«We found that decomposition converted 60 percent of the carbon
in the thawed permafrost to carbon dioxide in two weeks,» Stubbins said.
Sure, there was warming and glaciers are receding, but the logical leap that this warming is because of humans is simply an unsubstantiated claim, even more so when considering that you can find Roman remains under receded glaciers in the Alps or Viking graves
in thawed permafrost in Greenland.
But determining the size of the permafrost threat also requires calculating how much of the carbon
in thawed permafrost will be decomposed by microbes and released as CO2.
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 Arctic is changing, but nowhere is this less immediately visible than
in the thawing permafrost.
In the thawing permafrost slopes of Ellesmere Island, for instance, Fletcher and colleagues have been mapping black layers of charcoal in sediments dating from the Pliocene.
(1) The reported low contribution of CH4 production to anoxic carbon decomposition
in thawing permafrost is due to the lack of an active methanogen community that only establishes over longer time periods.
Beyond monitoring directly within or above the permafrost, another set of papers have pointed to the role of leaching and export via streams and groundwater to lakes as a significant source of carbon transport
in thawing permafrost.
not just in the thermometer, not in astrology, but it has been recently calculated that there are 793 gigagrams (more than 15 million gallons)
in the thawing permafrost.
Microbial communities
in thawing permafrost contribute a significant amount to atmospheric methane, a greenhouse gas many times more potent than carbon dioxide.
Or the house sinking
in thawing permafrost.
They have, for what they say is the first time, measured in the laboratory the long - term production of methane
in thawing permafrost.
Methane and carbon dioxide are both produced
in thawing permafrost as dead animal and plant remains decompose.
«But we find that
in thawing permafrost, most methane initially doesn't come from acetate as previously assumed, but the other pathway.
The observed effects of cryosphere reduction include modification of river regimes due to enhanced glacial melt, snowmelt advance and enhanced winter base flow; formation of thermokarst terrain and disappearance of surface lakes
in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven by ice and permafrost melting; regional ocean freshening; sea - level rise due to glacier and ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected by lake - ice and sea - ice reduction; changes in livelihoods; reduced tourism activities related to skiing, ice climbing and scenic activities in cryospheric areas affected by degradation; and increased ease of ship transportation in the Arctic.
Microbes
in thawing permafrost: the unknown variable in the climate change equation David E Graham, Matthew D Wallenstein, Tatiana A Vishnivetskaya, Mark P Waldrop, Tommy J Phelps, Susan M Pfiffner, Tullis C Onstott, Lyle G Whyte, Elizaveta M Rivkina, David A Gilichinsky, Dwayne A Elias, Rachel Mackelprang, Nathan C...
Not exact matches
For now, the increases
in CO2 soaked up by new vegetation — including trees now growing where shrubs used to dominate — more than compensate for the amounts of the gas released by
thawing permafrost, the team says.
The world's largest reservoir of mercury lies
in Arctic
permafrost, the layer of frozen soil that's at risk of
thawing because of warming temperatures, The Washington Post reports.
One unknown is how the addition of massive flows of freshwater from Siberian rivers, bolstered by
thawing permafrost, could affect the system, says study co-author Eddy Carmack, an oceanographer with Fisheries and Oceans Canada
in Sidney.
Thawing permafrost may mean more CO2
in the atmosphere but less sea ice may mean more carbon captured by the Arctic ocean
Headed toward an 8 F rise
in warming Other such low - probability but high - risk scenarios mentioned
in the report include ecosystem collapses, destabilization of methane stored
in the seafloor and rapid greenhouse gas emissions from
thawing Arctic
permafrost.
Old carbon isn't part of that equation if it remains trapped
in frozen soil, but it's released as methane and carbon dioxide when
permafrost soils
thaw and decompose.
A University of Alaska Fairbanks - led research project has provided the first modern evidence of a landscape - level
permafrost carbon feedback,
in which
thawing permafrost releases ancient carbon as climate - warming greenhouse gases.
«If you open the freezer door, you
thaw permafrost soil that's been frozen for a long time, and the organic matter
in it is decomposed by microbes,» Walter Anthony said.
The data is important for climate change models, since the emissions released by
thawing permafrost could significantly affect levels of greenhouse gases
in the atmosphere.
Chanton and Hodgkins» work, «Changes
in peat chemistry associated with
permafrost thaw increase greenhouse gas production,» was funded by a three - year, $ 400,000 Department of Energy grant.
