[HTML][HTML] The Antarctic contribution to 21st-century sea-level rise predicted by the UK Earth System Model with an interactive ice sheet

A Siahaan, RS Smith, PR Holland, A Jenkins… - The …, 2022 - tc.copernicus.org
Abstract The Antarctic Ice Sheet will play a crucial role in the evolution of global mean sea
level as the climate warms. An interactively coupled climate and ice sheet model is needed …

The PhanSST global database of Phanerozoic sea surface temperature proxy data

EJ Judd, JE Tierney, BT Huber, SL Wing, DJ Lunt… - Scientific Data, 2022 - nature.com
Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …

[HTML][HTML] Lipid-biomarker-based sea surface temperature record offshore Tasmania over the last 23 million years

S Hou, F Lamprou, FS Hoem, MRN Hadju… - Climate of the …, 2023 - cp.copernicus.org
Abstract The Neogene (23.04–2.58 Ma) is characterised by progressive buildup of ice
volume and climate cooling in the Antarctic and the Northern Hemisphere. Heat and …

[HTML][HTML] Southern Ocean bottom-water cooling and ice sheet expansion during the middle Miocene climate transition

TJ Leutert, S Modestou, SM Bernasconi… - Climate of the …, 2021 - cp.copernicus.org
The middle Miocene climate transition (MMCT), around 14 Ma, was associated with a
significant climatic shift, but the mechanisms triggering the event remain enigmatic. We …

[HTML][HTML] Atmospheric carbon dioxide variations across the middle Miocene climate transition

M Raitzsch, J Bijma, T Bickert, M Schulz… - Climate of the …, 2021 - cp.copernicus.org
The middle Miocene climate transition∼ 14 Ma marks a fundamental step towards the
current “ice-house” climate, with a∼ 1‰ δ 18 O increase and a∼ 1‰ transient δ 13 C rise in …

[HTML][HTML] Clumped isotopes in globally distributed Holocene coccoliths reveal their habitat depth

LM Mejía, SM Bernasconi, H Zhang, J Guitián… - Earth and Planetary …, 2023 - Elsevier
Reliable temperature reconstructions are necessary to improve climate reconstructions and
comparisons with paleoclimate model simulations. Most existing paleotemperature proxies …