Section 7.2.2. The reservoir of carbon in fossil fuels and mudrocks is also sub-
stantial and a major portion of the latter is thought to be recoverable and thus
available for burning. The smallest reservoirs are the land biosphere (2000 GtC)
and the atmosphere (749 GtC, equivalent to an atmospheric concentration of
about 354 ppm). It is the small size of the latter which makes it sensitive to even
small percentage changes in the other larger reservoirs, where these changes
result in emissions to the atmosphere, as, for example, in the burning of fossil
fuels.
Natural fluxes
It is often assumed that natural flows between the major reservoirs are balanced
two-way fluxes when averaged over the whole year and the total surface of the
reservoir. For example, the land biosphere and the oceans exchange approxi-
mately 120 and 90 GtC yr-^1 respectively in both directions with the atmosphere.
There is, however, some uncertainty about this assumption over periods of years
and it is surely wrong on longer timescales. Evidence for short-term imbalance
comes from careful inspection of the atmospheric record (as shown in Fig. 7.8).
At the end of the record (in the early 1990s) the rate of increase of atmospheric
CO 2 is significantly smaller than for previous years. The explanation for this
decrease in the rate of change is very unlikely to be alterations in anthropogenic
inputs to the atmosphere, since there is no evidence that fossil fuel burning or
Global Change 253
Atmosphere
749 (354 ppm CO 2 ) Annual increase 3.3 ± 0.1
Fossil fuels
and shales
(7500 recoverable)
12 000
1020
38 100
Oceans
Sediments
20 000 000
2000
Land biosphere
Reservoirs
Natural fluxes
Anthropogenic fluxes
Key:
5.4
± 0.3
0.2
(^120) ± 0.7
1.9
(^90) ± 0.6
Fig. 7.9A simplified version of the global carbon cycle for the 1980s. The numbers in boxes indicate the
reservoir size in GtC. Arrows represent fluxes and the associated numbers indicate the magnitude of the flux
in GtC yr-^1. After IPCC (2001). With permission of the Intergovernmental Panel on Climate Change.