Climate controls must cover gases other than CO2

Agriculture is one of the main sources for the greenhouse gas nitrous oxide (N2O) which results from the use of fertilisers. Credit: André Künzelmann/UFZ

Agriculture is one of the main sources for the greenhouse gas nitrous oxide (N2O) which results from the use of fertilisers. Credit: André Künzelmann/UFZ

Cutting emissions of other greenhouse gases would slam the brakes on short-term climate change faster than controlling CO2 alone. But rather than offering an easy way out, warns Jim Butler, director of the Global Monitoring Division at the US National Oceanic and Atmospheric Administration (NOAA), they present both an opportunity and a challenge. “Addressing them can help us see earlier results than we would see with CO2, which poses a problem today but a much bigger one in the future,” he told Simple Climate. “CO2 must be addressed, but ignoring these other gases too could take us to places where we don’t want to go.”

Butler’s division has tracked the levels of different gases in the atmosphere for decades. Among them he says, CO2 rightfully gains most attention. That’s because it traps so much of the sun’s energy, it currently accounts for almost two-thirds of the warming power known as “climate forcing”. “It is responsible for well over 80 per cent of the increase in climate forcing from long-lived gases each year,” Butler said. “It is also very long lived, with around one-fifth of what is emitted hanging around for at least 1,000 years.” Yet as burning oil, natural gas and coal, which produces CO2, propels modern life, cutting the amount we use enough will take some time. “In the meantime there are other gases that could and probably should receive attention,” Butler underlined.

Stephen Montzka of NOAA, along with colleagues Butler and Ed Dlugokencky, looked at exactly how these gases have been affecting climate in top scientific journal Nature this week. Monitoring and evaluating these gases helps show how humans are affecting their levels in the atmosphere. It also serves as a check on the results of claimed emissions. Unfortunately, the amount countries say they produce and levels recorded at observatories across the world disagree. However, Butler noted that no approach is perfect, and that at least comparing the two gave them some idea how far out they were. “The beauty of comparing the two is that each relies on completely different measurements, procedures and assumptions,” he said. Read the rest of this entry »

Soot and methane cuts promise threefold benefits

Vehicles are a significant source of black carbon and other pollutants in many countries. Credit: Caramel/flickr

Vehicles are a significant source of black carbon and other pollutants in many countries. Credit: Caramel/flickr

Limiting methane and soot emissions would save lives and keep farming output high, as well as playing an important role in fighting global warming. That’s according to some 70 scientists who have reviewed the available research on these substances for the United Nations Environment Partnership (UNEP). Such cuts were also surprisingly feasible, with just 16 ways of limiting emissions providing about 90 percent of the possible climate benefit from a list of 2000 control measures.

“We estimate that adoption of the 16 control measures we considered would save about 2 million lives a year and save 50 million tons of crops a year,” said NASA’s Drew Shindell, who led the project. “For climate, putting control measures in place could eliminate about half the warming we’ll otherwise face over the next 40 years.” Read the rest of this entry »

CO2 dominates Earth’s climate, NASA reveals

A new atmosphere-ocean climate modeling study shows that atmospheric carbon dioxide acts as a thermostat in regulating the temperature of Earth. Credit: NASA GISS/ Lilly Del Valle

A new atmosphere-ocean climate modeling study shows that atmospheric carbon dioxide acts as a thermostat in regulating the temperature of Earth. Credit: NASA GISS/ Lilly Del Valle

Almost 200 years after the greenhouse effect was discovered, and 150 years after its experimental proof, NASA scientists have finally demonstrated that CO2 is the most important greenhouse gas. That’s despite the fact that it only accounts for around one-fifth of the Earth’s greenhouse effect, whereas water vapour accounts for about half, and clouds – water in its solid or liquid forms – contribute a quarter.

“It often is stated that water vapour is the chief greenhouse gas (GHG) in the atmosphere,” write NASA’s Andrew Lacis, Gavin Schmidt, David Rind and Reto Ruedy in top journal Science on Thursday. “This would imply that changes in atmospheric CO2 are not important influences on the natural greenhouse capacity of Earth, and that the continuing increase in CO2 due to human activity is therefore not relevant to climate change. This misunderstanding is resolved through simple examination of the terrestrial greenhouse.”

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Saturday round-up: Climate change threatens to quell China’s green revolution

A farmer in Guizhou province, China, holds his poor harvest. Severe drought has greatly affected crops in many parts of China this year. Credit: Xinhua

A farmer in Guizhou province, China, holds his poor harvest. Severe drought has greatly affected crops in many parts of China this year. Credit: Xinhua

China’s remarkable recent surge in agricultural output is at risk from climate change. However,  how much risk won’t be clear without better regional climate predictions and understanding of how crops will react to their altered environment. That’s according to Peking University’s Shilong Piao and his colleagues. “Climate simulations point to serious potential vulnerabilities in China’s future agricultural security,” they wrote in top journal Nature on Thursday, “but extensive uncertainties prevent a definitive conclusion.”

