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Latest developments in hydrology -
hydrodynamic modelling using the
Delft3D FM Suite
Arthur van Dam and Mark Hegnauer
Modelling from catchment to coast
12 November 2018
Extreme weather: time and place matters
Evacuating people as the early effects of Hurricane Sandy are felt in the Red
Hook neighborhood of Brooklyn (EPA)
Water availability in 2018
12 November 2018
Water availability in 2018
12 November 2018
Water availability in 2018
Precipitation deficit in The Netherlands in 2018
Nationwide average over 13 stations
5% most dry years
Median
Record year 1976
Year 2018: currently 296 mm
2018 Innovation projects
4 options for hydrological modelling with Delft3D FM
0) Distributed hydrology (do it all in the D-Flow FM module)
1) Lumped hydrology: domain coupling with RR
2) Fully distributed with MetaSWAP and MODFLOW
3) Distributed hydrology: vertical coupling with wflow
4) Distributed hydrology: domain coupling with wflow
4 options for hydrological modelling with Delft3D FM
1. 2.3.4.
Option 0: Do it all in the D-Flow FM module
Fully distributed: grid covering entire domain, and all
interception/evaporation/infiltration/etc. computed by D-Flow FM
Movie by Herman Kernkamp
Software development
Option 1: Lumped hydrology: domain coupling with RR
12 November 2018
- RR-unpaved ( id 1) and RR-Sacramento ( id 2)
- Coupled to 1D laterals with id 5 and 6
- 1D channel
- trapezoidal cross-section
- upstream boundary (id 3) Q=1 m3/s
- downstream boundary (id 4) h=1m
Joint work with Geert Prinsen
and Martijn Russcher
Lumped concepts, known from SOBEK RR
Coupled with D-Flow FM module
(online/in timeloop)
Only lumped or semi-distributed modelling,
using concepts like Sacramento, HBV,
Walrus, polder model with Capsim,
HWRW Urban runoff model, SCS, ..
Option 1: Lumped hydrology: domain coupling with RR
DIMR
DIMR-configuratie
Lumped concepts
Initialize
Perform_
Timestep
Finalize
Set (varId)
Get (varId)
D-Flow FM (1D-2D-3D)
timeloop
Initialize
Perform_
Timestep
Finalize
Set (varId)
Get (varId)
Option 1: Impact on-line coupling depends on lumped concept
- RR-Sacramento: not depending on 1D water level
- RR-Unpaved: there is impact of 1D water level
- Test using constant water level 0.0 or on-line level
from D-Flow FM (1D), approximately 1.0
12 November 2018
Whole simulation Detail – zoomed in
Conclusion: It works!
D-Flow FM - RR on-line coupled gives very similar results as
SOBEK 1DFLOW - RR combination (but not identical)
SOBEK-RR, no on-line coupling
SOBEK, on-line 1D level
D-Flow FM on-line
coupled to RR
Option 1: Comparison: Delft3D FM Suite and SOBEK 2 Suite
Option 1: Lumped RR in practice: Westamstel
6 december 2018
1D surface water
2D surface water
2D unsaturated zone
(soil moisture)
2D/3D groundwater
Option 2: Fully distributed with MetaSWAP and MODFLOW
Detailed coupling “LUMBRICUS” project
12 November 2018
Option 2: Fully distributed with MetaSWAP and MODFLOW
From: the Lumbricus project
Option 2: Fully distributed with MetaSWAP and MODFLOW
Option 3 and 4: Coupling with wflow
▪ Distributed hydrology: vertical coupling with wflow
▪ Distributed hydrology: domain coupling with wflow
wflow = An open source hydrological modelling framework
Key strengths:
▪ Directly links to available (gridded) datasets
▪ Multiple hydrological concepts included
▪ Open Source – easy to work together / share knowledge
▪ Strongly linked to other products, modules, platforms and tools
(e.g. MODFLOW (BMI), Delft-FEWS (wflow-adapter) and
OpenDA (BMI))
12 November 2018
Connectivity via:
▪ BMI
▪ NETCDF-CF
▪ Open standards
Usage of the wflow framework
wflow is used by Universities, Research Institutes, Consultants and
Governments around the world
12 November 2018
wflow model available
Example projects using wflow
▪ “RWSOS Rivieren” (forecasting Rhine / Meuse flows into
The Netherlands)
▪ Indonesia (nation wide water availability)
▪ Sava Flood Forecasting System (forecasting)
▪ Ganga River Basin Model for strategic basin planning (IWRM)
What is wflow?
