Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records
Using Pacific benthic foraminiferal δ18O and Mg/Ca records, we derive a Cenozoic (66 Ma)
global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene …
global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene …
The Anthropocene is functionally and stratigraphically distinct from the Holocene
BACKGROUND Humans are altering the planet, including long-term global geologic
processes, at an increasing rate. Any formal recognition of an Anthropocene epoch in the …
processes, at an increasing rate. Any formal recognition of an Anthropocene epoch in the …
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 …
Global and regional sea level rise scenarios for the United States
WV Sweet, RE Kopp, CP Weaver, J Obeysekera… - 2017 - ntrs.nasa.gov
The Sea Level Rise and Coastal Flood Hazard Scenarios and Tools Interagency Task
Force, jointly convened by the US Global Change Research Program (USGCRP) and the …
Force, jointly convened by the US Global Change Research Program (USGCRP) and the …
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
The major cause of sea-level change during ice ages is the exchange of water between ice
and ocean and the planet's dynamic response to the changing surface load. Inversion of∼ …
and ocean and the planet's dynamic response to the changing surface load. Inversion of∼ …
Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 C global warming could be dangerous
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 …
the effect of growing ice melt from Antarctica and Greenland. Meltwater tends to stabilize the …
Sea-level rise due to polar ice-sheet mass loss during past warm periods
BACKGROUND Although thermal expansion of seawater and melting of mountain glaciers
have dominated global mean sea level (GMSL) rise over the last century, mass loss from the …
have dominated global mean sea level (GMSL) rise over the last century, mass loss from the …
[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Sea-level variability over five glacial cycles
Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …
[HTML][HTML] Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review
This article reviews key data and debates focused on relative sea-level changes since the
Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and …
Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and …