Impacts ranged from a strong increase to a severe loss
of vegetation carbon (cv), depending on differences in climate projections, as well as the physiological response to rising [CO2].
Analyses of differences in model behavior should therefore focus not only on the processes of carbon acquisition (i.e., photosynthesis and NPP), but also on the dynamics
of vegetation carbon turnover.
Not exact matches
Eating less meat will free up a lot
of agricultural land which can revert to growing trees and other
vegetation, which, in turn, will absorb more
carbon dioxide from the atmosphere.
Evidence suggests that the Indians, through the burning
of remnants
of logs, branches, weeds, crop remains, felled secondary growth
vegetation, near - by forest litter, and cut material brought to the fields along with kitchen - fire
carbon and ash from the houses, modified the fertility
of their soils.
With global climate models projecting further drying over the Amazon in the future, the potential loss
of vegetation and the associated loss
of carbon storage may speed up global climate change.
Determining the rate
of old
carbon release from permafrost had been a challenge for researchers, since
vegetation that grows in thawed permafrost in forest and tundra systems releases its own modern organic
carbon into soils, which readily decomposes and dilutes the «old
carbon» signal from thawing permafrost soils.
The simulations suggested that the indirect effects
of increased CO2 on net primary productivity (how much
carbon dioxide
vegetation takes in during photosynthesis minus how much
carbon dioxide the plants release during respiration) are large and variable, ranging from less than 10 per cent to more than 100 per cent
of the size
of direct effects.
The researchers believe the greening is a response to higher atmospheric
carbon dioxide inducing decreases in plant stomatal conductance — the measure
of the rate
of passage
of carbon dioxide entering, or water vapor exiting, through the stomata
of a leaf — and increases in soil water, thus enhancing
vegetation growth.
This is because firstly, the micro-organisms that break down dead trees produce copious amounts
of CO2, and secondly, there is less
vegetation remaining that can remove the greenhouse gas from the air by capturing the
carbon in leaves, trunks and roots as part
of its growth cycle.
«We were surprised that, no matter where we looked, roughly half
of the
carbon in river insects had originated from
vegetation in the surrounding landscape rather than the river itself — in other words leaves falling or being blown into the river,» said lead author Dr Stephen Thomas, from Cardiff University's School
of Biosciences.
Woody
vegetation also may be expanding in grasslands because
of more
carbon dioxide in the atmosphere, Dodds said.
If damaged, they would stop capturing
carbon dioxide and a large amount
of it could be released into the atmosphere by decomposing
vegetation
The method takes advantage
of varying levels
of carbon and hydrogen isotopes in the soil, water, and
vegetation at different latitudes.
So even though the natural processes, the
vegetation, the bacteria, the soil are enormous fluxors
of carbon, in fact there are larger fluxors
of carbon than our fossil fuel release, but we can see that they would have been in balance for the 10,000 years going back in time.
Prior to this study, «the understanding
of permafrost feedbacks to climate change had been limited by a lack
of data examining warming effects on both
vegetation and permafrost
carbon simultaneously,» said Dr. Natali.
To understand the complex relationship that determines the fate
of soil
carbon, the Dartmouth researchers collected soil from shrub and grass
vegetation in western Greenland and conducted controlled experiments back in the laboratory.
They measured
carbon dioxide emissions from mineral soils
of the two
vegetation types incubated at five temperatures and two moisture levels.
We like to think
of green,
carbon - absorbing
vegetation as our ally in the fight against global warming.
They then selectively removed different plant species such as heather, cotton grass and moss enabling them to study the effects
of both warming and
vegetation change on
carbon release from the dead plant material into the atmosphere.
Dr Sue Ward, the Senior Research Associate for the project at Lancaster University, said: «Peat is one
of the earth's most important stores
of carbon, but one
of the most vulnerable to changes in climate and changes in
vegetation caused by both climate and land management.
«This study is further evidence that the diversity and makeup
of the
vegetation, and the soil organisms beneath our feet are vitally important in controlling how much
carbon is locked up or released from these
carbon rich ecosystems.»
In addition to the «fertiliser effect» on
vegetation of rising
carbon dioxide levels (12 October, p 40), the work
of...
«If ozone continues to increase,
vegetation will take up less and less
of our
carbon dioxide emissions, which will leave more CO2 in the atmosphere, adding to global warming,» Sitch says.
Although
carbon stocks may be the same with or without understory
vegetation, by controlling competing
vegetation,
carbon is reallocated into the trees instead
of shrubs; and
carbon loss to wildfire is reduced.
This means that more
carbon is accumulating in forests and other
vegetation and soils in the Northern Hemisphere during the summer, and more
carbon is being released in the fall and winter, says study lead scientist Heather Graven
of SIO.
