Determining the rates, mechanisms, and geographic variability of relative sea-level (RSL)
change following the Last Glacial Maximum (LGM) provides insight into the sensitivity of ice …

Ocean and coastal ecosystems support life on Earth and many aspects of human well-being.
Covering two-thirds of the planet, the ocean hosts vast biodiversity and modulates the global …

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 …

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 rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …

Sea-level rise is a significant indicator of broader climate changes, and the time of
emergence concept can be used to identify when modern rates of sea-level rise emerged …

Sea‐level rise sits at the frontier of usable climate climate change research, because it
involves natural and human systems with long lags, irreversible losses, and deep …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

Sea-level budgets account for the contributions of processes driving sea-level change, but
are predominantly focused on global-mean sea level and limited to the 20th and 21st …

Globally, mineral sediment supply to deltaic wetlands has generally decreased so these
wetlands increasingly rely on accretion of organic matter to keep pace with relative sea …