Holocene thermal maximum mode versus the continuous warming mode: Problems of data-model comparisons and future research prospects-Reference-Cited by-同舟云学术

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Holocene thermal maximum mode versus the continuous warming mode: Problems of data-model comparisons and future research prospects

Published:2023-06-12 Issue:8 Volume:66 Page:1683-1701
ISSN:1674-7313
Container-title:Science China Earth Sciences
language:en
Short-container-title:Sci. China Earth Sci.

Author:

Chen Fahu,Duan Yanwu,Hao Shuo,Chen Jie,Feng Xiaoping,Hou Juzhi,Cao Xianyong,Zhang Xu,Zhou Tianjun

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s11430-022-1113-x.pdf

Reference151 articles.

1. Affolter S, Häuselmann A, Fleitmann D, Edwards R L, Cheng H, Leuenberger M. 2019. Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years. Sci Adv, 5: Eaav3809

2. Andersson C, Pausata F S R, Jansen E, Risebrobakken B, Telford R J. 2010. Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean. Clim Past, 6: 179–193

3. Bader J, Jungclaus J, Krivova N, Lorenz S, Maycock A, Raddatz T, Schmidt H, Toohey M, Wu C J, Claussen M. 2020. Global temperature modes shed light on the Holocene temperature conundrum. Nat Commun, 11: 4726

4. Baker J L, Lachniet M S, Chervyatsova O, Asmerom Y, Polyak V J. 2017. Holocene warming in western continental Eurasia driven by glacial retreat and greenhouse forcing. Nat Geosci, 10: 430–435

5. Banerjee A, Yeung L Y, Murray L T, Tie X, Tierney J E, Legrande A N. 2022. Clumped-isotope constraint on upper-tropospheric cooling during the Last Glacial Maximum. AGU Adv, 3: E2022AV000688

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