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This table lists only the most important of the standard versions detailed in following sections. The major changes listed were in some cases introduced in intermediate standard versions that are not included in the table. No published version so far includes a well-tempered TRIFFID, although this is under test in xfhcs
This table lists only the most important of the standard versions detailed in following sections. The major changes listed were in some cases introduced in intermediate standard versions that are not included in the table.
Note that single-PE operation is not supported by these versions. Use MPP even when running on a single processor.
For technical updates and differences between standard jobs see standard job updates.
Where bugs are found post-release, they will be flagged here. In general, fixes will be included in the next release but not backported into older jobs. Bugs flagged up for any given version can be assumed to exist in all previous versions. More information on these issues and their fixes can usually be found on Robin’s old page, or more recently [[2015development|here].
Where bugs are found post-release, they will be flagged here. In general, fixes will be included in the next release but not backported into older jobs. Bugs flagged up for any given version can be assumed to exist in all previous versions. More information on these issues and their fixes can usually be found on Robin’s old page, or more recently here.
Where bugs are found post-release, they will be flagged here. In general, fixes will be included in the next release but not backported into older jobs. Bugs flagged up for any given version can be assumed to exist in all previous versions. More information on these issues and their fixes can usually be found on Robin’s page.
Where bugs are found post-release, they will be flagged here. In general, fixes will be included in the next release but not backported into older jobs. Bugs flagged up for any given version can be assumed to exist in all previous versions. More information on these issues and their fixes can usually be found on Robin’s old page, or more recently [[2015development|here].
LATEST (Robin’s jobs, not strictly release versions yet - ie. not available from Annette. Job names may change)
LATEST (Robin’s jobs, not strictly release versions yet. Job names may change)
xhkkg: MOSES2.2-BISICLES, unified Bristol/Reading format.
Development version of multi-layer snow, subgrid elevation tiles, mass-balance coupling to BISICLES icesheet
xfhcr: MOSES2.2/TRIFFID interactive CO2.
Full coupled carbon cycle FAMOUS. As used for NCAS Earth System summer schools
| xfhcu/s | currently being tested | MOSES 2.2, friction on top-level winds, free-drift sea-ice, tuned by Jonny Williams (Bristol) |
| xfhcu/s | Williams et al. (2008), Williams et al. (2014) | MOSES 2.2, friction on top-level winds, free-drift sea-ice, tuned by Jonny Williams (Bristol) |
see Williams et al. (2012) and now Williams et al. (2014)
| xfhcc | Smith (GMD, submitted) | xfxwb with friction on top-level winds instead of cap |
| xfxwb | EMICmip (AR5), Smith (GMD, submitted), Smith and Gregory (in press, about the last glacial cycle) | bug-fix for coastal snow on sea-ice, cap on top-level winds |
| xdbua | Smith et al. (2008), Smith and Gregory (2009), Balan Sarojini et al. (2011, UK THCMIP) | ozone vertical profile improved, sea-ice albedo returned to alleviate cold bias at high N latitudes, orbital parameters can be set or computed conveniently, very long absolute filenames, HadOCC with Utopia, salinity conservation and iceberg calving recalibrated |
| xfhcc | Smith (2012) | xfxwb with friction on top-level winds instead of cap |
| xfxwb | EMICmip (AR5), Smith (2012), Smith and Gregory (2012, about the last glacial cycle) | bug-fix for coastal snow on sea-ice, cap on top-level winds |
| xdbua | Smith et al. (2008), Smith and Gregory (2009, about AMOC response to hosing), Balan Sarojini et al. (2011, UK THCMIP) | ozone vertical profile improved, sea-ice albedo returned to alleviate cold bias at high N latitudes, orbital parameters can be set or computed conveniently, very long absolute filenames, HadOCC with Utopia, salinity conservation and iceberg calving recalibrated |
| xdbua | Smith et al. (2008), Smith and Gregory (2009), Balan Sarojini et al. (2011, UK THCMIP) | ozone vertical profile improved, sea-ice albedo returned to alleviate cold bias at high N latitudes, orbital parameters can be set or computed conveniently, very long absolute filenames, HadOCC with Utopia, salinity conservation and iceberg calving recalibrated |
| xdbua | Smith et al. (2008), Smith and Gregory (2009), Balan Sarojini et al. (2011, UK THCMIP) | ozone vertical profile improved, sea-ice albedo returned to alleviate cold bias at high N latitudes, orbital parameters can be set or computed conveniently, very long absolute filenames, HadOCC with Utopia, salinity conservation and iceberg calving recalibrated |
xcggb: New version of salinity correction - two minor bugfixes, correction also applied to the surface virtual fluxes of TCO2 and Alkalinity due to P-E+R (if HadOCC is switched on). The corrections are now STASHed in units of <tracer units> per second, rather than <tracer units> per timestep, so restarts that used the old scheme will have screwy corrections for the first year.
xcggb: New version of salinity correction - two minor bugfixes, correction also applied to the surface virtual fluxes of TCO2 and Alkalinity due to P-E+R (if HadOCC is switched on). The corrections are now STASHed in units of <tracer units> per second, rather than <tracer units> per timestep, so restarts that used the old scheme will have screwy corrections for the first year.
xbyvs: adtan with salinity drift corrected. (Standard job for HPCx is xcgga in the Reading UMUI.) Model largely as adtan (Jones et al., 2005) but includes a volume-uniform time-dependent correction to conserve water in the open oceans to cancel the drift from the rigid-lid salt-flux representation of ocean surface water fluxes. Isolated inland seas are not affected by this fix: their runaway salinities due to local P-E+R imbalance are simply capped at 0 or 50.
xbyvs: adtan with salinity drift corrected. (Standard job for HPCx is xcgga in the Reading UMUI.) Model largely as adtan (Jones et al., 2005) but includes a volume-uniform time-dependent correction to conserve water in the open oceans to cancel the drift from the rigid-lid salt-flux representation of ocean surface water fluxes. Isolated inland seas are not affected by this fix: their runaway salinities due to local P-E+R imbalance are simply capped at 0 or 50.