Only three per cent
of existing plant species have C4 lineages but they account for 25 per cent
of carbon fixation by
vegetation on Earth.
The unnerving new estimate puts permafrost up there with soils (1,500 gigatons) and
vegetation (650 gigatons), Earth's second and third largest repositories
of carbon after the oceans.
The cows» manure would also recycle nutrients such as nitrogen and phosphorous to the soil, encouraging the growth
of new
vegetation and sequestering even more
carbon.
Though these processes are influenced by factors including climate,
vegetation and human activity, erosion is the main factor that affects the amount
of carbon that ends up in rivers.
Research conducted by Jin - Soo Kim and Professor Jong - Seong Kug from the Division
of Environmental Science and Engineering at Pohang University
of Science and Technology (POSTECH), in collaboration with Professor Su - Jong Jeong from the School
of Environmental Science and Engineering at South University
of Science and Technology
of China, has shown that the warmer Arctic has triggered cooler winters and springs in North America, which has in turn weakened
vegetation growth and lowered
carbon uptake capacity in its ecosystems.
Instruments on the platforms will monitor changes in the concentrations
of gases such
carbon dioxide, which is mainly produced when
vegetation is burnt during the dry season.
When members
of the Argonne team arrived at Murdock in 2004 for an initial assessment, they found trace levels
of «
carbon tet» in the resident
vegetation.
To explore how well the timing
of the changes matched up, the researcher focused on a
carbon isotope called 13C, which is retained in soil in the same proportions as in the
vegetation the soil once contained.
She has already found a large increase in soil
carbon two years after a single application
of compost, probably due to enhanced
vegetation growth.
The amount and type
of genetic material, along with
carbon dating
of the samples, reveal that between 50,000 and 25,000 years ago — before the peak
of the last ice age — arctic
vegetation consisted mainly
of forbs, the researchers report today in Nature.
Another co-author, Rhonda Quinn
of Seton Hall University, studied
carbon isotopes in the soil, which along with animal fossils at the site allowed researchers to reconstruct the area's
vegetation.
These wetland ecosystems contain live
vegetation at the surface, but house extensive stores
of dead,
carbon - rich organic matter underground.
More natural processes
of cloud brightening or enhanced weathering are less likely to raise objections, but the public react best to creating biochar (making charcoal from
vegetation to lock in CO2) or capturing
carbon directly from the air.»
Weather conditions strongly affect the litter production by
vegetation and the decomposition
of organic matter, in particular, and thus soil
carbon stock changes.
This study highlights the key role
of vegetation in controlling future terrestrial hydrologic response and emphasizes that the continental
carbon and water cycles are intimately coupled over land and must be studied as an interconnected system.
Based on satellite monitoring and models that estimate the
carbon released from burning
vegetation (plus or minus 50 percent), the group reckons that U.S. fires produce 290 million metric tons
of carbon per year, equal to about 5 percent
of the nation's annual emissions from fossil fuels.
For this subsystem, many
of the longer term feedbacks in the full climate system (such as ice sheets,
vegetation response, the
carbon cycle) and some
of the shorter term bio-geophysical feedbacks (methane, dust and other aerosols) are explicitly excluded.
The climate sensitivity classically defined is the response
of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures, clouds, water vapour, winds, snow, sea ice etc.), but before any
of the «slow» feedbacks have kicked in (ice sheets,
vegetation,
carbon cycle etc.).
The study, recently published in the journal Proceedings
of National Academy
of Sciences (PNAS), details how NASA experts and their peers determined a stunning new way to conduct the normal «apples - to - apples» comparison between various forms
of vegetation as a
carbon sink.
Forests and other land
vegetation currently remove up to 30 percent
of human
carbon dioxide emissions from the atmosphere during photosynthesis, but thanks to this latest study, experts now know that we have tropical forests to thank for a great deal
of this work - absorbing a whopping 1.4 billion metric tons
of CO2 out
of a total total global absorption
of 2.5 billion metric tons.
Tropical forests are especially important because, even though they cover only 7 percent
of the Earth's surface, they contain the largest
vegetation carbon stocks, and are also important
carbon sinks.
GEDI's
vegetation measurements will help close a critical gap in our current understanding
of how
carbon is stored and emitted over time by forests and other ecosystems.
an emerging body
of science indicates that rapidly increasing atmospheric
carbon dioxide may be boosting the onrushing waves
of woody
vegetation.
Desertification also contributes to climate change, with land degradation and related loss
of vegetation resulting in increased emissions and reduced
carbon sink.
Sitch, S., et al., 2003: Evaluation
of ecosystem dynamics, plant geography and terrestrial
carbon cycling in the LPJ dynamic global
vegetation model.