Zobrazeno 1 - 10
of 191
pro vyhledávání: '"E J, Stone"'
Autor:
C. J. R. Williams, A. A. Sellar, X. Ren, A. M. Haywood, P. Hopcroft, S. J. Hunter, W. H. G. Roberts, R. S. Smith, E. J. Stone, J. C. Tindall, D. J. Lunt
Publikováno v:
Climate of the Past, Vol 17, Pp 2139-2163 (2021)
Here we present the experimental design and results from a new mid-Pliocene simulation using the latest version of the UK's physical climate model, HadGEM3-GC31-LL, conducted under the auspices of CMIP6/PMIP4/PlioMIP2. Although two other palaeoclimat
Externí odkaz:
https://doaj.org/article/54880e0e2032455abb1e5dd1c40fd15c
Autor:
P. J. Valdes, E. Armstrong, M. P. S. Badger, C. D. Bradshaw, F. Bragg, M. Crucifix, T. Davies-Barnard, J. J. Day, A. Farnsworth, C. Gordon, P. O. Hopcroft, A. T. Kennedy, N. S. Lord, D. J. Lunt, A. Marzocchi, L. M. Parry, V. Pope, W. H. G. Roberts, E. J. Stone, G. J. L. Tourte, J. H. T. Williams
Publikováno v:
Geoscientific Model Development, Vol 10, Pp 3715-3743 (2017)
Understanding natural and anthropogenic climate change processes involves using computational models that represent the main components of the Earth system: the atmosphere, ocean, sea ice, and land surface. These models have become increasingly co
Externí odkaz:
https://doaj.org/article/ffd93422f1584d69a0a51748b9ae3511
Publikováno v:
Climate of the Past, Vol 12, Iss 9, Pp 1919-1932 (2016)
Recent data compilations of the early Last Interglacial period have indicated a bipolar temperature response at 130 ka, with colder-than-present temperatures in the North Atlantic and warmer-than-present temperatures in the Southern Ocean and over An
Externí odkaz:
https://doaj.org/article/4cf4b7c2d1dc4f3ebe437bbfec3a1120
Autor:
A. Landais, V. Masson-Delmotte, E. Capron, P. M. Langebroek, P. Bakker, E. J. Stone, N. Merz, C. C. Raible, H. Fischer, A. Orsi, F. Prié, B. Vinther, D. Dahl-Jensen
Publikováno v:
Climate of the Past, Vol 12, Iss 9, Pp 1933-1948 (2016)
The last interglacial period (LIG, ∼ 129–116 thousand years ago) provides the most recent case study of multimillennial polar warming above the preindustrial level and a response of the Greenland and Antarctic ice sheets to this warming, as well
Externí odkaz:
https://doaj.org/article/2f23b461616d462481193acfe6fe777d
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
Publikováno v:
Geoscientific Model Development, Vol 6, Iss 5, Pp 1715-1728 (2013)
We measure the potential of an observational data set to constrain a set of inputs to a complex and computationally expensive computer model. We use each member in turn of an ensemble of output from a computationally expensive model, corresponding to
Externí odkaz:
https://doaj.org/article/5cd666f2ee4643ab87980efc88ac0eb6
Autor:
P. Bakker, E. J. Stone, S. Charbit, M. Gröger, U. Krebs-Kanzow, S. P. Ritz, V. Varma, V. Khon, D. J. Lunt, U. Mikolajewicz, M. Prange, H. Renssen, B. Schneider, M. Schulz
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 605-619 (2013)
There is a growing number of proxy-based reconstructions detailing the climatic changes that occurred during the last interglacial period (LIG). This period is of special interest, because large parts of the globe were characterized by a warmer-than-
Externí odkaz:
https://doaj.org/article/0760909349d3459d951754cb7d044559
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 621-639 (2013)
During the Last Interglacial period (~ 130–115 thousand years ago) the Arctic climate was warmer than today, and global mean sea level was probably more than 6.6 m higher. However, there are large discrepancies in the estimated contributions to thi
Externí odkaz:
https://doaj.org/article/d2425196aeb942dfa69e8d99116d3572
Autor:
D. J. Lunt, A. Abe-Ouchi, P. Bakker, A. Berger, P. Braconnot, S. Charbit, N. Fischer, N. Herold, J. H. Jungclaus, V. C. Khon, U. Krebs-Kanzow, P. M. Langebroek, G. Lohmann, K. H. Nisancioglu, B. L. Otto-Bliesner, W. Park, M. Pfeiffer, S. J. Phipps, M. Prange, R. Rachmayani, H. Renssen, N. Rosenbloom, B. Schneider, E. J. Stone, K. Takahashi, W. Wei, Q. Yin, Z. S. Zhang
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 699-717 (2013)
The last interglaciation (~130 to 116 ka) is a time period with a strong astronomically induced seasonal forcing of insolation compared to the present. Proxy records indicate a significantly different climate to that of the modern, in particular Arct
Externí odkaz:
https://doaj.org/article/b51afee21c4040bb8d52e7bef3598cf0
Publikováno v:
The Cryosphere, Vol 6, Iss 3, Pp 589-606 (2012)
Lack of knowledge about the values of ice sheet model input parameters introduces substantial uncertainty into projections of Greenland Ice Sheet contributions to future sea level rise. Computer models of ice sheet behavior provide one of several mea
Externí odkaz:
https://doaj.org/article/cfd74e0dece04a798b680866098b4c7a