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DASSFLOW
The present page can give you a good idea of DassFlow's features (below: use of former versions V1.1 and V1.3), even if this page is not up-to-date.
Few other applications have been developped or are under progress by colleagues:
flood plain flow (Leze river, France) in collaboration with IMFT,
glacier flows (Variagated Alaska, Jakobshavn Groenland, Mertz Antarctica) , lab. LGGE and LEGOS.
discharge identification using satelitte data (Garonne river, France) in collaboration with IMFT.
Identification of inflow discharges. Pearl River, China.
Collaboration X. Lai (Niglas, Nanjin, China), J. Monnier.
- Identification of inflow discharge (at 3
boundaries)
- Observations :
- water elevation at 3 gauging stations
- discharge at 1 gauging station
Reference :
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Assimilation of one satellite image. Flood plain, Moselle River, France.
Collaboration: R. Hostache (PhD Cemagref 03-06), X. Lai (Niglas, China), J. Monnier, C. Puech (D.R. Cemagref Montpellier / Engref).
- Observations :
- Partial discharge measurements from the EDF station
- One satellite image : partial elevation values
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Observations from the EDF station
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discharge values |
Reliable elevation values
extracted from the satellite image
Work done by R. Hostache and
C. Puech |
- Sensitivities and identification of Manning coefficients
Manning coefficients: 10 land-uses
An video of a direct simulation on
the Moselle River is available.
References :
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Lagrangian data
Identification of the topography. Toy test case.
Collaboration M. Honnorat (PhD'07, Grenoble), J. Monnier, FX Le Dimet (U. Grenoble).
Configuration :
- Flow over a bump in a canal
- First guess : constant topography slope
Observations :
- Particle trajectories at surface
- Elevation at x=15m and x=70m
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Topography and reference
flow
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Reference and identified
topography
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References :
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Identification of the topography in a canal using a video camera.
Collaboration: M. Honnorat (PhD'07, Grenoble), J. Monnier, N. Rivière (Insa Lyon), E. Huot (Inria), FX Le Dimet (U. Grenoble).
- Video from an experiment conducted at the LMFA laboratory (N.
Rivière, LMFA Lyon) :
- flow over a plank in a canal
- floating particles (confetti) are introduced
- Particle trajectories are extracted from the video (E. Huot, INRIA
Clime Project)
- Identification of an "equivalent" topography (i.e. real topography + recirculation); identification of an "equivalent" Manning coefficient.
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Experiment
configuration |
Image shot from the video: tracers at surface |
References :
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Joint Assimilation Coupling algorithm: 2D zoom model over 1D global model
Collaboration: I. Gejadze (U. Strathclyde), J. Marin (engineer), J. Monnier, J.-B. Faure (Cemagref Lyon).
1D main channel coupled with 2D plain area
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JAC Algorithm performs calibration (data
assimilation) and coupling simultaneously.
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References:
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