The substitution of high‐resolution terrestrial biosphere models and carbon sequestration in response to changing CO2 and climate
- 1 September 1999
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 13 (3) , 785-802
- https://doi.org/10.1029/1999gb900035
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- The variability in the carbon sinks as reconstructed for the last 1000 yearsGeophysical Research Letters, 1999
- Comparing global models of terrestrial net primary productivity (NPP): analysis of the seasonal atmospheric CO2 signalGlobal Change Biology, 1999
- Terrestrial carbon storage during the past 200 years: A Monte Carlo Analysis of CO2 data from ice core and atmospheric measurementsGlobal Biogeochemical Cycles, 1997
- Change in net primary production and heterotrophic respiration: How much is necessary to sustain the terrestrial carbon sink?Global Biogeochemical Cycles, 1996
- On the relations between the oceanic uptake of CO2 and its carbon isotopesGlobal Biogeochemical Cycles, 1996
- Climatic, edaphic, and biotic controls over storage and turnover of carbon in soilsGlobal Biogeochemical Cycles, 1994
- Structure of a global and seasonal carbon exchange model for the terrestrial biosphere the frankfurt biosphere model (FBM)Water, Air, & Soil Pollution, 1993
- Interactions between carbon and nitrogen dynamics in estimating net primary productivity for potential vegetation in North AmericaGlobal Biogeochemical Cycles, 1992
- Transport and storage of CO2 in the ocean ??an inorganic ocean-circulation carbon cycle modelClimate Dynamics, 1987
- A biochemical model of photosynthetic CO2 assimilation in leaves of C3 speciesPlanta, 1980