snowpack

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Oct 21, 2014
5 years 27 days More default values for Canopy, it should now be possible to run with Canopy without providing any extra keys
Commit 697, by Mathias Bavay
5 years 27 days Utils: improvements to function for unit conversion DataClasses: correction of a mistake in a comment CaaMLIO: first working version for reading/writing caaml (xml) files
Commit 696, by Adrien Gaudard
Oct 17, 2014
5 years 1 month Renamed HTRUNKS as QStrunks (a little clearer for a sensible heat flux)
Commit 695, by Mathias Bavay
Oct 13, 2014
5 years 1 month Integrating the two layers Canopy model. Now the new keys are in SnowpackAdvanced and are handled like any other key with a default value, the .met files have been reverted (in order to avoid breaking existing applications) and the indentation fixed
Commit 694, by Mathias Bavay
5 years 1 month The special assignment operator "=" does not seem to be necessary for ElementData and NodeData, so remove it again from the code (introduced by commit 691). Related to the element-splitting code.
Commit 693, by Nander Wever
Oct 10, 2014
5 years 1 month Some afterthoughts for commit 691.
Commit 692, by Nander Wever
5 years 1 month Implementation of a mechanism to reduce the number of elements deeper in the snowpack, and splitting the elements again when they come closer to the surface. Of interest for simulations with Glaciers or deep firn, to reduce the computational load. Ac
Commit 691, by Nander Wever
5 years 1 month Putting back a previous commit that was deleted by either the moving around of source files, or someone committing an old version of Snowpack.cc???
Commit 690, by Nander Wever
Oct 8, 2014
5 years 1 month 2-layer canopy model, litter albedo and mixed precipitations. Main change for the user : add CanopyBasalArea=xxx -default value : 0.004 - in the .snoold file after the CanopyLeafAreaIndex specification
5 years 1 month Allowing to specify the lower boundary condition for Richards equation in the ini file, using the key LB_COND_WATERFLUX. Implemented choices are: WATERTABLE (recommended), FREEDRAINAGE (recommended and default), DIRICHLET, GRAVITATIONALDRAINAGE and S
Commit 688, by Nander Wever
Oct 7, 2014
5 years 1 month porting stable commit 686 (svn version on Windows)
Commit 687, by Mathias Bavay
5 years 1 month Allowing the svn version to be used also on Windows
Commit 686, by Mathias Bavay
5 years 1 month The problem of snow surface temperatures above 0 degC is very present and visible, but the opposite may very, very rarely also occur: cooling wet snow elements may get a surface temperature below 0 degC, altough the element itself doesn't undergo pha
Commit 685, by Nander Wever
5 years 1 month Hopefully finally solving the issue of surface temperatures above 0 degC, in case the surface element itself remains below 0 degC, and consequently, no phase changes occur.
Commit 684, by Nander Wever
5 years 1 month When merging elements, it turned out to be a more consistent approach to keep the density of the lower element constant. Often elements that are "removed" (in fact: merged), have low density, as they are melting. This artificially seemed to produce l
Commit 683, by Nander Wever
5 years 1 month Forgot once more to consider the case of simulations without soil layers....
Commit 682, by Nander Wever
Oct 1, 2014
5 years 1 month Repairing typo in previous commit.
Commit 681, by Nander Wever
5 years 1 month Solving a bug where SNOW surface temperature could become above 0 degC. This particularly happened when the element itself remained below 0 degC and only the surface node exceeded 0 degC. Then no phase change occured, so the top node remains above 0
Commit 680, by Nander Wever
5 years 1 month Solving a bug where SNOW surface temperature could become above 0 degC. This particularly happened when the element itself remained below 0 degC and only the surface node exceeded 0 degC. Then no phase change occured, so the top node remains above 0
Commit 679, by Nander Wever
Sep 29, 2014
5 years 1 month Proper commit 675: Introduce a very simple constant degree day melt model, which only is active as long as the surface layer is melting and replaces the other energy fluxes; more complex version may be implemented later
Commit 678, by Mathias Bavay

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