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Sep 25, 2019
10 months 21 days Some improvements for salinity transport, including an upstream implementation of the upper and lower boundary conditions for advection. Setting the lower boundary diffusion to a zero-flux boundary condition also seems to improve the stability.
Commit 1798, by Nander Wever
10 months 21 days Fixing clumsy commit 1795
Commit 1797, by Nander Wever
10 months 21 days Bug fix for salinity transport.
Commit 1796, by Nander Wever
10 months 21 days Improved initial conditions for sea ice.
Commit 1795, by Nander Wever
10 months 21 days Take care of pressure head upon layer merging.
Commit 1794, by Nander Wever
Sep 23, 2019
10 months 23 days Small improvement for sea ice simulations.
Commit 1793, by Nander Wever
10 months 23 days Changing lower boundary condition for diffusion.
Commit 1792, by Nander Wever
Sep 20, 2019
10 months 26 days Several improvements for the stability of Richards solver for sea ice, including applying relative convergence criterions instead of absolute ones. This is necessary, as we work with very tiny pore spaces, such that tiny values of theta can be relat…
Commit 1791, by Nander Wever
10 months 26 days Correcting the implicit numerical scheme for salinity transport.
Commit 1790, by Nander Wever
10 months 26 days Stability improvements for the new phase change method for sea ice.
Commit 1789, by Nander Wever
10 months 26 days Recently merged elements where frequently splitted immediately after in the sea ice simulations, fixing that.
Commit 1788, by Nander Wever
10 months 26 days Instabilities in the sea ice version when melt occurs is now mitigated by a different layer merging strategy.
Commit 1787, by Nander Wever
Sep 19, 2019
10 months 27 days Bug fix for keeping track of the marked reference layer when splitting elements.
Commit 1786, by Nander Wever
10 months 27 days Making test against undefined/nodata consistent.
Commit 1785, by Nander Wever
Sep 18, 2019
10 months 28 days Implementing the possibility to have a different boundary condition for advection for incoming or outgoing flux, such that the incoming flux (rain for example) can advect fresh water, while evaporation would leave salt behind.
Commit 1784, by Nander Wever
10 months 28 days Fixing commit 1782.
Commit 1783, by Nander Wever
10 months 28 days Decreasing convergence criterions for temperature equation to improve stability of the sea ice simulations.
Commit 1782, by Nander Wever
10 months 28 days Adjusting pressure head for removed water from the model domain. Also improving a split condition, as it was counteracting some ongoing element merging.
Commit 1781, by Nander Wever
Aug 30, 2019
11 months 16 days Small documentation fix (wrong units)
Commit 1780, by Mathias Bavay
11 months 16 days File missing in previous commit
Commit 1779, by Adrien Michel

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