The project, led by UAF researcher Katey Walter Anthony, studied lakes
in Alaska, Canada, Sweden and Siberia where
permafrost thaw surrounding lakes led to lake shoreline expansion during the past 60 years.
«We've known for a while now that
permafrost is
thawing,» said Suzanne Hodgkins, the lead author on the paper and a doctoral student
in chemical oceanography at Florida State.
Controlling greenhouse gas emissions
in the coming decades could substantially reduce the consequences of carbon releases from
thawing permafrost during the next 300 years, according to a new paper published this week
in the Proceedings of National Academy of Sciences.
Permafrost expert Dmitry Nicolsky of the UAF Geophysical Institute provided simulation data on changes in the extent of permafrost in the northern hemisphere and the predicted thaw depth under the two
Permafrost expert Dmitry Nicolsky of the UAF Geophysical Institute provided simulation data on changes
in the extent of
permafrost in the northern hemisphere and the predicted thaw depth under the two
permafrost in the northern hemisphere and the predicted
thaw depth under the two scenarios.
For this study, Jansson and colleagues wanted to examine how natural
thawing affected microbes
in tundra transitioning from
permafrost to bog
in the Arctic.
«How drowsy microbes
in Arctic tundra change to methane - makers as
permafrost thaws.»
During the new study the scientists replicated the conditions of a freezing environment
in the
Permafrost Laboratory at the University of Sussex and monitored the freeze -
thaw of six hard and soft limestone blocks during an experiment that simulated 27 years of natural freezing and
thawing.
«This work provides the first demonstration of this combination of omics tools to gain a more mechanistic understanding of life
in permafrost and the changes that occur during natural
thaw,» said Jansson.
The bodies of water, each less than a hectare
in area, fill depressions
in the hummocky tundra landscape with meltwater from
thawing permafrost.
But warmer temperatures, longer growing seasons, and
thawing permafrost (which supplies nutrients) are also promoting the growth of aquatic plants
in the ponds, shrinking the size of the basins.
But
thawing permafrost can have dramatic effects both visible and invisible, from collapsing roads and leaning trees
in Alaska to freeing greenhouse gases that had been frozen for millennia.
While
permafrost thawing or boreal wetlands
in high latitudes have values of about -60 ‰, tropical wetlands — such as would be found
in those regions — have slightly less negative values, about -52 ‰.
In addition to developing maps of near - surface
permafrost distributions, the researchers developed maps of maximum
thaw depth, or active - layer depth, and provided uncertainty estimates.
A high percentage of the world's peat mosses are found
in northern
permafrost areas, where only the top ground layer
thaws in summer, if at all.
Thawing permafrost in the Arctic both dismays and delights her.
«As the climate gets warmer, the
thawing permafrost not only enables the release of more greenhouse gases to the atmosphere, but our study shows that it also allows much more mineral - laden and nutrient - rich water to be transported to rivers, groundwater and eventually the Arctic Ocean,» explained Ryan Toohey, a researcher at the Interior Department's Alaska Climate Science Center
in Anchorage and the lead author of the study.
The warming climate threatens to
thaw permafrost, which will result
in the release of carbon dioxide and methane into the atmosphere creating feedbacks to climate change — more warming and greater
permafrost thaw.
However, sub-lake
permafrost thaw will likely unlock a portion of the
permafrost carbon pool and potentially release this carbon
in the form of greenhouse gases.
Given the amount of carbon stored belowground
in the arctic, it is very unlikely that plant growth can ever fully offset C losses from
permafrost thaw.»
In contrast, the warming on the land may increase the protective vegetation layer and delay
thawing of
permafrost outside of lakes,» said Vladimir Romanovsky of the UAF Geophysical Institute and co-author of the new study.
The climate is warming
in the arctic at twice the rate of the rest of the globe creating a longer growing season and increased plant growth, which captures atmospheric carbon, and
thawing permafrost, which releases carbon into the atmosphere.
More serious for the rest of the world is the possibility that gas hydrates
in permafrost are more vulnerable to
thawing than was thought.
The study entitled «
Permafrost degradation stimulates carbon loss from experimentally warmed tundra,» published in the journal Ecology found that growing season gains do not offset carbon emissions from permaf
Permafrost degradation stimulates carbon loss from experimentally warmed tundra,» published
in the journal Ecology found that growing season gains do not offset carbon emissions from
permafrostpermafrost thaw.
According to Dr. Natali, «Our results show that while
permafrost degradation increased carbon uptake during the growing season,
in line with decadal trends of «greening» tundra, warming and
permafrost thaw also enhanced winter respiration, which doubled annual carbon losses.»