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Akademický článek

The role of atmospheric CO2 in controlling sea surface temperature change during the Pliocene

Autor: L. E. Burton, A. M. Haywood, J. C. Tindall, A. M. Dolan, D. J. Hill, E. L. McClymont, S. L. Ho, H. L. Ford

Publikováno v: Climate of the Past, Vol 20, Pp 1177-1194 (2024)

We present the role of CO2 forcing in controlling Late Pliocene sea surface temperature (SST) change using six models from Phase 2 of the Pliocene Model Intercomparison Project (PlioMIP2) and palaeoclimate proxy data from the PlioVAR working group. A

Externí odkaz: https://doaj.org/article/bbda1dfe238e40bdb3788ad4ce544ed4

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Akademický článek

On the climatic influence of CO2 forcing in the Pliocene

Autor: L. E. Burton, A. M. Haywood, J. C. Tindall, A. M. Dolan, D. J. Hill, A. Abe-Ouchi, W.-L. Chan, D. Chandan, R. Feng, S. J. Hunter, X. Li, W. R. Peltier, N. Tan, C. Stepanek, Z. Zhang

Publikováno v: Climate of the Past, Vol 19, Pp 747-764 (2023)

Understanding the dominant climate forcings in the Pliocene is crucial to assessing the usefulness of the Pliocene as an analogue for our warmer future. Here, we implement a novel yet simple linear factorisation method to assess the relative influenc

Externí odkaz: https://doaj.org/article/b2b940e11d494abcab1122986d68ab33

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Akademický článek

The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity

Publikováno v: Climate of the Past, Vol 16, Pp 2095-2123 (2020)

The Pliocene epoch has great potential to improve our understanding of the long-term climatic and environmental consequences of an atmospheric CO2 concentration near ∼400 parts per million by volume. Here we present the large-scale features of Plio

Externí odkaz: https://doaj.org/article/e324750e9a7743cc94547358d398759f

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Akademický článek

Modelling ice sheet evolution and atmospheric CO2 during the Late Pliocene

Autor: C. J. Berends, B. de Boer, A. M. Dolan, D. J. Hill, R. S. W. van de Wal

Publikováno v: Climate of the Past, Vol 15, Pp 1603-1619 (2019)

In order to investigate the relation between ice sheets and climate in a warmer-than-present world, recent research has focussed on the Late Pliocene, 3.6 to 2.58 million years ago. It is the most recent period in Earth's history when such a warm cli

Externí odkaz: https://doaj.org/article/c8707378aeb64464bf43520f8a2de81b

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Akademický článek

Using results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period

Publikováno v: Climate of the Past, Vol 11, Iss 3, Pp 403-424 (2015)

During an interval of the Late Pliocene, referred to here as the mid-Pliocene Warm Period (mPWP; 3.264 to 3.025 million years ago), global mean temperature was similar to that predicted for the end of this century, and atmospheric carbon dioxide conc

Externí odkaz: https://doaj.org/article/f71a08cb5b1e449a86c181372f2564ad

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Akademický článek

Ice sheet model dependency of the simulated Greenland Ice Sheet in the mid-Pliocene

Autor: S. J. Koenig, A. M. Dolan, B. de Boer, E. J. Stone, D. J. Hill, R. M. DeConto, A. Abe-Ouchi, D. J. Lunt, D. Pollard, A. Quiquet, F. Saito, J. Savage, R. van de Wal

Publikováno v: Climate of the Past, Vol 11, Iss 3, Pp 369-381 (2015)

The understanding of the nature and behavior of ice sheets in past warm periods is important for constraining the potential impacts of future climate change. The Pliocene warm period (between 3.264 and 3.025 Ma) saw global temperatures similar to tho

Externí odkaz: https://doaj.org/article/1b0ab5fbe5944159bc64d66acb035ddc

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Akademický článek

Evaluating the dominant components of warming in Pliocene climate simulations

Autor: D. J. Hill, A. M. Haywood, D. J. Lunt, S. J. Hunter, F. J. Bragg, C. Contoux, C. Stepanek, L. Sohl, N. A. Rosenbloom, W.-L. Chan, Y. Kamae, Z. Zhang, A. Abe-Ouchi, M. A. Chandler, A. Jost, G. Lohmann, B. L. Otto-Bliesner, G. Ramstein, H. Ueda

Publikováno v: Climate of the Past, Vol 10, Iss 1, Pp 79-90 (2014)

The Pliocene Model Intercomparison Project (PlioMIP) is the first coordinated climate model comparison for a warmer palaeoclimate with atmospheric CO2 significantly higher than pre-industrial concentrations. The simulations of the mid-Pliocene warm p

Externí odkaz: https://doaj.org/article/1795f1a57cf74b1cad8d9859c6c9b6e9

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Akademický článek

Mid-Pliocene East Asian monsoon climate simulated in the PlioMIP

Publikováno v: Climate of the Past, Vol 9, Iss 5, Pp 2085-2099 (2013)

Based on simulations with 15 climate models in the Pliocene Model Intercomparison Project (PlioMIP), the regional climate of East Asia (focusing on China) during the mid-Pliocene is investigated in this study. Compared to the pre-industrial, the mult

Externí odkaz: https://doaj.org/article/560529a63d664c18a5c90e46d4011808

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Akademický článek

Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

Publikováno v: Climate of the Past, Vol 9, Iss 4, Pp 1495-1504 (2013)

In the Pliocene Model Intercomparison Project (PlioMIP), eight state-of-the-art coupled climate models have simulated the mid-Pliocene warm period (mPWP, 3.264 to 3.025 Ma). Here, we compare the Atlantic Meridional Overturning Circulation (AMOC), nor

Externí odkaz: https://doaj.org/article/a866fcbeeaa44094a7f644bf2f0d5b9b

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Akademický článek

Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project

Publikováno v: Climate of the Past, Vol 9, Iss 1, Pp 191-209 (2013)

Climate and environments of the mid-Pliocene warm period (3.264 to 3.025 Ma) have been extensively studied. Whilst numerical models have shed light on the nature of climate at the time, uncertainties in their predictions have not been systematically

Externí odkaz: https://doaj.org/article/5c2efbb083264877b3c4560f06aecdf9

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