Custom Query (964 matches)
Results (877 - 879 of 964)
| Ticket | Owner | Reporter | Resolution | Summary |
|---|---|---|---|---|
| #321 | Fixed | Problem with Lfloats == F | ||
| Description |
This option is supposed to work like Lstations == F, i.e. we can compile with FLOATS or STATIONS and still deactivate them at runtime. But those options create segmentation faults when running. The solution is to modify the files inp_par.F, grid_coord.F and main3d.F by adding some tests there. |
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| #329 | Done | Horizontal diffusion of tracer perturbation | ||
| Description |
Implemented a new option, CLIMA_TS_MIX, to diffuse tracer perturbation (t-tclm) instead of tracer (t) field alone. This option can be used in some applications to reduce the numerical diapycnal mixing of tracer in deep waters. This strategy has been used extensively in other models. For example, see Mellor and Blumberg, 1985. |
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| #347 | Fixed | Correct small bug in step_floats.F for isobaric/geopotential floats | ||
| Description |
The is a bug in step_floats.F when computing the vertical position for isobaric (flt_Isobar) or geopotential floats (flt_Geopot). The k-loop in lines 265 and 441 should be: DO k=N(ng)-1,0,-1 instead of: DO k=N(ng)-1,1,-1 Notice that the interpolated value (cff6) for k=N(ng) needs to be computed first outside this loop. |
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