|Apr 24, 2014|
|5 years 8 months ||fix a typo
|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
|5 years 8 months ||taking dev commit 548, 550, 551, 552, 553 and 554
|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...
|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
|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.
|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
|Apr 17, 2014|
|5 years 9 months ||CodingStyle, updated broken link|
|Apr 16, 2014|
|5 years 9 months ||Correcting some units specified in comments accompanying variable
|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.
|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.
|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
|Apr 14, 2014|
|5 years 9 months ||Merging dev-542 and 545 (bug fix)
|5 years 9 months ||Email-NewRelease, Email sent for new Snowpack releases
|5 years 9 months ||Email-NewSnowpackUser, Email sent to new Snowpack users
|Apr 10, 2014|
|5 years 9 months ||committing dev-540 and 541
|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.
|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.
|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
|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