carbon Storage – There are three places geoengineers are looking to put the carbon after capturing it.
- Geologic storage-pumping condensed CO2 in old oil reservoirs, or in non efficient coal deposits.
- Ocean storage putting CO2 in the natural sink of the oceans
- Storage in deep saline aquifers in the earths crust.
Access a range of articles on the issue from The Conversation here
2 July 2015, Climate News Network, Carbon capture goes down the tubes: One of the much-heralded solutions to climate change which its supporters believe could enable the world to continue to burn fossil fuels looks likely to be a failure. Carbon capture and storage (CCS) is backed by governments and the International Energy Agency (IEA) as one of the best methods of reducing carbon dioxide levels in the atmosphere and saving the planet from overheating. The problem is that despite this enthusiasm and the fact that CCS (also called carbon sequestration) is technically possible, it is not happening. It is cheaper and easier to build wind and solar farms to produce electricity than it is to collect and store the carbon from coal-powered plants’ emissions. For years CO2 has been used by injecting it into old oil wells to extract more fuel, but the cost of building new plants just to store the gas is proving prohibitive. Hundreds of plants were expected to be up and running by 2030, but so far none has been built. Despite this, the IEA and governments across the world are relying on CCS to save the planet from climate change. For example, official policy in the UK still envisages up to fifty industrial plants and power stations using CCS being linked to CO2 pipelines which would inject the gas into old oil and gas wells, removing it from the atmosphere for ever. But research by Mads Dahl Gjefsen, a scientist at the TIK Centre of Technology, Innovation and Culture at the University of Oslo, Norway, says pessimism prevails within the industry about the future of carbon capture and storage in both the US and the European Union. Read More here
29 June 2015, Science Daily, Pessimism prevails about the future of carbon capture and storage in both the USA and EU. This is despite the fine promises that it was precisely this technology that would save the oil and gas industry. “There’s a sombre mood among people who work with carbon capture and storage now. Lobbyists in the US and the EU wonder how much longer they can keep going,” says Mads Dahl Gjefsen, a scientist at the TIK Centre of Technology, Innovation and Culture at the University of Oslo. In his PhD thesis: “Vehicle or destination? Discordant perspectives in CCS advocacy”,he has studied how different players work to gain support for CCS. Murkiness in the corridors of Power Norway has invested several billion kroner in the research and development of carbon capture and storage (CCS). The technology was intended to reduce emissions from the oil and gas industry, and in 2007 former Prime Minister Jens Stoltenberg said that CCS would be Norway’s moon landing. But a full-scale treatment plant at Mongstad never came to fruition. The major challenge has been that the technology is energy-intensive and too costly for large-scale use. And this is not just a Norwegian problem. According to Gjefsen, the enthusiasm for CCS in the corridors of power has gradually dissipated in both the USA and EU. Read More here
Pricing carbon is key to investors’ understanding of the risks corporations face if they do not manage their climate change exposure, as well as new revenue opportunities inherent in addressing climate change head on. Over the past 15 years, CDP has been gathering and synthesizing information on how companies have been using carbon pricing in their internal planning. We’ve been able to keep a close track of this growing trend. In 2014 we published a report showing how 150 companies globally already incorporate a price on carbon emissions into their business decision-making. These companies fully expect carbon emissions will one day have to be capped and regulated worldwide. Associating a dollar cost with each ton of carbon emitted now, before required, is a way to prepare for future regulation and a smart strategy for early adopters. Read More here
27 May 2015, Carbon Brief, Carbon pricing schemes climb to $50bn, despite Australian backtracking: The value of carbon pricing schemes rose to $50 billion in 2015, according to a new assessment by the World Bank. It outlines its findings in the latest edition ofCarbon Pricing Watch, which examines the state of the world’s carbon markets in advance of its more detailed report due later this year. As of 1 April 2015, emissions trading schemes were valued at $34 billion, up from $32 billion the previous year. This was despite the repeal of Australia’s carbon pricing mechanism in July 2014 at the hands of prime minister Tony Abbott.
Emissions trading schemes are not the only way to put a price on carbon. For the first time, the World Bank has also valued carbon taxes across the world, which it finds amount to $14 billion. The World Bank calculated the value of emissions trading schemes by multiplying the allowances issued for each scheme, multiplied by the price. Estimates of the price of carbon taxes were based on government budgets for 2015, or by the greenhouse gas emissions covered by the carbon price on 1 April 2015. All in all, emissions are currently being priced in 39 nations and 23 subnational jurisdictions, as the World Bank map shows below.
Map of existing and potential carbon pricing schemes. Source: World Bank Carbon Pricing Watch 2015
The report says in 2015, carbon pricing covered around 12% of the world’s emissions.
The actual volume of carbon that was covered by a carbon price in 2015 rose slightly from the previous year, from almost 6 gigatonnes of carbon dioxide equivalent up to 7 gigatonnes, the World Bank report says.
Over the last decade, the picture has changed more dramatically, as the graph below shows. In 2005, only 4% of the world’s annual greenhouse gas emissions were priced, and almost all of this was a result of the EU’s newly launched emissions trading system (EU ETS). Read More here
13 May 2015, An innovative game to explore the range of futures open to the pastoral industry within a carbon economy has been launched by Federation University Australia. The game, Narmboolville, is based on the Sovereign Hill property Narmbool, 15 km south east of Ballarat. It brings together environmental science, accounting and information technology and is the culmination of a two-year research project supported by the Williamson H.D. Trust and Sovereign Hill Museums Association.
“We saw Narmbool as a fantastic location to demonstrate the options that may present themselves for agriculture into the future, not least because of the excellent environmental education program associated with the property,” Professor Peter Gell, one of the co-ordinators of the project, said. “The main challenge was the real interdisciplinary nature of the project as we wanted to ensure that the game was based on real scientific data and real carbon accounting approaches. “We then let the IT boffins loose to create a really engaging game that tests your skills as a farm manager.”
The objective of this project is to bring together the principles of carbon sequestration and livestock management to encourage sustainable farm management practices under a range of future climate scenarios. The game, developed under the guidance of project co-coordinator Dr Charlynn Miller from FedUni, requires the user to secure an income from carbon but also seek to maintain an economically viable farm business.
In essence the user becomes the farm manager, making decisions about the trade-off between managing for trees and agricultural production. The game is freely accessible via the University’s Narmbool game website.
When starting the game, you can choose how much carbon you would like to sell as Australian Carbon Credit Units (ACCUs). ACCUs are regulated carbon credits issued by the Clean Energy Regulator for Australian sequestration or emission reduction projects. When you choose the amount of stored carbon to sell as ACCUs, keep in mind that a risk of reversal buffer will be deducted from your ACCUs. The larger the buffer size, the less ACCUs you will be issued upfront but the greater chance you will be able to maintain the carbon storage for 100 years. Basically, you promise to store carbon in the land and trees of Narmbool for 100 years and get paid to do it! Just make sure you manage the property well so that you don’t go broke in the meantime!