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 …
Tropical teleconnection impacts on Antarctic climate changes
Over the modern satellite era, substantial climatic changes have been observed in the
Antarctic, including atmospheric and oceanic warming, ice sheet thinning and a general …
Antarctic, including atmospheric and oceanic warming, ice sheet thinning and a general …
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 …
Ice velocity and thickness of the world's glaciers
The effect of climate change on water resources and sea-level rise is largely determined by
the size of the ice reservoirs around the world and the ice thickness distribution, which …
the size of the ice reservoirs around the world and the ice thickness distribution, which …
The Paris Climate Agreement and future sea-level rise from Antarctica
Abstract The Paris Agreement aims to limit global mean warming in the twenty-first century to
less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit …
less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit …
[HTML][HTML] Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
Ocean-driven melting of floating ice-shelves in the Amundsen Sea is currently the main
process controlling Antarctica's contribution to sea-level rise. Using a regional ocean model …
process controlling Antarctica's contribution to sea-level rise. Using a regional ocean model …
Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes
Quantifying changes in Earth's ice sheets and identifying the climate drivers are central to
improving sea level projections. We provide unified estimates of grounded and floating ice …
improving sea level projections. We provide unified estimates of grounded and floating ice …
Interannual variations in meltwater input to the Southern Ocean from Antarctic ice shelves
Ocean-driven basal melting of Antarctica's floating ice shelves accounts for about half of
their mass loss in steady state, where gains in ice-shelf mass are balanced by losses. Ice …
their mass loss in steady state, where gains in ice-shelf mass are balanced by losses. Ice …
Future emergence of new ecosystems caused by glacial retreat
Glacier shrinkage and the development of post-glacial ecosystems related to anthropogenic
climate change are some of the fastest ongoing ecosystem shifts, with marked ecological …
climate change are some of the fastest ongoing ecosystem shifts, with marked ecological …
Response of the East Antarctic Ice Sheet to past and future climate change
Abstract The East Antarctic Ice Sheet contains the vast majority of Earth's glacier ice (about
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …