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| Titel |
Sensitivity of Holocene atmospheric CO2 and the modern carbon budget to early human land use: analyses with a process-based model |
| VerfasserIn |
B. D. Stocker, K. Strassmann, F. Joos |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1726-4170
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| Digitales Dokument |
URL |
| Erschienen |
In: Biogeosciences ; 8, no. 1 ; Nr. 8, no. 1 (2011-01-17), S.69-88 |
| Datensatznummer |
250005346
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| Publikation (Nr.) |
 copernicus.org/bg-8-69-2011.pdf |
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| Zusammenfassung |
| A Dynamic Global Vegetation model coupled to a simplified Earth
system model is used to simulate the impact of anthropogenic land cover changes (ALCC)
on Holocene atmospheric CO2 and the contemporary carbon cycle.
The model results suggest that early agricultural activities cannot explain
the mid to late Holocene CO2 rise of 20 ppm measured on ice cores and that proposed
upward revisions of Holocene ALCC imply a smaller contemporary terrestrial carbon sink.
A set of illustrative scenarios is applied to test the robustness of these
conclusions and to address the large discrepancies between published ALCC
reconstructions.
Simulated changes in atmospheric CO2 due to ALCC are less than 1 ppm
before 1000 AD and 30 ppm at 2004 AD when the HYDE 3.1 ALCC
reconstruction is prescribed for the past 12 000 years. Cumulative emissions
of 69 GtC at 1850 and 233 GtC at 2004 AD are comparable to earlier estimates.
CO2 changes due to ALCC exceed the simulated natural interannual variability only after
1000 AD.
To consider evidence that land area used per person was higher before than
during early industrialisation, agricultural areas from HYDE 3.1 were increased
by a factor of two prior to 1700 AD (scenario H2). For the H2 scenario, the
contemporary terrestrial carbon sink required to close the atmospheric CO2
budget is reduced by 0.5 GtC yr−1.
Simulated CO2 remains small even in scenarios where average land use per person
is increased beyond the range of published estimates. Even extreme assumptions
for preindustrial land conversion and high per-capita land use do not result
in simulated CO2 emissions that are sufficient to explain the
magnitude and the timing of the late Holocene CO2 increase. |
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