Palmer, T.N. and Williams, P. D. ORCID: https://orcid.org/0000-0002-9713-9820
(2008)
Introduction. Stochastic physics and climate modelling.
Philosophical Transactions of the Royal Society. Part A, 366 (1875).
pp. 2421-2427.
ISSN 1364-503X
doi: 10.1098/rsta.2008.0059
Abstract/Summary
Finite computing resources limit the spatial resolution of state-of-the-art global climate simulations to hundreds of kilometres. In neither the atmosphere nor the ocean are small-scale processes such as convection, clouds and ocean eddies properly represented. Climate simulations are known to depend, sometimes quite strongly, on the resulting bulk-formula representation of unresolved processes. Stochastic physics schemes within weather and climate models have the potential to represent the dynamical effects of unresolved scales in ways which conventional bulk-formula representations are incapable of so doing. The application of stochastic physics to climate modelling is a rapidly advancing, important and innovative topic. The latest research findings are gathered together in the Theme Issue for which this paper serves as the introduction.
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Item Type | Article |
URI | https://reading-clone.eprints-hosting.org/id/eprint/1357 |
Item Type | Article |
Refereed | Yes |
Divisions | Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology |
Uncontrolled Keywords | climate modelling; stochastic physics; parametrization |
Publisher | The Royal Society |
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