Revision fe53297356da5f02478fe9cafab5d9914a36d2be authored by Thorsten Becker on 14 August 2007, 03:33:21 UTC, committed by Thorsten Becker on 14 August 2007, 03:33:21 UTC
spacing to top and lower layers of shell. The coor_refine=0.1,0.15,0.1,0.2 parameters specify the radius fraction of the bottom layer [0], the fraction of the nodes in this layer [1], the top layer fraction [2], and the top layer node fraction [3]. I.e. the defaults will put 15% of all nz nodes into the 10% lower layer, 20% in the top 10% upper layer, and the rest in between. - renamed gzipped output version with sub-directory storage ascii-gz - built in restart facilities for temperature and tracers when using ascii-gz I/O with vtkio != 2 - added a composition viscosity function, CDEPV, based on two tracer flavors - for this to work, I had to move viscosity_input() *behind* tic_input() and tracer_input() in instructions - added tracer_enriched option for internal heating. If tracer = on and tracer_enriched = on, will reader Q0_enriched and vary the element heat production between Q0 for C = 0 and Q0_enriched for C = 1. I.e. this only works if C varies between 0 and 1. - added an option to write from all processros to a single VTK file, if ascii-gz is activated, and vtkio = 2. The VTK output is of the "legacy", serial, single-file type, and requires that all processors see the same filesystem. This will lead to a bottleneck for large # of CPU computations as each processor has to wait til the previous is done. More efficient I/O should be possible by using the distributed storage version of VTK, but I have no clue how this works. Anyone?
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README
We are pleased to announce the version 2.2 release of CitComS.py.
See the file INSTALL for building and installation instructions.
See the file NEWS for new features and bug fixes of this release.
Please send all bug reports by electronic mail to:
cig-mc@geodynamics.org
CitComS.py is free software. See the file COPYING for copying conditions.
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