What can stop global warming?
The world's arid areas — deserts filled with scrubby vegetation and sand — are absorbing more of the carbon dioxide that's being emitted into the atmosphere than expected, a new study shows. While these ecosystems will not stop global warming, scientists said the finding provides a better understanding of the carbon cycle, and thus how the global climate will change in the future.
"It is definitely not going to stop it ... just now we are understanding the processes that are going on, " lead author Dave Evans, a biologist specializing in ecology and global change at Washington State University, told NBC News. "But we are still seeing huge amounts of carbon accumulating in the atmosphere."
Carbon dioxide is the main greenhouse gas driving global climate change. More of the planet-warming gas is released into the atmosphere from the burning of fossil fuels, and scientists want to know where it all goes. Reconciling this so-called carbon budget has proven one of the trickier areas of climate science, Evans explained.
It's well-known that some of the carbon dioxide remains in the atmosphere, and the rest gets stored in the land or oceans in other carbon-containing forms, such as microbes, plants and animals. But the finer details of the process are elusive.
Getting a handle on the budget
To get a better handle on the carbon budget, several research teams around the world are conducting so-called free air carbon dioxide enrichment experiments, where plots of land are fumigated with the elevated levels of carbon dioxide expected in the future. This extra carbon dioxide has a specific chemical fingerprint that can be detected when the soils and plants are analyzed.
Akihiro Koyama, now of Colorado State University, and Ben Harlow of Washington State University gather soil samples from a test plot in the Mojave Desert. Desert Research Institute
For 10 years, three of the desert plots received no extra air; three were pumped with air containing carbon dioxide concentrations of 380 parts per million, the current level; and three received concentrations of 550 parts per million, the level expected in 2050.
"After 10 years, the experiment stopped and we dug everything up to ask the question: Is there more carbon under future carbon dioxide conditions than there are under current conditions, " Evans said. "And what we found was, there was indeed more carbon. During those 10 years, carbon accumulated at a faster rate under future CO2 conditions."
'Significant' carbon sinks
The findings indicate that these arid ecosystems are "significant, previously unrecognized sinks" for atmospheric carbon dioxide, Evans and colleagues write in a paper published Sunday in the journal Nature Climate Change.
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"Earth is now at the peak of one of its passing warm spells. It started in the 17th century when there was no industrial influence on the climate to speak of and no such thing as the hothouse effect. The current warming is evidently a natural process and utterly independent of hothouse gases.
The real reasons for climate changes are uneven solar radiation, terrestrial precession (that is, axis gyration), instability of oceanic currents, regular salinity fluctuations of the Arctic Ocean surface waters, etc. There is another, principal reason—solar activity and luminosity. The greater t…
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