Hi everyone! Today I will show you a natural continuous
conflict that all people depend on:
The whole system of the carbon cycle “fights back” the
anthropogenic CO2 (one important greenhouse effect) using the fluxes
illustrated in the 2nd post.
- The oceans:
The oceans uptake large amount of CO2 derived
from the difference between the carbon concentrations in the atmosphere and the
surface of the oceans. The limitation of this absorption is that the increase
of the CO2 emissions in the air reduces the uptake from the oceans
because of the:
- Reduction of the buffer capacity of the oceans
- Mixing rate between the surface and the deep water
The result of the carbon dissolved in the sea is the lower
pH that effect the marine life (Prentice et al.,
2003).
- The terrestrial system:
The terrestrial system absorbs the CO2 from the
atmosphere with the help of the vegetation. The carbon sinks in the terrace is
connected with the photosynthesis. More carbon dioxide in the atmosphere means
more production by the plants. On the other hand, high concentration of atmospheric
CO2, does not benefit the production at the same scale. Thus, the
ability of the terrestrial ecosystem to sink carbon from the atmosphere is
limited. (Prentice
et al., 2003)
The following video illustrates the human impact in the
carbon fluxes and the result of the increasing CO2 in the atmosphere
(greenhouse effect).
Next time we will continue our trip in Carbonland examining
the terrestrial mechanisms.
See you!
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