Open AccessLand contribution to natural CO 2 variability on time scales of centuries
Author(s) -
Schneck Rainer,
Reick Christian H.,
Raddatz Thomas
Publication year - 2013
Publication title -
journal of advances in modeling earth systems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.03
H-Index - 58
ISSN - 1942-2466
DOI - 10.1002/jame.20029
Subject(s) - environmental science , biosphere , primary production , carbon cycle , climatology , atmospheric sciences , coupled model intercomparison project , earth system science , shortwave , data assimilation , greenhouse gas , climate change , climate model , meteorology , ecosystem , geography , geology , radiative transfer , physics , ecology , oceanography , quantum mechanics , astronomy , biology
The present paper addresses the origin of natural variability arising internally from the climate system of the global carbon cycle at centennial time scales. The investigation is based on the Max Planck Institute for Meteorology, Coupled Model Intercomparison Project Phase 5 (MPI‐MCMIP5) preindustrial control simulations with the MPI Earth System Model in low resolution (MPI‐ESM‐LR) supplemented by additional simulations conducted for further analysis. The simulations show a distinct low‐frequency component in the global terrestrial carbon content that induces atmospheric CO 2 variations on centennial time scales of up to 3 ppm. The main drivers for these variations are low‐frequency fluctuations in net primary production (NPP) of the land biosphere. The signal arises from small regions scattered across the whole globe with a pronounced source in North America. The main reason for the global NPP fluctuations is found in climatic changes leading to long‐term variations in leaf area index, which largely determines the strength of photosynthetic carbon assimilation. The underlying climatic changes encompass several spatial diverse climatic alterations. For the particular case of North America, the carbon storage changes are (besides NPP) also dependent on soil respiration. This second mechanism is strongly connected to low‐frequency variations in incoming shortwave radiation at the surface.