Edilbert Kirk
KlimaCampus, University of Hamburg, Germany
Klaus Frædrich
KlimaCampus, University of Hamburg, Germany
Frank Lunkeit
KlimaCampus, University of Hamburg, Germany
Carmen Ulmen
KlimaCampus, University of Hamburg, Germany
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Ingår i: State of Climate Visualization
Linköping Electronic Conference Proceedings 45:7, s. 49-55
Publicerad: 2009-12-09
ISBN:
ISSN: 1650-3686 (tryckt), 1650-3740 (online)
The Planet Simulator is a Model of Intermediate Complexity (MIC); suitable for climate and paleo-climate simulations and time scales up to ten thousand years or more. It runs on a wide range of hardware and operating systems including massive parallel cluster and workstations with UNIX; Solaris; Linux; MAC OS or any other UNIX style operating system. The priorities in development are set to speed; easy handling and portability. Its modular structure allows a problem dependent configuration. A graphical Model Starter (MoSt) can be used to select a model configuration from the repository; set its parameters; compile and run the model. The model can be run either in production mode for maximum performance or in interactive mode using a Graphical User Interface (GUI). This GUI is both a real time visualization interface for all model variables and a tool for tuning and experimenting with the model.
Asselin; R. (1972). Frequency filter for time integrations; Monthly Weather Review. 100; pp. 487–490.
Eliasen; E.; B. Machenhauer; E. Rasmusson; (1970). On a numerical method for integration of the hydrodynamical equations with a spectral representaion of the horizontal fields; Institute of Theoretical Meteorology; University of Copenhagen.
Fraedrich; K.; H. Jansen; E. Kirk; F. Lunkeit; (2005). The Planet Simulator: Green planet and desert world; Meteorologische Zeitschrift; 14; pp. 305–314.
Fraedrich; K.; E. Kirk; U. Luksch; and F. Lunkeit; (2005). The Portable University Model of the Atmosphere (PUMA): Storm track dynamics and low frequency variability; Meteorologische Zeitschrift; 14; pp. 735–745.
Hoskins; B. J.; A. J. Simmons; (1975). A multi-layer spectral model and the semi-implicit method; Quarterly Journal of the Royal Meteorological Society; 101; pp. 637–655.
Lunkeit; F.; M. Böttinger; K. Fraedrich; H. Jansen; E. Kirk; A. Kleidon; U. Luksch; (2007). Planet Simulator Reference Manual Version 15.0. Available at http://www.mi.uni hamburg.de/fileadmin/files/forschung/theomet/planet_simulator/downloads/PS_ReferenceGuide.pdf.
Orszag; S. A. (1970). Transform method for calculation of vector coupled sums; Journal of the Atmospheric Sciences; 27; pp. 890–895.
Robert; A. J. (1981). A stable numerical integration scheme for the primitive meteorological equations; Atmos. Ocean 19; pp. 35–46.
Roeckner; E.; K. Arpe; L. Bengtsson; (992). Simulation of present-day climate with the ECHAM model: Impact of model physics and resolution; Technical Report 93; Max- Planck-Institut.
Simmons; A. J.; B. Hoskins; D. Burrdidge; (1978). Stability of the semi-implicit method of time integration; Monthly Weather Review; 106; pp. 405–412.
