Changing state of the climate system
2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
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 …
Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments
Carbon is one of the key elements in organisms and non-living compounds on Earth.
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
[HTML][HTML] Climate forcing of regional deep-sea biodiversity documented by benthic foraminifera
The biodiversity of deep-sea ecosystems is closely linked to orbital and suborbital climate
changes during the late Quaternary as documented by the diversity and species …
changes during the late Quaternary as documented by the diversity and species …
Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age
No single mechanism can account for the full amplitude of past atmospheric carbon dioxide
(CO2) concentration variability over glacial–interglacial cycles. A build-up of carbon in the …
(CO2) concentration variability over glacial–interglacial cycles. A build-up of carbon in the …
Marine anoxia linked to abrupt global warming during Earth's penultimate icehouse
Piecing together the history of carbon (C) perturbation events throughout Earth's history has
provided key insights into how the Earth system responds to abrupt warming. Previous …
provided key insights into how the Earth system responds to abrupt warming. Previous …
Global reorganization of deep-sea circulation and carbon storage after the last ice age
Using new and published marine fossil radiocarbon (14C/C) measurements, a tracer
uniquely sensitive to circulation and air-sea gas exchange, we establish several …
uniquely sensitive to circulation and air-sea gas exchange, we establish several …
Anatomy of Heinrich Layer 1 and its role in the last deglaciation
X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …
Abrupt global-ocean anoxia during the Late Ordovician–early Silurian detected using uranium isotopes of marine carbonates
Widespread marine anoxia is hypothesized as the trigger for the second pulse of the Late
Ordovician (Hirnantian) mass extinction based on lithologic and geochemical proxies that …
Ordovician (Hirnantian) mass extinction based on lithologic and geochemical proxies that …
Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2
LC Skinner, F Primeau, E Freeman… - Nature …, 2017 - nature.com
While the ocean's large-scale overturning circulation is thought to have been significantly
different under the climatic conditions of the Last Glacial Maximum (LGM), the exact nature …
different under the climatic conditions of the Last Glacial Maximum (LGM), the exact nature …