Paleoclimate data assimilation: Comments on “A 485-million-year history of Earth’s surface temperature” DOI
Zhongshi Zhang, Yonggang Liu

Science China Earth Sciences, Journal Year: 2025, Volume and Issue: unknown

Published: April 14, 2025

Language: Английский

Cenozoic evolution of spring persistent rainfall in East Asia and North America driven by paleogeography DOI Creative Commons
Linqiang He, Tianjun Zhou, Zhun Guo

et al.

Communications Earth & Environment, Journal Year: 2025, Volume and Issue: 6(1)

Published: Feb. 27, 2025

Language: Английский

Citations

0

When were global temperatures as high as today? DOI
Ian Candy

Elsevier eBooks, Journal Year: 2025, Volume and Issue: unknown

Published: Jan. 1, 2025

Language: Английский

Citations

0

Eccentricity pacing of the Paleocene-Eocene thermal Maximum: Multi-section astrochronology and statistical insights in China DOI

Runjian Chu,

Huaichun Wu, Qiang Fang

et al.

Global and Planetary Change, Journal Year: 2025, Volume and Issue: unknown, P. 104800 - 104800

Published: March 1, 2025

Language: Английский

Citations

0

Tropical Atlantic Temperature and Hydrologic Change During the Paleocene‐Eocene Thermal Maximum DOI

Corey Storm Howard,

Donald E. Penman, Jiang Zhu

et al.

Paleoceanography and Paleoclimatology, Journal Year: 2025, Volume and Issue: 40(4)

Published: April 1, 2025

Abstract The Paleocene‐Eocene Thermal Maximum (PETM, ∼56 million years ago) is among the best‐studied climatic warming events in Earth history and often compared to projected anthropogenic climate change. PETM characterized by a rapid negative carbon isotope excursion global temperature increase of 4–5°C, accompanied changes spatial patterns evaporation precipitation hydrologic cycle. Recent model reconstructions suggest regionally complex non‐linear response one important aspect hydrology: enhanced moisture flux from low‐latitude ocean. In this study, we use elemental stable geochemistry surface‐dwelling planktic foraminifera Atlantic deep‐sea sedimentary record (IODP Site 1258) quantify sea‐surface (SST) salinity. Foraminiferal Mg/Ca δ 18 O values are interpreted with Bayesian forward proxy system reconstruct how SST salinity changed over at site. These then recent simulations Eocene warming. Our indicate °C warming, excellent agreement estimates other tropical locations modeled warmth. regional change not as straightforward, demonstrating slight decrease extreme p CO 2 forcing (a reversal sense under moderate forcing) both reconstructions. cause unclear but may relate increased South American continental runoff or shifts Inter‐Tropical Convergence Zone.

Language: Английский

Citations

0

Paleoclimate data assimilation: Comments on “A 485-million-year history of Earth’s surface temperature” DOI
Zhongshi Zhang, Yonggang Liu

Science China Earth Sciences, Journal Year: 2025, Volume and Issue: unknown

Published: April 14, 2025

Language: Английский

Citations

0