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Climate Change 2021—The Physical Science Basis
The Intergovernmental Panel on Climate Change (IPCC) is the United Nations body responsible for assessing the science related to climate change. The Sixth Report from IPCC Working Group 1 publishedExpand
Global climate projections
Mid- to Late Holocene climate change: an overview
The last 6000 years are of particular interest to the understanding of the Earth System because the boundary conditions of the climate system did not change dramatically (in comparison to largerExpand
High-resolution carbon dioxide concentration record 650,000–800,000 years before present
It is found that atmospheric carbon dioxide is strongly correlated with Antarctic temperature throughout eight glacial cycles but with significantly lower concentrations between 650,000 and 750,000 yr before present, which extends the pre-industrial range of carbon dioxide concentrations during the late Quaternary by about 10 p.p.m.v. Expand
Atmospheric CO2 concentrations over the last glacial termination.
The similarity of changes in CO2 concentration and variations of atmospheric methane concentration suggests that processes in the tropics and in the Northern Hemisphere, where the main sources for methane are located, also had substantial effects on atmospheric CO2 concentrations. Expand
Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years
It is suggested that the interplay between obliquity and precession accounts for the variable intensity of interglacial periods in ice core records. Expand
Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica
A high-resolution ice-core record of atmospheric CO2 concentration over the Holocene epoch shows that the global carbon cycle has not been in steady state during the past 11,000 years. Analysis ofExpand
Asynchrony of Antarctic and Greenland climate change during the last glacial period
A central issue in climate dynamics is to understand how the Northern and Southern hemispheres are coupled during climate events. The strongest of the fast temperature changes observed in GreenlandExpand
Spatiotemporal patterns of carbon‐13 in the global surface oceans and the oceanic suess effect
A global synthesis of the 13C/12C ratio of dissolved inorganic carbon (DIC) in the surface ocean is attempted by summarizing high-precision data obtained from 1978 to 1997 in all major ocean basins.Expand