Over the coming century humanity may need to find reservoirs to store several trillions of
tons of carbon dioxide (CO2) emitted from fossil fuel combustion, which would otherwise …

Global climate and the atmospheric partial pressure of carbon dioxide () are correlated over
recent glacial cycles, with lower during ice ages, but the causes of the changes are …

This latest Fifth Assessment Report of the Intergovernmental Panel on Climate Change
(IPCC) will again form the standard scientific reference for all those concerned with climate …

We use numerical climate simulations, paleoclimate data, and modern observations to study
the effect of growing ice melt from Antarctica and Greenland. Meltwater tends to stabilize the …

This chapter addresses the biogeochemical cycles of carbon dioxide (CO2), methane (CH4),
and nitrous oxide (N2O). The three greenhouse gases have increased in the atmosphere …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

230Th-dated oxygen isotope records of stalagmites from Sanbao Cave, China, characterize
Asian Monsoon (AM) precipitation through the ends of the third-and fourthmost recent ice …

Ocean Biogeochemical Dynamics provides a broad theoretical framework upon which
graduate students and upper-level undergraduates can formulate an understanding of the …

Wind-driven upwelling in the ocean around Antarctica helps regulate the exchange of
carbon dioxide (CO2) between the deep sea and the atmosphere, as well as the supply of …

The concentration of CO2 in the atmosphere has risen from close to 280 parts per million
(ppm) in 1800, at first slowly and then progressively faster to a value of 367 ppm in 1999 …