|First direct measurement finds more geothermal
heat than expected here
|Pacific Decadal Oscillation may have flipped to
warming phase here
|Study finds Arctic seaice more resilient
than thought here
|Astronomers predict rapid activity fall
The planet's soil releases about 60 billion tons of carbon into the atmosphere each year, which is far more than that released by burning fossil fuels. This happens through a process called soil respiration. This enormous release of carbon is balanced by carbon coming into the soil system from falling leaves and other plant matter, as well as by the underground activities of plant roots.
Short-term warming studies have documented that rising temperatures increase the rate of soil respiration. As a result, scientists have worried that global warming would accelerate the decomposition of carbon in the soil, and decrease the amount of carbon stored there. If true, this would release even more carbon dioxide into the atmosphere, where it would accelerate global warming.
New work by a team of scientists including Carnegie's Greg Asner and Christian Giardina of the U.S. Forest Service used an expansive whole-ecosystem study, the first of its kind, on tropical montane wet forests in Hawaii to sort through the many processes that control soil carbon stocks with changing temperature. Their work is published in Nature Climate Change.
The team revealed that higher temperatures increased the amount of leaf litter falling onto the soil, as well as other underground sources of carbon such as roots. Surprisingly, long-term warming had little effect on the overall storage of carbon in the tropical forest soil or the rate at which that carbon is processed into carbon dioxide.
"If these findings hold true in other tropical regions, then warmer temperatures may not necessarily cause tropical soils to release their carbon to the atmosphere at a faster rate," remarked Asner. "On the other hand, we cannot expect that the soil will soak up more carbon in places where vegetation is stimulated by warmer temperatures. Unlike tropical trees, the soil seems to be on the sidelines in the climate adaptation game."
This means the observed increase in the rate of soil respiration accompanying rising temperatures is due to carbon dioxide released by the an uptick in the amount of litter falling on the forest floor and an increase in carbon from underground sources. It is not from a decrease in the overall amount of carbon stored in the soil.
Giardina noted "While we found that carbon stored in the mineral soil was insensitive to long-term warming, the loss of unprotected carbon responded strongly to temperature. This tells us that the sensitivity of each source of soil respiration needs to be quantified, and the aggregate response examined, before an understanding of ecosystem carbon balance in a warmer world can be achieved."
The universally observed exponential increase in soil-surface CO2 efflux (‘soil respiration’; FS) with increasing temperature has led to speculation that global warming will accelerate soil-organic-carbon (SOC) decomposition1, reduce SOC storage, and drive a positive feedback to future warming2. However, interpreting temperature–FS relationships, and so modelling terrestrial carbon balance in a warmer world, is complicated by the many sources of respired carbon that contribute to FS (ref. 3) and a poor understanding of how temperature influences SOC decomposition rates4. Here we quantified FS, litterfall, bulk SOC and SOC fraction size and turnover, and total below-ground carbon flux (TBCF) across a highly constrained 5.2 °C mean annual temperature (MAT) gradient in tropical montane wet forest5. From these, we determined that: increases in TBCF and litterfall explain >90% of the increase in FS with MAT; bulk SOC and SOC fraction size and turnover rate do not vary with MAT; and increases in TBCF and litterfall do not influence SOC storage or turnover on century to millennial timescales. This gradient study shows that for tropical montane wet forest, long-term and whole-ecosystem warming accelerates below-ground carbon processes with no apparent impact on SOC storage.
Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux by Christian P. Giardina, Creighton M. Litton, Susan E. Crow & Gregory P. Asner published in Nature Climate Change (2014) doi:10.1038/nclimate2322
Read the abstract and get the paper here.
News release issued by The Carnegie Institution for Science and released via EurekAlert! here.
Site by Accentika