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paper: Minor change (included figure size and position).

mesh
Pierre-Antoine Rouby 2023-09-15 09:52:14 +02:00
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@ -50,6 +50,8 @@ Boundary conditions (BC) are associated with a network node. There are three dif
Figure 3: Edition window of the boundary conditions hydrograph for the Saar river upstream node.
3.1.3 Lateral contribution
The user interface for lateral contributions is similar to that for boundary conditions, except that it applies to a part of a reach between two KP, and not to a node.
3.1.4 Friction
@ -57,7 +59,6 @@ Friction editing is linked to a reach, a friction coefficient is defined and the
Figure 4: The reach portions for friction coefficient edition window for the Saar study.
3.1.5 Initial conditions
@ -94,10 +95,12 @@ Figure 8: Sediment layers definition window for Saar study. This sediment layers
Figure 9: Sediment layers defined in Figure 8 applied to the reach Saar.
Figure 10: Sedimentary results window for “Elargissement” tests case at timestamps 2113200.0 sec for reach R1 and cross-section at KP 427.7778. This example has only two sediment layers.
4. Future work
@ -115,7 +118,7 @@ Old PAMHyR functionalities and additional functionalities, allowed the definitio
5. Conclusion
After a great deal of preparatory work, experimentation, technical selection, proof-of-concept and several months of development, Pamhyr2 is currently in version “v0.0.0”14 and contains almost 20,000 lines of Python code. It allows to create a minimal 1D hydro-sedimentary study, run a Mage simulation and visualize some of the results obtained, all with a more user-friendly interface. But the software is still unstable and under development, and many modifications and improvements are still to be made before it can really be used by everyone. Furthermore, even though many of the features of the original version of PAMHyR are already available (see 3.1 page 3), there are still many to be added to make Pamhyr2 a complete, useful and fully functional piece of software.
ACKNOWLEDGEMENTS
The results presented here come from the Pamhyr project partially funded by the Carnot Eau & Environnement institute and the French National Research Agency. Carnot Eau & Environnement was accredited in March 2020 by the French Ministry of Research and Higher Education on the proposal of the Agence Nationale de la Recherche. The signatory members are INRAE, CNRS, Aix Marseille University, IFTS, INSA Lyon, IRD, Université de Montpellier and Université de Savoie Mont-Blanc.
The results presented here partially come from the Pamhyr PITI project funded by the Carnot Eau & Environnement institute and the French National Research Agency. Carnot Eau & Environnement was accredited in March 2020 by the French Ministry of Research and Higher Education on the proposal of the Agence Nationale de la Recherche. The signatory members are INRAE, CNRS, Aix Marseille University, IFTS, INSA Lyon, IRD, Université de Montpellier and Université de Savoie Mont-Blanc.
The authors thank Sylvain Coulibaly for his preparatory work and his technical choices.
REFERENCES and Citations