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| Dec 30, 2013 | |
| 6 years 1 month | This is now a hopefully well tested commit that finalizes the introduction of a SNOW_EROSION switch acting only on the main station and SNOW_REDISTRIBUTION acting on virtual slopes only. Unless NUMBER_SLOPES is set to 1 and SNOW_EROSION is true, the |
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Commit 497, by Charles Fierz | |
| Dec 21, 2013 | |
| 6 years 2 months | A SOS Xmas commit (will be described later by H.C.G. Fierz) |
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Commit 496, by Charles Fierz | |
| Dec 20, 2013 | |
| 6 years 2 months | Switching to DGESVD solver when DGTSV fails is not always preferred, as DGESVD can be so slow, that a smaller time step and trying DGTSV again works faster. This is especially the case in simulations with many layers. Now this can be controlled with |
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Commit 495, by Nander Wever | |
| Dec 19, 2013 | |
| 6 years 2 months | Implementation of the liquid water index for virtual north and south slopes (dumped to SDBO only). Surface hoar at the surface (nodal property) also shows up in dumped profiles (PRF and IMIS). Rename new_snow_grain_rad and new_snow_bond_rad to *_size |
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Commit 494, by Charles Fierz | |
| Dec 16, 2013 | |
| 6 years 2 months | Implement Edgar Schmucki's new albedo parameterization (SCHMUCKI, version X32 is set) thereby moving element property rg_opt to ogs, that is twice the former value ;-) New keys SNOW_ALBEDO, ALBEDO_PARAMETERIZATION, ALBEDO_FIXEDVALUE Renamed quite a n |
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Commit 493, by Charles Fierz | |
| Dec 15, 2013 | |
| 6 years 2 months | Disentangle HN_DENSITY and HN_DENSITY_MODEL to HN_DENSITY, HN_DENSITY_PARAMETERIZATION and HN_DENSITY_FIXEDVALUE |
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Commit 492, by Charles Fierz | |
| Dec 11, 2013 | |
| 6 years 2 months | New approach for determining the residual water content when solving water transport in snow using Richards equation. Just taking theta_r=0 was causing a too big error in wet snow covers, so something different was needed. |
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Commit 491, by Nander Wever | |
| 6 years 2 months | When CHANGE_BC=false, there is no need to make THRESH_CHANGE_BC mandatory... |
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Commit 490, by Mathias Bavay | |
| Dec 10, 2013 | |
| 6 years 2 months | The Calonne (2012) parameterization of saturated hydraulic conductivity provides a better agreement with measured runoff at CDP and WFJ, so I make it the default. Furthermore, it is better to use the rg_opt for Calonne, instead of rg, as the first on |
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Commit 489, by Nander Wever | |
| Dec 9, 2013 | |
| 6 years 2 months | Introducing the Calonne (2012) parameterization for hydraulic conductivity. So now, one can choose between Shimizu (1970) and Calonne (2012). |
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Commit 488, by Nander Wever | |
| 6 years 2 months | The van Genuchten parameters used for Richards equation needed adequate referencing, so a revision was necessary, as I could not find the original source. I now use the ROSETTA data for the soil types, which is widely used. |
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Commit 487, by Nander Wever | |
| 6 years 2 months | Making the air entry pressure variable. It depends on a maximum pore size, which can be specified now differently from the standard 5mm for each soil layer or the snowpack. |
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Commit 486, by Nander Wever | |
| Dec 4, 2013 | |
| 6 years 2 months | A follow up on my commit in rev 479: a better approach turned out to be to only limit settling in case we use richards equation for snow in an alpine3d simulation. All other cases seem to work fine with normal settling treatment. |
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Commit 485, by Nander Wever | |
| Nov 27, 2013 | |
| 6 years 2 months | Introducing a finer control of boundary conditions for solving Richards equation, depending on whether snow is present or not. |
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Commit 484, by Nander Wever | |
| 6 years 2 months | Setting the predefined soil properties to more realistic values and update the CDP-soil. |
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Commit 483, by Nander Wever | |
| Nov 25, 2013 | |
| 6 years 2 months | Make the SOIL_FLUX configuration key optional (set to FALSE by default) in order to be consistent with inishell |
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Commit 482, by Mathias Bavay | |
| Nov 20, 2013 | |
| 6 years 3 months | Forgot a ";"... |
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Commit 481, by Nander Wever | |
| 6 years 3 months | Adding a soil definition for Col de Porte (CDP) in Richards equation solver. |
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Commit 480, by Nander Wever | |
| Nov 17, 2013 | |
| 6 years 3 months | Closing issue 304. Amount of settling is now limited to theta[AIR], while leaving also some space in case all liquid water would refreeze. This makes the loop (hopefully) obsolete. An additional tuning factor was added to ensure stability in the Rich |
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Commit 479, by Nander Wever | |
| 6 years 3 months | A small correction on Rev 469: when there is no snow, but we have soil layers, AsciiIO should write out the soil layers, and not close the file directly. |
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Commit 478, by Nander Wever | |
