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dc.contributor.authorVallis, GK
dc.contributor.authorColyer, G
dc.contributor.authorGeen, R
dc.contributor.authorGerber, E
dc.contributor.authorJucker, M
dc.contributor.authorMaher, P
dc.contributor.authorPaterson, A
dc.contributor.authorPietschnig, M
dc.contributor.authorPenn, J
dc.contributor.authorThomson, SI
dc.date.accessioned2018-03-07T15:22:11Z
dc.date.issued2018-03-06
dc.description.abstractIsca is a framework for the idealized modelling of the global circulation of planetary atmospheres at varying levels of complexity and realism. The framework is an outgrowth of models from the Geophysical Fluid Dynamics Laboratory in Princeton, USA, designed for Earth's atmosphere, but it may readily be extended into other planetary regimes. Various forcing and radiation options are available, from dry, time invariant, Newtonian thermal relaxation to moist dynamics with radiative transfer. Options are available in the dry thermal relaxation scheme to account for the effects of obliquity and eccentricity (and so seasonality), different atmospheric optical depths and a surface mixed layer. An idealized grey radiation scheme, a two-band scheme, and a multiband scheme are also available, all with simple moist effects and astronomically based solar forcing. At the complex end of the spectrum the framework provides a direct connection to comprehensive atmospheric general circulation models. For Earth modelling, options include an aquaplanet and configurable continental outlines and topography. Continents may be defined by changing albedo, heat capacity, and evaporative parameters and/or by using a simple bucket hydrology model. Oceanic Q fluxes may be added to reproduce specified sea surface temperatures, with arbitrary continental distributions. Planetary atmospheres may be configured by changing planetary size and mass, solar forcing, atmospheric mass, radiation, and other parameters. Examples are given of various Earth configurations as well as a giant planet simulation, a slowly rotating terrestrial planet simulation, and tidally locked and other orbitally resonant exoplanet simulations. The underlying model is written in Fortran and may largely be configured with Python scripts. Python scripts are also used to run the model on different architectures, to archive the output, and for diagnostics, graphics, and post-processing. All of these features are publicly available in a Git-based repository.en_GB
dc.description.sponsorshipThis work was funded by the Leverhulme Trust, NERC (grant NE/M006123/1), the Royal Society (Wolfson Foundation), EPSRC, the Newton Fund (CSSP project), and the Marie Curie Foundation.en_GB
dc.identifier.citationVol. 11, pp. 843 - 859en_GB
dc.identifier.doi10.5194/gmd-11-843-2018
dc.identifier.urihttp://hdl.handle.net/10871/31943
dc.language.isoenen_GB
dc.publisherEuropean Geosciences Union (EGU) / Copernicus Publicationsen_GB
dc.relation.urlhttp://hdl.handle.net/10871/31579en_GB
dc.rights© Author(s) 2018. Open access. This work is distributed under the Creative Commons Attribution 4.0 License: https://creativecommons.org/licenses/by/4.0/en_GB
dc.titleIsca, v1.0: a framework for the global modelling of the atmospheres of Earth and other planets at varying levels of complexityen_GB
dc.typeArticleen_GB
dc.date.available2018-03-07T15:22:11Z
dc.identifier.issn1991-959X
dc.descriptionThis is the final version of the article. Available from EGU via the DOI in this record.en_GB
dc.descriptionThe accepted author manuscript, published in Geoscientific Model Development Discussions, is in ORE: http://hdl.handle.net/10871/31579en_GB
dc.identifier.journalGeoscientific Model Developmenten_GB


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