From the Yale School of Forestry & Environmental Studies
Carbon cycle models underestimate indirect role of animals
Animal populations can have a far more significant impact on carbon storage and exchange in regional ecosystems than is typically recognized by global carbon models, according to a new paper authored by researchers at the Yale School of Forestry & Environmental Studies (F&ES).
In fact, in some regions the magnitude of carbon uptake or release due to the effects of specific animal species or groups of animals — such as the pine beetles devouring forests in western North America — can rival the impact of fossil fuel emissions for the same region, according to the paper published in the journal Ecosystems.
While models typically take into account how plants and microbes affect the carbon cycle, they often underestimate how much animals can indirectly alter the absorption, release, or transport of carbon within an ecosystem, says Oswald Schmitz, the Oastler Professor of Population and Community Ecology at F&ES and lead author of the paper. Historically, the role of animals has been largely underplayed since animal species are not distributed globally and because the total biomass of animals is vastly lower than the plants that they rely upon, and therefore contribute little carbon in the way of respiration.
“What these sorts of analyses have not paid attention to is what we call the indirect multiplier effects,” Schmitz says. “And these indirect effects can be quite huge – and disproportionate to the biomass of the species that are instigating the change.”
In the paper, “Animating the Carbon Cycle,” a team of 15 authors from 12 universities, research organizations and government agencies cites numerous cases where animals have triggered profound impacts on the carbon cycle at local and regional levels.
In one case, an unprecedented loss of trees triggered by the pine beetle outbreak in western North America has decreased the net carbon balance on a scale comparable to British Columbia’s current fossil fuel emissions.
And in East Africa, scientists found that a decline in wildebeest populations in the Serengeti-Mara grassland-savanna system decades ago allowed organic matter to accumulate, which eventually led to about 80 percent of the ecosystem to burn annually, releasing carbon from the plants and the soil, before populations recovered in recent years.
“These are examples where the animals’ largest effects are not direct ones,” Schmitz says. “But because of their presence they mitigate or mediate ecosystem processes that then can have these ramifying effects.”
“We hope this article will inspire scientists and managers to include animals when thinking of local and regional carbon budgets,” said Peter Raymond, a professor of ecosystem ecology at the Yale School of Forestry & Environmental Studies.
According to the authors, a more proper assessment of such phenomena could provide insights into management schemes that could help mitigate the threat of climate change.
For example, in the Arctic, where about 500 gigatons of carbon is stored in permafrost, large grazing mammals like caribou and muskoxen can help maintain the grasslands that have a high albedo and thus reflect more solar energy. In addition, by trampling the ground these herds can actually help reduce the rate of permafrost thaw, researchers say.
“It’s almost an argument for rewilding places to make sure that the natural balance of predators and prey are there,” Schmitz says. “We’re not saying that managing animals will offset these carbon emissions. What we’re trying to say is the numbers are of a scale where it is worthwhile to start thinking about how animals could be managed to accomplish that.”
The paper, which is published online in the journal Ecosystems, was inspired by a conference, “Managing Species for Regulating the Carbon Cycle,” hosted by the Yale Climate and Energy Institute in 2012.
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Ferdinand Engelbeen:
I said I intended to give you the ‘last word’ and I still do, but I write to ask you to explain your statement in your post at October 19, 2013 at 3:09 am because I genuinely do not understand it.
Please complete your ‘last word’ by explaining why – having repeatedly asserted the seasonal CO2 variation is a sinusoid – you now agree it is a saw-tooth and claim
How does it make it “even more certain that these processes are limited in capacity”?
As the limit to capacity nears then the rate of sequestration would reduce, and at the same time the rate of temperature change reduces (because it varies sinusoidally through the year) so the ‘pressure’ to sequester would reduce. Hence, as I understand these matters, the saw-tooth denies that the fast sequestration processes saturate prior to the atmospheric CO2 concentration conducting its seasonal reversal.
Please explain why my understanding is wrong and why – as you now say – the saw-tooth “makes it even more certain that these processes are limited in capacity, or they would react more sinusoid-like to the temperature variation”?
And please note that I am not stopping you having the ‘last word’: I am asking you to explain your ‘last word’ because it has come ‘out of the blue’ and I don’t understand it.
Richard
Richard,
One need to be careful with graphs: the Keeling curve is a combination of a near-sinusoid and a trend. But because of the density of the years in the graph, the seasonal variation looks like a saw-tooth in the upgoing trend. If you expand that to one year of seasonal variability only, that gives over the years:
http://www.ferdinand-engelbeen.be/klimaat/klim_img/mlo_co2_seasons.jpg
Where it is clear that at MLO the CO2 swings are quite sinusoidal, which makes it near impossible to know if there are limits in the uptake. That is because there is a lag between the sinks and sources, which are all near ground:
http://www.ferdinand-engelbeen.be/klimaat/klim_img/seasonal_height.jpg
That graph shows that the spring-early summer uptake is sharper near ground than at height, the total variability is higher and CO2 at height lags the variability near ground.
Have a look at Barrow (7 m above sealevel):
http://www.ferdinand-engelbeen.be/klimaat/klim_img/co2_brw_day_2012.jpg
As you can see, that is far more saw-tooth like. Levels stay high in winter, as long as there is snowcover and sea ice. Once temperature is sufficient above freezing, plant growth starts abundantly up to saturation, and then get level, despite temperatures still high enough. On the other hand, biolife goes on to destruct organic debris from earlier years with a peak in fall. That goes up and down with temperature all year round, even under snow cover.
The saw-tooth thus is caused by the saturation of the first phase of plant growth in spring, followed by a much slower growth of new wood in stems and roots and accompanied with a continuous temperature dependent release of CO2 from the decay of fallen leaves and dead shrubs.
Pamela Gray says:
October 17, 2013 at 8:57 am “…If it does anything well at all, it allows climate warmers to point and laugh.”
++++++++++
I do not see how you arrive at making the post above. One of the reasons this blog site is interesting is that we get to read all viewpoints. I rather enjoy richardscourtney’s comments immensely. I hope you are correct when you write “And you will continue on. And on. And on.” Because sometimes repetition of truth will sink in –or give pause to illogical thinking.
One more comment. If you believe your attack on Richard will not have any effect, then why make the attack? What was gained from your post other than to attack?