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| Apr 24, 2014 | |
| 5 years 8 months | fix a typo |
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Commit 558, by Mathias Bavay | |
| 5 years 8 months | The air emissivity is now computed the same way regardless of where it happens (since it was computed at two different locations in Main.cc). A new function has been created for readability in Main.cc |
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Commit 557, by Mathias Bavay | |
| 5 years 8 months | taking dev commit 548, 550, 551, 552, 553 and 554 |
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Commit 556, by Mathias Bavay | |
| 5 years 8 months | Fixed a warning for undefined variable that was leading to random memory access. This whole piece of code will be rewritten anyway... |
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Commit 555, by Mathias Bavay | |
| Apr 23, 2014 | |
| 5 years 8 months | Introducing the water retention curve based on the Yamaguchi (2012) results. Recommended is to use the old one from 2010, as that one is verified in the publication in the cryosphere-paper. The new one should be tested in a next paper, together with |
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Commit 554, by Nander Wever | |
| 5 years 8 months | BUGFIX! If the key WATERTRANSPORTMODEL_SOIL = RICHARDSEQUATION was specified, the RE-solver was called for the soil part even in simulations without soil. This crashes the simulation (of course). Adjusted the if-statement. |
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Commit 553, by Nander Wever | |
| Apr 22, 2014 | |
| 5 years 9 months | To improve energy balance, it's recommended to suppress merging of two elements at the surface when the surface layer is dry and the layer below is wet (due to penetrating shortwave radiation). After removal of the top layer, the node below suddenly |
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Commit 552, by Nander Wever | |
| Apr 17, 2014 | |
| 5 years 9 months | CodingStyle, updated broken link |
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Change of CodingStyle, by Aurelien Gallice | |
| Apr 16, 2014 | |
| 5 years 9 months | Correcting some units specified in comments accompanying variable declarations. |
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Commit 551, by Nander Wever | |
| 5 years 9 months | A follow up on commit 548: I now implement the calculation of the limiting case explicitly, in case some future generation wants to change Constants::density_ice or *_water. |
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Commit 550, by Nander Wever | |
| Apr 15, 2014 | |
| 5 years 9 months | Small problems in the new phase change scheme are solved by this commit. Nodal temperature of the surface layer should be limited based on the presence of water or ice, or both. |
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Commit 549, by Nander Wever | |
| 5 years 9 months | The function defined for residual water content could reach a point where theta_i + (theta_r * (Constants::density_water/Constants::density_ice)) >= 1.0. This limiting case is when theta[ICE]=0.970886735. Although I think this is not causing problems |
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Commit 548, by Nander Wever | |
| Apr 14, 2014 | |
| 5 years 9 months | Merging dev-542 and 545 (bug fix) |
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Commit 547, by Mathias Bavay | |
| 5 years 9 months | Email-NewRelease, Email sent for new Snowpack releases |
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Creation of resource Email-NewRelease, by Mathias Bavay | |
| 5 years 9 months | Email-NewSnowpackUser, Email sent to new Snowpack users |
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Creation of resource Email-NewSnowpackUser, by Mathias Bavay | |
| Apr 10, 2014 | |
| 5 years 9 months | committing dev-540 and 541 |
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Commit 546, by Mathias Bavay | |
| 5 years 9 months | BUG FIX! Element temperature of upper soil layer was cooling too much when last snow element was being removed, as a result of a wrongly calculated energy needed for melt. |
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Commit 545, by Nander Wever | |
| 5 years 9 months | To keep a properly energy balance, shortwave absorption by the top soil element may be considered part of the snow-soil interface flux. |
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Commit 544, by Nander Wever | |
| Apr 8, 2014 | |
| 5 years 9 months | This commit introduces the variables and functions necessary to keep track of the energy balance of the soil part, very similar to the already present variables for the energy balance of the snowpack. The variables are always calculated, but by defau |
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Commit 543, by Nander Wever | |
| Apr 7, 2014 | |
| 5 years 9 months | Element property Qmf (phase change energy) also needs to be calculated with soil freezing/thawing when using Richards solver for soil. |
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Commit 542, by Nander Wever | |
