Category Archives: Atmospheric Science
Coastal rain forest Mata Atlantica in Brazil. Compared to a natural tropical forest, the results of a study suggest a falling biomass of up to 40 per cent for fragmented forests. (Credit: Dr. Christoph Knogge/UFZ)
ScienceDaily (Dec. 10, 2009) — Deforestation in tropical rain forests could have an even greater impact on climate change than has previously been thought. The combined biomass of a large number of small forest fragments left over after habitat fragmentation can be up to 40 per cent less than in a continuous natural forest of the same overall size.
This is the conclusion reached by German and Brazilian researchers who used a simulation model on data from the Atlantic Forest, a coastal rain forest in the state of São Paulo, Brazil, around 88 per cent of which has already been cleared.
The remaining forest fragments are smaller, so the ratio between area and edge is less favourable. The reason for the reduction in biomass is the higher mortality rate of trees at the edges of forest fragments, according to the results published by researchers from the Helmholtz Centre for Environmental Research and the University of São Paulo in Ecological Modelling. This reduces the number of big old trees, which contain a disproportionately high amount of biomass.
Altered wind conditions and light climate lead to a general change in the microclimate at the forest edges. Big old trees are particularly vulnerable to these factors. With the help of FORMIND, a forest simulation software developed at the UFZ, the researchers modelled different sizes of forest patches left over after landscape fragmentation. The smaller a patch of forest is, the worse is the ratio between edge and area. Simulation results suggest that a natural tropical forest of our study area contained approximately 250 tonnes of aboveground biomass per hectare, a forest fragment measuring 100 hectares has around 228 tonnes of biomass per hectare, while a patch of rain forest measuring one hectare has only 140 tonnes of biomass per hectare. In other words, the biomass in the forest remnants in this study fell by as much as 40 per cent.
“This finding is of great significance for the function of rain forests as a biomass store. It is important to be clear about the fact that we are losing more than just the deforested areas. Even the remaining forest is thinned out as a result. It is a mistake to think only in terms of total area. We have to start thinking in terms of the spatial configuration of the remaining forest fragments as well,” says Dr Jürgen Groeneveld of the UFZ, explaining the significance of the study for climate policy. As well as the biomass yield per hectare, these fragmentation-related spatial (edge) effects also have impacts on climate balance and biodiversity, i.e. on several dimensions of sustainability.
The simulation integrated results from other researchers who are conducting unique long-term experiments on fragmentation in Amazonas. However, a large number of questions remain unanswered: Are the edges stable? Can the forest regenerate or does the degradation continue inwards? The researchers therefore view the figures as a preliminary, cautious estimate.
“But if it is confirmed, it is a really fundamental finding,” adds Dr Sandro Pütz of the UFZ. “Forest fragments cannot perform in the same way as continuous forests.” The researchers therefore intend to investigate the long-term effects over the coming years to find out how the rain forest remnants develop in the long term. The results of this study will also have fundamental consequences for forest conservation, at least in terms of the carbon balance: “In any case, in terms of carbon storage, it is better to protect 100 continuous hectares than to protect 100 one-hectare patches,” says Jürgen Groeneveld.
The data used in the model come from the tropical coastal rain forest in the state of São Paulo, Brazil. The Atlantic Forest was severely deforested in the second half of the 19th century for construction timber, charcoal and grazing and arable land. Although only around an eighth of the original forest area remains, these remnants are still regarded as international biodiversity hot spots, since they are home to an as yet not fully recorded, but impressive number of endangered animal and plant species that are not found anywhere else. Since 2003, Brazilian and German researchers have therefore been investigating the long-term effects of landscape fragmentation on habitats in the Atlantic Forest, which used to stretch along the whole of Brazil’s east coast and is today one of the most endangered rain forests in the world.
The new findings from the ecological modelling experts led by Andreas Huth and Klaus Henle are also relevant for negotiations at the UN climate conference in Copenhagen. Under the heading REDD (Reducing Emissions from Deforestation and Degradation), the conference will be discussing a mechanism for including the forests in climate protection. Forests bind carbon dioxide. Deforestation or degradation of forests leads to a further release or less fixing of carbon dioxide per unit area, thereby increasing the greenhouse effect. Around 20 per cent of total global CO2 emissions comes from the destruction of forests.
- J. Groeneveld, L.F. Alves, L.C. Bernacci, E.L.M. Catharino, C. Knogge, J.P. Metzger: S. Pütz, A. Huth. The impact of fragmentation and density regulation on forest succession in the Atlantic rain forest. Ecological Modelling, 2009; 220 (19): 2450
- M.C. Ribeiro, J.P. Metzger, A.C. Martensen, F.J. Ponzoni and M. M. Hirota. The Brazilian Atlantic Forest: How much is left, and how is the remaining forest distributed? Implications for conservation. Biological Conservation, 2009; 142 (6): 1141
ScienceDaily (July 6, 2009) — The vast amount of carbon stored in the arctic and boreal regions of the world is more than double that previously estimated, according to a study published this week.
The amount of carbon in frozen soils, sediments and river deltas (permafrost) raises new concerns over the role of the northern regions as future sources of greenhouse gases.
“We now estimate the deposits contain over 1.5 trillion tons of frozen carbon, about twice as much carbon as contained in the atmosphere”, said Dr. Charles Tarnocai, Agriculture and Agri-Food Canada, Ottawa, and lead author.
Dr. Pep Canadell, Executive Director of the Global Carbon Project at CSIRO, Australia, and co-author of the study says that the existence of these super-sized deposits of frozen carbon means that any thawing of permafrost due to global warming may lead to significant emissions of the greenhouse gases carbon dioxide and methane.
Carbon deposits frozen thousands of years ago can easily break down when permafrost thaws releasing greenhouse gases to the atmosphere, according to another recent study by some of the same authors.
“Radioactive carbon dating shows that most of the carbon dioxide currently emitted by thawing soils in Alaska was formed and frozen thousands of years ago. The carbon dating demonstrates how easily carbon decomposes when soils thaw under warmer conditions,” said Professor Ted Schuur, University of Florida and co-author of the paper.
The authors point out the large uncertainties surrounding the extent to which permafrost carbon thawing could further accelerate climate change.
“Permafrost carbon is a bit of a wildcard in the efforts to predict future climate change,” said Dr Canadell. “All evidence to date shows that carbon in permafrost is likely to play a significant role in the 21st century climate given the large carbon deposits, the readiness of its organic matter to release greenhouse gases when thawed, and the fact that high latitudes will experience the largest increase in air temperature of all regions.”
Carbon in permafrost is found largely in northern regions including Canada, Greenland, Kazakhstan, Mongolia, Russia, Scandinavia and USA.
The carbon assessment is published this week in the journal of Global Biogeochemical Cycles (GB2023,
doi:10.1029/2008GB003327) of the American Geophysical Union, and the radiocarbon study was recently published in the journal of Nature.