C Gougoulias, JM Clark, LJ Shaw - … of the Science of Food and …, 2014 - Wiley Online Library
It is well known that atmospheric concentrations of carbon dioxide (CO2)(and other greenhouse gases) have increased markedly as a result of human activity since the …
The enhanced vegetation productivity driven by increased concentrations of carbon dioxide (CO2)[ie, the CO2 fertilization effect (CFE)] sustains an important negative feedback on …
Soil carbon (C) is a critical component of Earth system models (ESMs), and its diverse representations are a major source of the large spread across models in the terrestrial C …
Microbes influence soil organic matter decomposition and the long‐term stabilization of carbon (C) in soils. We contend that by revising the representation of microbial processes …
S Menon, KL Denman, G Brasseur, A Chidthaisong… - 2007 - osti.gov
The Earth's climate is determined by a number of complex connected physical, chemical and biological processes occurring in the atmosphere, land and ocean. The radiative properties …
Subfossil pollen and plant macrofossil data derived from 14 C-dated sediment profiles can provide quantitative information on glacial and interglacial climates. The data allow climate …
Soil respiration–RS, the flux of CO 2 from the soil to the atmosphere–is probably the least well constrained component of the terrestrial carbon cycle. Here we introduce the SRDB …
P Peylin, RM Law, KR Gurney, F Chevallier… - …, 2013 - bg.copernicus.org
Atmospheric CO 2 inversions estimate surface carbon fluxes from an optimal fit to atmospheric CO 2 measurements, usually including prior constraints on the flux estimates …
J Kattge, W Knorr, T Raddatz, C Wirth - Global Change Biology, 2009 - Wiley Online Library
Photosynthetic capacity and its relationship to leaf nitrogen content are two of the most sensitive parameters of terrestrial biosphere models (TBM) whose representation in global …