Zobrazeno 1 - 10
of 50
pro vyhledávání: '"S. Liddicoat"'
Autor:
A. Asaadi, J. Schwinger, H. Lee, J. Tjiputra, V. Arora, R. Séférian, S. Liddicoat, T. Hajima, Y. Santana-Falcón, C. D. Jones
Publikováno v:
Biogeosciences, Vol 21, Pp 411-435 (2024)
Limiting global warming to well below 2 ∘C by the end of the century is an ambitious target that requires immediate and unprecedented emission reductions. In the absence of sufficient near-term mitigation, this target will only be achieved by carbo
Externí odkaz:
https://doaj.org/article/978a35344349491fa7ca25bfefa70019
Autor:
L. de Mora, R. Swaminathan, R. P. Allan, J. C. Blackford, D. I. Kelley, P. Harris, C. D. Jones, C. G. Jones, S. Liddicoat, R. J. Parker, T. Quaife, J. Walton, A. Yool
Publikováno v:
Earth System Dynamics, Vol 14, Pp 1295-1315 (2023)
We show that the distribution of anthropogenic carbon between the atmosphere, land surface, and ocean differs with the choice of projection scenario even for identical changes in mean global surface temperature. Warming thresholds occur later in lowe
Externí odkaz:
https://doaj.org/article/e81517977d1c475499fbc357807413a2
Autor:
A. J. Wiltshire, E. J. Burke, S. E. Chadburn, C. D. Jones, P. M. Cox, T. Davies-Barnard, P. Friedlingstein, A. B. Harper, S. Liddicoat, S. Sitch, S. Zaehle
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 2161-2186 (2021)
Understanding future changes in the terrestrial carbon cycle is important for reliable projections of climate change and impacts on ecosystems. It is well known that nitrogen (N) could limit plants' response to increased atmospheric carbon dioxide an
Externí odkaz:
https://doaj.org/article/4a5d2b025e2243b7b5138eb379cba448
Autor:
L. R. Boysen, V. Brovkin, J. Pongratz, D. M. Lawrence, P. Lawrence, N. Vuichard, P. Peylin, S. Liddicoat, T. Hajima, Y. Zhang, M. Rocher, C. Delire, R. Séférian, V. K. Arora, L. Nieradzik, P. Anthoni, W. Thiery, M. M. Laguë, D. Lawrence, M.-H. Lo
Publikováno v:
Biogeosciences, Vol 17, Pp 5615-5638 (2020)
Changes in forest cover have a strong effect on climate through the alteration of surface biogeophysical and biogeochemical properties that affect energy, water and carbon exchange with the atmosphere. To quantify biogeophysical and biogeochemical ef
Externí odkaz:
https://doaj.org/article/ed475938e6ac42679d62c6d99ea83c14
Autor:
W. J. Collins, N. Bellouin, M. Doutriaux-Boucher, N. Gedney, P. Halloran, T. Hinton, J. Hughes, C. D. Jones, M. Joshi, S. Liddicoat, G. Martin, F. O'Connor, J. Rae, C. Senior, S. Sitch, I. Totterdell, A. Wiltshire, S. Woodward
Publikováno v:
Geoscientific Model Development, Vol 4, Iss 4, Pp 1051-1075 (2011)
We describe here the development and evaluation of an Earth system model suitable for centennial-scale climate prediction. The principal new components added to the physical climate model are the terrestrial and ocean ecosystems and gas-phase troposp
Externí odkaz:
https://doaj.org/article/2ac5b81199c44f5aa7ac94b16e9939c7
Autor:
The HadGEM2 Development Team: G. M. Martin, N. Bellouin, W. J. Collins, I. D. Culverwell, P. R. Halloran, S. C. Hardiman, T. J. Hinton, C. D. Jones, R. E. McDonald, A. J. McLaren, F. M. O'Connor, M. J. Roberts, J. M. Rodriguez, S. Woodward, M. J. Best, M. E. Brooks, A. R. Brown, N. Butchart, C. Dearden, S. H. Derbyshire, I. Dharssi, M. Doutriaux-Boucher, J. M. Edwards, P. D. Falloon, N. Gedney, L. J. Gray, H. T. Hewitt, M. Hobson, M. R. Huddleston, J. Hughes, S. Ineson, W. J. Ingram, P. M. James, T. C. Johns, C. E. Johnson, A. Jones, C. P. Jones, M. M. Joshi, A. B. Keen, S. Liddicoat, A. P. Lock, A. V. Maidens, J. C. Manners, S. F. Milton, J. G. L. Rae, J. K. Ridley, A. Sellar, C. A. Senior, I. J. Totterdell, A. Verhoef, P. L. Vidale, A. Wiltshire
Publikováno v:
Geoscientific Model Development, Vol 4, Iss 3, Pp 723-757 (2011)
We describe the HadGEM2 family of climate configurations of the Met Office Unified Model, MetUM. The concept of a model "family" comprises a range of specific model configurations incorporating different levels of complexity but with a common physica
Externí odkaz:
https://doaj.org/article/e575b09f408c4694b359c9f73b017798
Autor:
C. D. Jones, J. K. Hughes, N. Bellouin, S. C. Hardiman, G. S. Jones, J. Knight, S. Liddicoat, F. M. O'Connor, R. J. Andres, C. Bell, K.-O. Boo, A. Bozzo, N. Butchart, P. Cadule, K. D. Corbin, M. Doutriaux-Boucher, P. Friedlingstein, J. Gornall, L. Gray, P. R. Halloran, G. Hurtt, W. J. Ingram, J.-F. Lamarque, R. M. Law, M. Meinshausen, S. Osprey, E. J. Palin, L. Parsons Chini, T. Raddatz, M. G. Sanderson, A. A. Sellar, A. Schurer, P. Valdes, N. Wood, S. Woodward, M. Yoshioka, M. Zerroukat
Publikováno v:
Geoscientific Model Development, Vol 4, Iss 3, Pp 543-570 (2011)
The scientific understanding of the Earth's climate system, including the central question of how the climate system is likely to respond to human-induced perturbations, is comprehensively captured in GCMs and Earth System Models (ESM). Diagnosing th
Externí odkaz:
https://doaj.org/article/6a5fd3067ed14c24a14a0a013e7f8b3b
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