Intergovernmental Panel on Climate Change (IPCC). Global carbon and other biogeochemical cycles and feedbacks
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 …
and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …
Climatic evolution in the Australian region over the last 94 ka-spanning human occupancy-, and unveiling the Last Glacial Maximum
P De Deckker, M Moros, K Perner, T Blanz… - Quaternary Science …, 2020 - Elsevier
The Quaternary is well known for being a period of the geological record that saw significant
and alternating climatic fluctuations. Here, we concentrate on the last 94 millennia that saw …
and alternating climatic fluctuations. Here, we concentrate on the last 94 millennia that saw …
Southern Ocean glacial conditions and their influence on deglacial events
Abstract The Southern Ocean is an important regulator of global CO2 levels and likely had a
key role in lowering atmospheric CO2 levels during the Last Glacial Maximum (LGM) and …
key role in lowering atmospheric CO2 levels during the Last Glacial Maximum (LGM) and …
Direct astronomical influence on abrupt climate variability
Abstract Changes in the magnitude of millennial-scale climate variability (MCV) during the
Late Pleistocene occur as a function of changing background climate state over tens of …
Late Pleistocene occur as a function of changing background climate state over tens of …
Abrupt changes in the global carbon cycle during the last glacial period
During the last glacial period, atmospheric carbon dioxide (CO2) closely followed Antarctic
temperature on millennial timescales. This strong correlation between Antarctic climate and …
temperature on millennial timescales. This strong correlation between Antarctic climate and …
[HTML][HTML] LongRunMIP: motivation and design for a large collection of millennial-length AOGCM simulations
LongRunMIP: Motivation and Design for a Large Collection of Millennial-Length AOGCM
Simulations in: Bulletin of the American Meteorological Society Volume 100 Issue 12 (2019) …
Simulations in: Bulletin of the American Meteorological Society Volume 100 Issue 12 (2019) …
Millennial atmospheric CO2 changes linked to ocean ventilation modes over past 150,000 years
Ice core measurements show diverse atmospheric CO2 variations—increasing, decreasing
or remaining stable—during millennial-scale North Atlantic cold periods called stadials. The …
or remaining stable—during millennial-scale North Atlantic cold periods called stadials. The …
Southern Ocean drives multidecadal atmospheric CO2 rise during Heinrich Stadials
KA Wendt, C Nehrbass-Ahles… - Proceedings of the …, 2024 - National Acad Sciences
The last glacial period was punctuated by cold intervals in the North Atlantic region that
culminated in extensive iceberg discharge events. These cold intervals, known as Heinrich …
culminated in extensive iceberg discharge events. These cold intervals, known as Heinrich …
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4
Here we use high-precision carbon isotope data (δ13C-CO2) to show atmospheric CO2
during Marine Isotope Stage 4 (MIS 4,~ 70.5-59 ka) was controlled by a succession of …
during Marine Isotope Stage 4 (MIS 4,~ 70.5-59 ka) was controlled by a succession of …
[HTML][HTML] Rejuvenating the ocean: mean ocean radiocarbon, CO2 release, and radiocarbon budget closure across the last deglaciation
Radiocarbon is a tracer that provides unique insights into the ocean's ability to sequester CO
2 from the atmosphere. While spatial patterns of radiocarbon in the ocean interior can …
2 from the atmosphere. While spatial patterns of radiocarbon in the ocean interior can …