Not exact matches
The WHRC said that widespread deforestation, degradation and disturbance had caused forests to become a «source» of
carbon rather
than a net
carbon «
sink.»
Sinks are those zones that take in more
carbon than they emit, effectively storing the
carbon and preventing it from contributing to global warming.
Now, new research shows that one of the planet's largest and most important
carbon sinks, the forests of northern Eurasia, may be pulling in
carbon at a slower rate
than in the past.
«Our four - year study suggests that AMP grazing can potentially offset greenhouse gas emissions, and the finishing phase of beef production could be a net
carbon sink, with
carbon levels staying in the green rather
than in the red.»
Researchers from the United Kingdom and Brazil also said the pair of droughts have raised concerns that the forest could be approaching a point where it ceases to be a
carbon «
sink,» absorbing more
carbon dioxide from the atmosphere
than it produces, and flips to a
carbon source.
«The amount of
carbon that you can
sink into the Southern Ocean is much less
than I expected.»
Sugar cane provide a better
carbon sink than pasture, leading to a net decrease in emissions.
The U.N. Convention to Combat Desertification estimates that soil, as a
sink for
carbon dioxide, provides a larger reservoir
than either vegetation or the atmosphere, calling its sequestration capabilities «unparalleled.»
The approach ranked as the study's least viable strategy, in part because less
than a quarter of the algae could be expected to eventually
sink to the bottom of the ocean, which would be the only way that
carbon would be sequestered for a long period of time.
«For every ton of CO2 emitted [into] the atmosphere, the natural
sinks are removing less
carbon than before,» says biologist Josep «Pep» Canadell, executive director of the Global
Carbon Project — an Australia — based research consortium devoted to analyzing the pollution behind global warming.
«It essentially means that, through multiple means, in a world with mixotrophs, more organic
carbon is
sinking into the deep ocean
than in a world without mixotrophs,» Follows says.
But for more
than 20 years, experts have warned that the strength of this
carbon «
sink» is declining and will level off around mid-century.
That deep water is not only rich in nutrients, it also has relatively high concentrations of
carbon dioxide, both because it is cold (cold water can absorb and hold more
carbon dioxide
than warm water) and because the decomposition of organic matter that
sinks into the depths releases
carbon dioxide.
Deploying new sensors that drift with sometimes strong currents (allowing better measurement of marine snow
than sensors placed on the ocean floor or tethered to the surface), the team sampled the flora and fauna and measured the amount of falling
carbon material captured to assess the role of the ocean as a true
carbon sink.
The findings suggest that overestimates of China's emissions during this period may be larger
than China's estimated total forest
sink — a natural
carbon store — in 1990 - 2007 (2.66 gigatonnes of
carbon) or China's land
carbon sink in 2000 - 2009 (2.6 gigatonnes of
carbon).
Over recent decades the remaining Amazon forest has acted as a vast «
carbon sink» — absorbing more
carbon from the atmosphere
than it releases — helping to put a brake on the rate of climate change.
The latest IPCC report concludes that the terrestrial biosphere will become a source rather
than a
sink of
carbon before the end of the century.
Small, slow -
sinking organic particles may play a bigger role
than previously thought in the transport of
carbon below the surface ocean.
«And, what puzzles researchers working on the biological
carbon pump: it is higher
than that of non-calcifying phytoplankton and marine snow, the main
sinking particles and organic
carbon sources to the ocean interior».
Another frustrating misstatement in Flannery's book is the suggestion that young forests are better
carbon sinks than old forests, which misses the relaitvley larger
carbon pool (both above and below ground) associated with older forests.
A more sound approach would recognize that (1) converting old forest to young forests releases significant amounts of
carbon (both above and below ground), (2) young forests are only good
carbon sinks if they are allowed to grow and hold onto the
carbon for centuries, yet there are too few economic incentives for doing so, and (2) the fraction of
carbon that is put into long - term storage after logging is very small, i.e. old forests are better at storing
carbon than our disposable culture.
If an element takes up more
carbon than it emits, it is known as a «
carbon sink» and it acts to slow the pace of warming.
«We're trying to ensure that we have healthy, resilient forests that are net
sinks of
carbon so that they're storing more
carbon than they're releasing,» said Russ Henly, a California Natural Resources Agency official who helped draft the plan.
Today, environmentalists tend to describe forests as little more
than «
carbon sinks,» sucking
carbon dioxide from the atmosphere.
No wonder the
carbon sinks are saturating faster
than we thought (see here)-- unmodeled impacts of climate change are destroying them:
Vigorous convective mixing in the deep tropics also dilutes changes in near - surface CO2 much more
than at higher latitudes, so low - altitude sampling contains relatively less information about
carbon sources and
sinks.
Does the «business as usual» referred to here include the recent findings about substantially faster growth in CO2 emissions
than predicted, saturation of
carbon sinks, and arctic ice melting?
