Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Aisling M. Dolan"'
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-12 (2018)
Ice sheet models forced by climate model output indicate ice-sheet retreat during the Pliocene, yet concerns remain regarding potential model bias. Here, the authors present results from the Pliocene Ice-sheet Modelling Intercomparison Project, and s
Externí odkaz:
https://doaj.org/article/bfcd611b699a444fad011f467d9cf76c
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-14 (2016)
Abstract The mid-Pliocene Warm Period (mPWP) offers an opportunity to understand a warmer-than-present world and assess the predictive ability of numerical climate models. Environmental reconstruction and climate modelling are crucial for understandi
Externí odkaz:
https://doaj.org/article/85be2605900241bd8ed70f70a69e8b17
Autor:
Lauren E. Burton, Alan M. Haywood, Julia C. Tindall, Aisling M. Dolan, Daniel J. Hill, Ayako Abe-Ouchi, Wing-Le Chan, Deepak Chandan, Ran Feng, Stephen J. Hunter, Xiangyu Li, W. Richard Peltier, Ning Tan, Christian Stepanek, Zhongshi Zhang
Publikováno v:
EPIC3Climate of the Past, Copernicus GmbH, 19(3), pp. 747-764, ISSN: 1814-9324
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa6a269aa94f9419c89f5eab34adc9a8
https://cp.copernicus.org/articles/19/747/2023/
https://cp.copernicus.org/articles/19/747/2023/
Reconciling palaeodata with model simulations of the Pliocene climate is essential for understanding a world with atmospheric CO2 concentration near 400 ppmv (parts per million by volume). Both models and data indicate an amplified warming of the hig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::49326e52531780d11307a25b2835ec81
https://cp.copernicus.org/articles/18/1385/2022/
https://cp.copernicus.org/articles/18/1385/2022/
Reconciling palaeodata with model simulations of the Pliocene climate is essential for understanding a world with atmospheric CO2 concentration near 400 parts per million by volume. Both models and data indicate an amplified warming of the high latit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::441c151491fd14892e2bfedfea9cdae1
https://cp.copernicus.org/preprints/cp-2021-186/
https://cp.copernicus.org/preprints/cp-2021-186/
Autor:
A. R. Lewis, H. Chorley, Ross D. Powell, Fabio Florindo, Francesca Sangiorgi, Richard H. Levy, Christian Ohneiser, Trevor Williams, Laura De Santis, Molly O. Patterson, Tina van de Flierdt, Warren W. Dickinson, Nicholas R. Golledge, Carlota Escutia, Lara F. Pérez, Anna Ruth W. Halberstadt, David M. Harwood, Tim R Naish, Robert M. McKay, Edward Gasson, Aisling M. Dolan, Georgia R. Grant, Amelia E. Shevenell, Stephen R. Meyers, D. E. Kowalewski, Marjolaine Verret
Publikováno v:
Antarctic Climate Evolution ISBN: 9780128191095
The Miocene to Pliocene (Neogene) occurred between 23.04 and 2.58 million years ago and includes intervals of peak global warmth where Earth’s average surface temperature was up to 8℃ warmer than present. Major cooling steps also occurred, across
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca164b651c752f654245fc60315ca844
https://doi.org/10.1016/b978-0-12-819109-5.00014-1
https://doi.org/10.1016/b978-0-12-819109-5.00014-1
Publikováno v:
Climate of the Past, Vol 15, Pp 1691-1713 (2019)
We present the UK's input into the Pliocene Model Intercomparison Project phase 2 (PlioMIP2) using the Hadley Centre Climate Model version 3 (HadCM3). The 400 ppm CO2 Pliocene experiment has a mean annual surface air temperature that is 2.9 ∘C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6584fe7333b03f80199d7a020d6bc3ef
https://www.clim-past.net/15/1691/2019/cp-15-1691-2019.pdf
https://www.clim-past.net/15/1691/2019/cp-15-1691-2019.pdf
Autor:
Constantijn J. Berends, Daniel J. Hill, Roderik S. W. van de Wal, Aisling M. Dolan, Bas de Boer
Publikováno v:
Climate of the Past. 15:1603-1619
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0907a63ce586d214f670e578b9bd776
https://doi.org/10.5194/cp-15-1603-2019
https://doi.org/10.5194/cp-15-1603-2019
Modelling results from PlioMIP2 (the Pliocene Model Intercomparison Project Phase 2) focussing on MIS KM5c; ~3.205Ma, suggest that global mean surface air temperature was 1.7 – 5.2 °C higher than the preindustrial. This warming was amplified at th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a00c20feec58e481dbc09e09fa1df3b
https://doi.org/10.5194/egusphere-egu21-4802
https://doi.org/10.5194/egusphere-egu21-4802