In part those uncertainties come from Chinese farming’s success over the past four decades, increasing rice, maize and wheat yields by 90, 150 and 240 percent respectively. These improvements are vital as the country has just 7 percent of the world’s arable farmland available to feed 22 percent of the world’s population. However, they also obscure the impact of more frequent heat-waves, retreating glaciers and an average 1.2ºC temperature rise in China since 1960. “The improvements of crop management have been so important that they prevent a clear conclusion on the net impact of historical climate change on agriculture,” the team writes.

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Turbo-charged changes create climate roadkill

Jens Borken-Kleefeld, whose work on climate impacts on transport showed car transport creates more warming per passenger mile than flying in the long term. Credit: IIASA

Jens Borken-Kleefeld, whose work on climate impacts on transport showed car transport creates more warming per passenger mile than flying in the long term. Credit: IIASA

If there were to be a speed limit for climate change, humans might soon find their license to wander the globe revoked. That’s because, as Jens Borken-Kleefeld explains, how fast climate is changing can be be just as damaging as the size of the change. He notes that this is covered by the UN Framework Convention on Climate Change. This international agreement pledges to stabilize greenhouse gases in a time frame that will allow natural systems to adapt naturally to climate change.

“If you have a very quick change – as is actually happening today – lots of biosystems and habitats cannot adapt,” he explains. “They are at the verge of extinction. We could trigger some irreversible events, like switching off the Gulf Stream, or melting of the Arctic, which is as much linked to the level but more to the rate of change.”

Borken-Kleefeld is one member of a large team that has been studying people’s tendency to press down on their accelerator, and what this does to the pressure on the climate change pedal. In the journal Environmental Science and Technology they looked at how different modes of transport contribute to warming. While they found that in the long run aviation had less warming impact per passenger mile than driving, the International Institute for Applied Systems Analysis scientists explains that it’s not just the long run that matters. “We are acting on various timescales,” he said. Read the rest of this entry »

Driving up temperatures

While flying has a greater warming impact in the short term, it's actually less warming than driving in the long term - although the warming impact at all timescales must be considered. Credit: iStock

While flying has a greater warming impact in the short term, it's actually less warming than driving in the long term - although the warming impact at all timescales must be considered. Credit: iStock

Driving alone in a car increases global temperatures in the long run more than making the same long-distance journey by air, Austrian and Norwegian researchers said this week. “Car travel emits more CO2 than air travel per passenger mile,” explained Jens Borken-Kleefeld of Austria’s International Institute for Applied Systems Analysis. As CO2 is a very stable chemical, remaining in the atmosphere longer than other gases, cars have a greater long-term impact on climate change. However, aeroplanes’ impact is greater in the short term. “As planes fly at high altitudes, their impact on ozone and clouds is disproportionately high, though short lived,” Borken-Kleefeld said. Writing in the August issue of Environmental Science and Technology, his team point out that all forms of transport are being used all the time. It’s important, therefore, to tackle air pollutants leading to both short-term and long-term warming.

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What can we get out of the ozone hole, 25 years on?

Joe Farman, Brian Gardiner and Jon Shanklin (L-R), the authors of the 1985 paper in which the Antarctic ozone hole was first documented. Here they are pictured with a Dobson ozone spectrophotometer, used to determine stratospheric ozone concentrations. Credit: British Antarctic Survey.

Joe Farman, Brian Gardiner and Jon Shanklin (L-R), the authors of the 1985 paper in which the Antarctic ozone hole was first documented. Here they are pictured with a Dobson ozone spectrophotometer, used to determine stratospheric ozone concentrations. Credit: British Antarctic Survey.

