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 …
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 …
Abstract The Last Interglacial period, Marine Isotope Stage 5e (MIS 5e∼ 116–128 ka), is thought to have had a warmer, but less stable climate than the present interglacial. One key …
Z An, W Zhou, Z Zhang, X Zhang, Z Liu, Y Sun… - Science, 2024 - science.org
Despite extensive investigation, the nature and causes of the Mid-Pleistocene Transition remain enigmatic. In this work, we assess its linkage to asynchronous development of …
Two decades into the 21st century there is growing evidence for global impacts of Antarctic and Southern Ocean climate change. Reliable estimates of how the Antarctic climate system …
Sea level and deep-sea temperature variations are key indicators of global climate changes. For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O …
Polar temperatures during the Last Interglacial [LIG;~ 129 to 116 thousand years (ka)] were warmer than today, making this time period an important testing ground to better understand …
The future response of the Antarctic ice sheet to rising temperatures remains highly uncertain. A useful period for assessing the sensitivity of Antarctica to warming is the Last …
Warmer temperatures than today, over a period spanning millennia, most recently occurred in the Last Interglacial period, about 129,000 to 116,000 years ago. Yet, the timing and …