Also, dealing with the forests as a «
carbon sink,» deforestation and other factors may have rendered trees as a net
carbon emitter, rather
than a
sink.
Funny how difficult it is for him and his fellow denialati to look at 1) where that
carbon came from 2) its isotopic composition 3) the fact that it takes a while for permafrost to melt and oceans to become a source rather
than a
sink 4) the fact that humans are producing about 2x as much
carbon as is going into the atmosphere 5) the remaining CO2 is acidifying the oceans
A more sound approach would recognize that (1) converting old forest to young forests releases significant amounts of
carbon (both above and below ground), (2) young forests are only good
carbon sinks if they are allowed to grow and hold onto the
carbon for centuries, yet there are too few economic incentives for doing so, and (2) the fraction of
carbon that is put into long - term storage after logging is very small, i.e. old forests are better at storing
carbon than our disposable culture.
In fact the soil
sink capacity is so huge it is more
than all the biomass and all the atmospheric
carbon worldwide combined!
Soil is a vast
carbon sink, containing more
carbon than all terrestrial vegetation and the atmosphere combined.
Not only are they one of the most important
carbon sinks, storing more
carbon than both the atmosphere and the world's oil reserves, they also constantly remove
carbon from the atmosphere through photosynthesis, which converts atmospheric
carbon to organic matter.
Less well known is the immense potential of soils to act as vast
carbon sinks, with the ability to «naturally turn over about 10 times more greenhouse gas on a global scale
than the burning of fossil fuels.»
Those three facts suggest that most if not all of the observed increase in CO2 is natural unless it can be shown that for some reason warming oceans can nevertheless act as a
carbon sink rather
than a
carbon source.
After incorporating these «indirect emission» effects from changes in land use, often into areas valuable as
carbon sinks, the analysis found that biofuels produced from vegetable oils are likely to be worse for the climate
than fossil fuels.
«Cutting trees for fuel is antithetical to the important role that forests play as a
sink for CO2 that might otherwise accumulate in the atmosphere,» Schlesinger writes in an article published yesterday in the journal Science, adding later that
carbon neutrality «is only achieved» if harvested forests are allowed to regrow more biomass
than was lost.
Some regions may even shift from being a
carbon sink to being an atmospheric
carbon dioxide source, 50,51,52 though large uncertainties exist, such as whether projected disturbances to forests will be chronic or episodic.31 Midwest forests are more resilient to forest
carbon losses
than most western forests because of relatively high moisture availability, greater nitrogen deposition (which tends to act as a fertilizer), and lower wildfire risk.50, 51,53
Although global forests currently capture and store more
carbon each year
than they emit, 46 the ability of forests to act as large, global
carbon absorbers («
sinks») may be reduced by projected increased disturbances from insect outbreaks, 47 forest fire, 48 and drought, 49 leading to increases in tree mortality and
carbon emissions.
Using the NDVI, one team this year reported that «over the last few decades of the 20th century, terrestrial ecosystems acted as net
carbon sinks,» i.e., they absorbed more
carbon than they were emitting, and «net greening was reported in all biomes,» though the effect had slowed down in recent years.
If wildfire trends continue, at least initially, this biomass burning will result in
carbon release, suggesting that the forests of the western United States may become a source of increased atmospheric
carbon dioxide rather
than a
sink, even under a relatively modest temperature - increase scenario.
They report that stopping deforestation and allowing young secondary forests to grow back could establish a «forest
sink» — an area that absorbs
carbon dioxide rather
than releasing it into the atmosphere — which by 2100 could grow by over 100 billion metric tons of
carbon, about ten times the current annual rate of global fossil fuel emissions.
«If droughts become more frequent, as expected, the time between droughts may become shorter
than drought recovery time, leading to permanently damaged ecosystems and widespread degradation of the land
carbon sink.»
While it may be critical to sequester ocean
carbon at depths greater
than 1000 meters, this might prove extremely difficult given very high rates of respiration of particulate matter and remineralization by bacteria, resulting in only 1 - 10 % of
sinking particulates reaching depths below 1000 meters.
Meantime the CO2 hypothesis has no predictive power either; likely less so
than all the others; the main problem being that it is only a heating mechanism: To cause a cooling event you need a massive
carbon sink to appear out of nowhere.
The research challenges the long - held belief that forests act as «
carbon sinks» by storing more
carbon than they emit due to natural processes and human activity.
So far, the Arctic is considered a
carbon sink, meaning it absorbs more CO2
than it emits on an annual basis, thanks mainly to the vegetation that grows in the summer.
This decision defined small - scale afforestation or reforestation project activities as those that are expected to result in net anthropogenic GHG removals by
sinks of less
than 8 kilotonnes of
carbon dioxide per year.
«Given our findings, the Arctic is an even smaller
carbon sink than we thought since during some years nearly half of the summer uptake of CO2 is offset with these spring emissions,» Raz - Yaseef said.
The natural fluxes of
carbon are some 24 times the human flux and both natural
sinks and sources vary over less
than a geological age.