Intergovernmental Panel on Climate Change (IPCC). Global carbon and other biogeochemical cycles and feedbacks

JG Canadell, PMS Monteiro, MH Costa… - Climate change 2021 …, 2023 - cambridge.org
It is unequivocal that the increases in atmospheric carbon dioxide (CO2), methane (CH4)
and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …

Global carbon budget 2023

P Friedlingstein, M O'sullivan, MW Jones… - Earth System …, 2023 - essd.copernicus.org
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their
redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate …

Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models

VK Arora, A Katavouta, RG Williams… - Biogeosciences …, 2019 - bg.copernicus.org
Results from the fully-, biogeochemically-, and radiatively-coupled simulations in which CO
2 increases at a rate of 1% per year (1pctCO2) from its pre-industrial value are analyzed to …

[HTML][HTML] Is there warming in the pipeline? A multi-model analysis of the Zero Emissions Commitment from

AH MacDougall, TL Frölicher, CD Jones… - …, 2020 - bg.copernicus.org
Abstract The Zero Emissions Commitment (ZEC) is the change in global mean temperature
expected to occur following the cessation of net CO 2 emissions and as such is a critical …

[PDF][PDF] JSBACH 3-The land component of the MPI Earth System Model: documentation of version 3.2

CH Reick, V Gayler, D Goll, S Hagemann, M Heidkamp… - 2021 - pure.mpg.de
JSBACH is the land component of the atmospheric component ECHAM [55], and thereby
part of the Max Planck Institute Earth System Model (MPI-ESM)[89]. Historically, JSBACH …

Climate factors determine the utilization strategy of forest plant resources at large scales

J Wang, X Wang, Y Ji, J Gao - Frontiers in Plant Science, 2022 - frontiersin.org
Plant functional traits are a representation of plant resource utilization strategies. Plants with
higher specific leaf area (SLA) and lower leaf dry matter content (LDMC) exhibit faster …

[HTML][HTML] Evaluation of soil carbon simulation in CMIP6 Earth system models

RM Varney, SE Chadburn, EJ Burke, PM Cox - Biogeosciences, 2022 - bg.copernicus.org
The response of soil carbon represents one of the key uncertainties in future climate change.
The ability of Earth system models (ESMs) to simulate present-day soil carbon is therefore …

[HTML][HTML] Nitrogen cycling in CMIP6 land surface models: progress and limitations

T Davies-Barnard, J Meyerholt, S Zaehle… - …, 2020 - bg.copernicus.org
The nitrogen cycle and its effect on carbon uptake in the terrestrial biosphere is a recent
progression in earth system models. As with any new component of a model, it is important …

[HTML][HTML] Global soil organic carbon removal by water erosion under climate change and land use change during AD 1850–2005

V Naipal, P Ciais, Y Wang, R Lauerwald… - …, 2018 - bg.copernicus.org
Erosion is an Earth system process that transports carbon laterally across the land surface
and is currently accelerated by anthropogenic activities. Anthropogenic land cover change …

Accounting for carbon and nitrogen interactions in the global terrestrial ecosystem model ORCHIDEE (trunk version, rev 4999): Multi-scale evaluation of gross primary …

N Vuichard, P Messina, S Luyssaert… - Geoscientific Model …, 2019 - gmd.copernicus.org
Nitrogen is an essential element controlling ecosystem carbon (C) productivity and its
response to climate change and atmospheric [CO2] increase. This study presents the …