Happy
new year everyone! I grab this opportunity to travel north, near Santa’s house,
to write about the soil carbon ‘under’ the snow.
As
you know, nowadays, the snow on the poles melts faster in comparison to the previous
years, affected by the human activity and the global warming. You can check some
of my classmates’ blogs concerning the climate change in Arctic (check right in
the blog column). It is time for me to add something about the soil carbon.
Lands
near north pole, where frozen soil layers are observed all over the year, have
become large carbon storage and they can be characterised as carbon emitters
due to microbial activity and the global warming (Charles D. Koven et al., 2011).
During the summer season the top layer of the soil (active layer) thaws and
refreezes at winter leaving only the layer below it permanently frozen.
This
permanently frozen ground is very important reservoir for soil carbon although
is not usually taken under consideration in many studies about the global
carbon budget (Sergey
A. Zimov et al. 2006). An example of the crucial role of the carbon release
from the frozen layer, is the carbon emission at the end of the last glacial
age, when the snow retreated back in northern latitudes. In this period, a
potential reduction of soil carbon from 2.6% to 0.15% could have released up to
500 Gt of carbon (Sergey
A. Zimov et al. 2006).
It
could be easily noticed, that the microbial activity in the soil in combination
with the global warming can give a positive feedback in the climate change.
Hence, the rising temperature will continue to melt down the snow resulting in
soil carbon decomposition (Edward A.
G. Schuur et al., 2008).
Modelling
the permafrost declining (CIRES)
In
the figure above, we can observe the climate change impact on the permafrost
areas. The simulation shows the reduction of these areas over a century. As a
result, carbon will be released back into the global cycle and this will
contributes in the global warming.
See
you in the next post and let’s hope we will be able to pay a visit to Santa’s
home the following years.
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