When it comes to the duration of problems in our world’s atmosphere, the greenhouse effect and the ozone hole are the long and the short of it. “The ozone hole went from barely detectable to 50% depletion in around a decade, showing just how fragile our planet is,” explains Jon Shanklin, head of the British Antarctic Survey‘s Meteorology and Ozone Monitoring Unit. “Climate change is expected to proceed more slowly, however we are committing ourselves to changes that will last for many centuries, rather than the single century that should see the ozone layer back to normal.” Read the rest of this entry »

Saturday round-up: Humanity’s upper warming limit

This map shows the maximum wet-bulb temperatures reached in a climate model from a high carbon dioxide emissions future climate scenario with a global-mean temperature 12 degrees Celsius warmer than 2007. The white land areas exceed the wet-bulb limit at which researchers calculated humans would experience a potentially lethal level of heat stress. Credit: Purdue University graphic/Matthew Huber

This map shows the maximum wet-bulb temperatures reached in a climate model from a high carbon dioxide emissions future climate scenario with a global-mean temperature 12 degrees Celsius warmer than 2007. The white land areas exceed the wet-bulb limit at which researchers calculated humans would experience a potentially lethal level of heat stress. Credit: Purdue University graphic/Matthew Huber

Global warming of 12°C would make most areas of the world uninhabitable, and burning all the fossil fuels on the planet could get us to this level. That’s what Steven Sherwood of the University of New South Wales, Australia, and Matthew Huber of Purdue University, USA, claim.

Writing in a paper published online in the Proceedings of the National Academy of Science this week, the scientists examine the heat stress that humans and mammals can bear. This is assessed through a measure known as wet bulb temperature, which combines the effect of heat and humidity. The world’s hottest areas normally have low humidity, referred to as “dry heat”, Huber explained. “When it is dry, we are able to cool our bodies through perspiration and can remain fairly comfortable,” he said.

They say that currently wet bulb temperatures on the planet never exceed 31°C, while humans and other mammals would die if exposed to levels above 35°C for extended periods. They predict that conventional temperature rises of 7°C would begin to see wet bulb temperatures above 35°C in some regions, while 11-12°C rises would force humans out of most areas where they currently live . Read the rest of this entry »

Saturday round-up: Breathing space on CO2 cuts?

As well as satellite measurements, US National Oceanographic and Atmospheric Administration researchers used balloons at a single site in Boulder, Colorado, to find out how much water is in the stratosphere. (Credit NOAA)

Two major papers this week suggest that global warming is likely to accelerate at a slower pace than had previously been thought. In the first, Susan Solomon of the US National Oceanic and Atmospheric Administration has identified a possible cause of lower temperature increases in the noughties compared to the nineties. In the second, David Frank of the University of Bern in Switzerland suggests that the effect of a natural process that worsens man-made climate change has been overstated.

Together with a different set of Bern researchers, Solomon and colleagues in Boulder, Colorado, have shed some light on the poorly understood impact of water in the stratosphere on the world’s temperature. Water vapour in the stratosphere – the layer of the atmosphere above that which we live in – is known to cool that part of the atmosphere down but warm the troposphere underneath. However, it’s taken having satellites floating around the planet to measure accurately how much water is actually there.

The period in which measurements have been possible includes the rapid warming of the 1990s, and slower warming since. Solomon and her colleagues’ measurements show that water concentrations were higher during the warm period, and lower during the cool period. Creating computer models from these data suggest that the drop in stratospheric water vapour after 2000 decreased the rate of warming compared to what would have been otherwise expected by about 25%. The 1990s increase in water vapour could “have steepened the rate of global warming from 1990–2000 by about 30%,” the January 29 Science paper says. The researchers point out that it’s not yet known whether this is a feedback through which the earth tries to cool itself, or something that changes periodically.

The previous day, Frank’s team’s Nature paper tackled the question of just how much CO2 is released from biological sources when the planet warms up, adding to what man is making by burning fossil fuels. “Approximately 40% of the uncertainty related to projected warming of the twenty-first century stems from the unknown behaviour of the carbon cycle,” they write. They evaluated all available large-scale temperature reconstructions and estimates of over the past thousand years. Their results suggest that the likely range of how much CO2 is put into the atmosphere for each degree of warming is likely to be in the lower half of current estimates.

Although neither Frank’s or Solomon’s research team suggests that global warming is about to reverse, taken together they might mean that humanity has longer to fight it than previously thought.

Another process currently helping to cool the globe is the formation of clouds under the ozone hole in the Southern hemisphere, researchers revealed in Geophysical Research Letters on Wednesday. Higher winds that are linked to ozone loss whip up more sea spray, which creates more clouds. These clouds reflect heat from the sun back out into space, helping counteract greenhouse-gas based global warming. The link between the winds that create clouds and ozone loss could lead to the strange situation where a fully-repaired hole could lead to faster worldwide temperature rises.

Outside of climate research this week, a Yale and Mason University survey of 1001 US adults shows that only 57% think that global warming is happening in 2010, compared with 71% in a similar survey in 2008. The proportion that think it is not happening has doubled over that period, to 20% now. Regardless of which side of this debate you stand on, the silver lining may be the reduced amount of stress global warming is now causing Americans: The number who say that they are “very worried” about climate change has fallen from 17% in 2008, to 12% today.
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