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Gr rainfall intensity #325
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Voilà ma review.
**Transfer** | ||
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In context of high rainfall intensities triggering flash flood responses, it is crucial to account for fast dynamics related to surface/hypodermic runoff | ||
and slower responses due to delayed/deeper flows (e.g. https://doi.org/10.5194/hess-26-5185-2022). |
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Pq pas mettre une citation pour Douinot et al. (2022) plutôt qu'un lien ?
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La référence à citer est douinot et al. 2018 ; https://doi.org/10.5194/hess-22-5317-2018 (multi-hypothèses vs transferts latéraux, modele marine, bassins mediterranéens); je n'ai pas lu DOuinot 2022 (bassin et modele Luxembourg ?)
Rephrase please: |
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Well done!
Qu'en est il des aspects optimisation/bornes de ces nouveaux paramètres ? A discuter puis tester avec Ahmad, aussi avec imperviousness sur zone urbaine.
Je referai un passage sur la doc rst et les equations directement en sphinx, plus facile pour la lisibilité.
**Transfer** | ||
|
||
In context of high rainfall intensities triggering flash flood responses, it is crucial to account for fast dynamics related to surface/hypodermic runoff | ||
and slower responses due to delayed/deeper flows (e.g. https://doi.org/10.5194/hess-26-5185-2022). |
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Choose a reason for hiding this comment
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La référence à citer est douinot et al. 2018 ; https://doi.org/10.5194/hess-22-5317-2018 (multi-hypothèses vs transferts latéraux, modele marine, bassins mediterranéens); je n'ai pas lu DOuinot 2022 (bassin et modele Luxembourg ?)
Co-authored-by: Ngo Nghi Truyen Huynh <129378719+nghi-truyen@users.noreply.github.com>
Co-authored-by: Ngo Nghi Truyen Huynh <129378719+nghi-truyen@users.noreply.github.com>
Co-authored-by: Ngo Nghi Truyen Huynh <129378719+nghi-truyen@users.noreply.github.com>
les valeurs par défaut : |
Merci beaucoup Apolline. |
Je rajoute les comments sur la branch test de Ahmad. |
Implementation of a GR model structure adapted to manage high rainfall intensity, inspired from Astagneau et al., called gr4_ri and gr5_ri.
For each new structure have been added 2 tunable parameters: one affecting infiltration into production reservoir and one affecting the partitioning of net rainfall between the two transfer branches.