Poleward expansion of tropical cyclone latitudes in warming climates
Tropical cyclones (TCs, also known as hurricanes and typhoons) generally form at low
latitudes with access to the warm waters of the tropical oceans, but far enough off the …
latitudes with access to the warm waters of the tropical oceans, but far enough off the …
Evolution of Earth's tectonic carbon conveyor belt
Concealed deep beneath the oceans is a carbon conveyor belt, propelled by plate tectonics.
Our understanding of its modern functioning is underpinned by direct observations, but its …
Our understanding of its modern functioning is underpinned by direct observations, but its …
Changing state of the climate system
SK Gulev, PW Thorne, J Ahn, FJ Dentener… - 2021 - centaur.reading.ac.uk
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 …
Human influence on the climate system (Chapter 3)
V Eyring, NP Gillett, KM Achuta Rao, R Barimalala… - 2021 - pure.iiasa.ac.at
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 …
A 485-million-year history of Earth's surface temperature
A long-term record of global mean surface temperature (GMST) provides critical insight into
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
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 …
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 …
Past climates inform our future
BACKGROUND Anthropogenic emissions are rapidly altering Earth's climate, pushing it
toward a warmer state for which there is no historical precedent. Although no perfect analog …
toward a warmer state for which there is no historical precedent. Although no perfect analog …
Simulating miocene warmth: insights from an opportunistic multi‐model ensemble (MioMIP1)
Abstract The Miocene epoch, spanning 23.03–5.33 Ma, was a dynamic climate of sustained,
polar amplified warmth. Miocene atmospheric CO2 concentrations are typically …
polar amplified warmth. Miocene atmospheric CO2 concentrations are typically …