cyamin wrote:
Hello all,
The new FLUXLINE method works fine, but I miss the file output instead of the listing output. According to fluxpr_sisyphe, it looks quite a tedious process to implement. I will try to use the python code to parse the logs, but my case is not as straightforward as I have hot-starts and chaining loops that end up in tens of runs...
In the meantime, what are the shortcomings of the previous method? I might have to rely on it in the end.
Best Regards,
Costas
Hi Costas,
yes, it would be nice to have a single outputfile for the fluxlines. This is a good point for the further development. We will work on the fluxline during our next Telemac coding week at BAW.
The previous method was less accurate. The fluxline method uses exactly the same flux as used in Sisyphe for the balance computations. This means that we do not introduce some errors due different kind of flux approximations.
The main advantage is, that the method also accounts for the limiting of sediment discharge (positive depths) when not enough sediment is at an node/element. The old method gives only the potential discharge. This can lead to large differences/errors.
In my opinion it should be best practice to ensure that the mass balance is correct during modeling. This can be done with a combination of fluxlines and "mass boxes". A mass box is a part of the domain which is surrounded by fluxlines or the boundary. After your computation you can set up a local mass balance for parts of your domain or the whole domain.
Best regards
Leo