'Scary' climate message from past
BBC News.com, Sept. 10, 2009
A new historical record of carbon dioxide levels suggests current political targets on climate may be "playing with fire", scientists say.
Researchers used ocean sediments to plot CO2 levels back 20 million years.
Levels similar to those now commonly regarded as adequate to tackle climate change were associated with sea levels 25-40m (80-130 ft) higher than today.
Scientists write in the journal Science that this extends knowledge of the link between CO2 and climate back in time.
The last 800,000 years have been mapped relatively well from ice cores drilled in Antarctica, where historical temperatures and atmospheric content have left a series of chemical clues in the layers of ice.
But looking back further has been more problematic; and the new record contains much more precise estimates of historical records than have been available before for the 20 million year timeframe.
The new research was able to look back to the Miocene period, which began a little over 20 million years ago.
At the start of the period, carbon dioxide concentrations in the atmosphere stood at about 400 parts per million (ppm) before beginning to decline about 14 million years ago - a trend that eventually led to formation of the Antarctic icecap and perennial sea ice cover in the Arctic.
The high concentrations were probably sustained by prolonged volcanic activity in what is now the Columbia River basin of North America, where rock formations called flood basalts relate a history of molten rock flowing routinely onto the planet's surface.
In the intervening millennia, CO2 concentrations have been much lower; in the last few million years they cycled between 180ppm and 280ppm in rhythm with the sequence of ice ages and warmer interglacial periods.
Now, humanity's emissions of greenhouse gases are pushing towards the 400ppm range, which will very likely be reached within a decade.
"What we have shown is that in the last period when CO2 levels were sustained at levels close to where they are today, there was no icecap on Antarctica and sea levels were 25-40m higher," said research leader Aradhna Tripati from the University of California at Los Angeles (UCLA).
"At CO2 levels that are sustained at or near modern day values, you don't need to have a major change in CO2 levels to get major changes in ice sheets," she told BBC News.
The elevated CO2 and sea levels were associated with temperatures about 3-6C (5-11F) higher than today.
The data comes from the ratios of boron and calcium in the shells of tiny marine organisms called foraminifera.
The ratio indicates the pH of sea water at the time the organisms grew, which in turn allows scientists to calculate the carbon dioxide content of the atmosphere.
The shell fragments came from cores drilled from the floor of the Pacific Ocean.
According to Jonathan Overpeck, who co-chaired the Intergovernmental Panel on Climate Change (IPCC) work on ancient climates for the organisation's last major report in 2007, this provides a more accurate look at how past CO2 values relate to climate than previous methods.
"This is yet another paper that makes the future look more scary than previously thought by many," said the University of Arizona scientist.
"If anyone still doubts the link between CO2 and climate, they should read this paper."
The new research does not imply that reaching CO2 levels this high would definitely result in huge sea level changes, or that these would happen quickly, Dr Tripati pointed out - just that sustaining such levels on a long timescale might produce such changes.
"There aren't any perfect analogies in the past for climate change today or in the future," she said.
"We can say that we've identified past tipping points for ice sheet stability; the basic physics governing ice sheets that we've known from ice cores are extended further back, and... I think we should use our knowledge of the physics of climate change in the past to prepare for the future."
At the Rio Earth Summit of 1992, governments pledged to stabilise greenhouse gas concentrations "at a level that would prevent dangerous anthropogenic interference with the climate system".
What that level is has been the subject of intense debate down the years; but one figure currently receiving a lot of support is 450ppm.
On Tuesday, for example, the International Energy Agency (IEA) released its prescription for tackling climate change, which sees concentrations of greenhouse gases peaking at the equivalent of 510ppm of CO2 before stabilising at 450ppm.
The Boxer-Kerry Bill, which has just entered the US Senate, also cites the 450 figure.
"Trouble is, we don't know where the critical CO2 or temperature threshold is beyond which ice sheet collapse is inevitable," said Dr Overpeck.
"It could be below 450ppm, but it is more likely higher - not necessarily a lot higher - than 450ppm.
