[HTML][HTML] Climate change: Strategies for mitigation and adaptation
The sustainability of life on Earth is under increasing threat due to human-induced climate
change. This perilous change in the Earth's climate is caused by increases in carbon dioxide …
change. This perilous change in the Earth's climate is caused by increases in carbon dioxide …
The Miocene: The future of the past
Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …
to today. Continental configurations and mountain topography transitioned toward modern …
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 …
An astronomically dated record of Earth's climate and its predictability over the last 66 million years
Much of our understanding of Earth's past climate comes from the measurement of oxygen
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
Human influence on the climate system (Chapter 3)
The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …
Framing, Context, and Methods (Chapter 1)
Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …
the current evidence on the physical science of climate change, evaluating knowledge …
Spatial patterns of climate change across the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM; 56 Ma) is one of our best geological
analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
[HTML][HTML] The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons
Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a geologically rapid
warming period associated with carbon release, which caused a marked increase in the …
warming period associated with carbon release, which caused a marked increase in the …
Global mean surface temperature and climate sensitivity of the EECO, PETM and latest Paleocene
Accurate estimates of past global mean surface temperature (GMST) help to contextualise
future climate change and are required to estimate the sensitivity of the climate system to …
future climate change and are required to estimate the sensitivity of the climate system to …