"But what this new work suggests is that... efforts to stabilise at 450ppm should avoid going up above that level prior to stabilisation - that is, some sort of 'overshoot' above 450ppm on the way to stabilisation could be playing with fire."
Because of concerns about short-term sea level rise, the Association of Small Island States (Aosis), which includes low-lying countries such as The Maldives, Palau and Grenada, is pushing for adoption of the much lower figure of 350ppm.
But with concentrations already substantially higher, political support for that is scanty outside Aosis members.
Scientific American, Oct. 8, 2009
Carbon dioxide levels climbing toward a doubling of the 280 parts per million (ppm) concentration found in the preindustrial atmosphere pose the question: What impact will this increased greenhouse gas load have on the climate? If relatively small changes in CO2 levels have big effects—meaning that we live in a more sensitive climate system—the planet could warm by as much as 6 degrees Celsius on average with attendant results such as changed weather patterns and sea-level rise. A less sensitive climate system would mean average warming of less than 2 degrees C and, therefore, fewer ramifications from global warming.
Human civilization is now running an experiment (and without a control) that will definitively determine the answer. Scientists, however, have also realized that history can be a guide: Two new papers published in Science this week examine the historical record preserved in a stalagmite and microscopic seashells, respectively, to offer some clues.
Earth scientist Aradhna Tripati of the University of California, Los Angeles's Department of Earth and Space Sciences and her colleagues extracted a record of past atmospheric concentrations of CO2 stretching back 20 million years from the shells of tiny creatures known as foraminifera buried in a column of ocean mud and rock. The microscopic animals build shells of calcium carbonate out of minerals in seawater—a process that is affected by the water's relative pH (acidity), which is, in turn controlled by the level of CO2 in the atmosphere. More CO2 in the atmosphere means a more acidic ocean.
"The two species we picked to analyze [Globigerinoides ruber and G. sacculifer] are both ones that are around today, and the living animals actually have photosynthetic algae as symbionts, which means that they live in the surface ocean, since the algae require sunlight to survive," Tripati explains. And that means the fossil record of their shells will reveal the relative acidity of the surface waters in the ratio of boron to calcium as well as the specific chemical signature of the boron itself. "When seawater is more acidic, less boron gets incorporated into the calcium carbonate shells," she adds.
The researchers first matched this fossil record secured by the Integrated Ocean Drilling Program Expedition in the western tropical Pacific to existing records from bubbles trapped in Antarctic ice cores that stretch back 800,000 years, which preserve a precise record of past atmospheric composition. Thus reassured of the technique's accuracy, they plunged back into deep geologic time.
"Modern-day levels of carbon dioxide were last reached about 15 million years ago," Tripati says, when sea levels were at least 25 meters higher and temperatures were at least 3 degrees C warmer on average. "During the middle Miocene, an [epoch] in Earth's history when carbon dioxide levels were sustained at values similar to what they are today [330 to 500 ppm], the planet was much warmer, sea level was higher, there was substantially less ice at the poles, and the distribution of rainfall was very different."
Further, "at no time in the last 20 million years have levels of carbon dioxide increased as rapidly as at present," Tripati adds; CO2 concentrations have climbed from 280 ppm to 387 ppm in the past 200 years. And "our work indicates that moderate changes in carbon dioxide levels of 100 to 200 parts per million were associated with major climate transitions and large changes in temperature"—indicative of a very sensitive climate.
The rock record reveals that such rainfall changes occur at the same time as general alterations in the relative strength of sunlight hitting the planet thanks to periodic shifts in Earth's orbit, known as Milankovitch cycles. At the same time as the solar heat increases, according to the monsoon record published in Science, CO2 levels also begin to rise.
"Climate systems are well linked worldwide, such as sea-level, CO2, ice sheet[s], the Asian monsoon, regional temperature and precipitation," Cheng says. "So a change in one of them could trigger changes in others." And that might mean the climate is too sensitive to tolerate current levels of CO2 without changing the conditions that have allowed human civilization to flourish in the past 10,000 years.