A hydrological modelling framework:
▪ Based on PCRaster / Python framework
▪ Fully distributed hydrological model
▪ Different hydrological concepts available
▪ HBV
▪ SBM
▪ FlexTopo (beta)
▪ W3RA
▪ PCRGLOB-WB
▪ Different modules available:
▪ Routing module
▪ (Simple) reservoirs module
▪ Crop growth module (LINTUL)
Characteristics of the wflow model
▪ Grid based hydrological modelling
12 November 2018
Snowpack simulation in Albania Runoff simulation in France
Goal:
▪ Better description of hydrological
processes in Delft3D FM Suite
▪ Sharing code in a hydrological
library
▪ Experiment with hydrological
modelling on unstructured grids
12 November 2018
Option 3: Distributed hydrology: vertical coupling with wflow
wflow
wflow framework
• Kinematic wave
• Sub-surface flow
• Reservoir module
• …
Delft3D FM Suite
framework
• Dynamic wave
• 1D network
• 2D grids
• …
Hydrological lib
• Snowmelt
• Interception
• Evaporation
• Infiltration
• Percolation
• …
Goal:
▪ “From catchment to coast” models
▪ Simulate each process with the right model
wflow
D-Flow FM
Option 4: Distributed hydrology: domain coupling with wflow
More information
Open Source Software portal:
▪ https://oss.deltares.nl/web/delft3dfm
▪ https://oss.deltares.nl/web/wflow
Online technical documentation wflow:
▪ http://wflow.readthedocs.io/en/latest/
12 November 2018

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DSD-INT 2018 Latest developments in hydrology - hydrodynamic modelling using the Delft3D FM Suite - van Dam

  • 1. Latest developments in hydrology - hydrodynamic modelling using the Delft3D FM Suite Arthur van Dam and Mark Hegnauer
  • 2. Modelling from catchment to coast 12 November 2018
  • 3. Extreme weather: time and place matters Evacuating people as the early effects of Hurricane Sandy are felt in the Red Hook neighborhood of Brooklyn (EPA)
  • 4. Water availability in 2018 12 November 2018
  • 5. Water availability in 2018 12 November 2018
  • 6. Water availability in 2018 Precipitation deficit in The Netherlands in 2018 Nationwide average over 13 stations 5% most dry years Median Record year 1976 Year 2018: currently 296 mm
  • 7. 2018 Innovation projects 4 options for hydrological modelling with Delft3D FM
  • 8. 0) Distributed hydrology (do it all in the D-Flow FM module) 1) Lumped hydrology: domain coupling with RR 2) Fully distributed with MetaSWAP and MODFLOW 3) Distributed hydrology: vertical coupling with wflow 4) Distributed hydrology: domain coupling with wflow 4 options for hydrological modelling with Delft3D FM 1. 2.3.4.
  • 9. Option 0: Do it all in the D-Flow FM module Fully distributed: grid covering entire domain, and all interception/evaporation/infiltration/etc. computed by D-Flow FM Movie by Herman Kernkamp
  • 11. Option 1: Lumped hydrology: domain coupling with RR 12 November 2018 - RR-unpaved ( id 1) and RR-Sacramento ( id 2) - Coupled to 1D laterals with id 5 and 6 - 1D channel - trapezoidal cross-section - upstream boundary (id 3) Q=1 m3/s - downstream boundary (id 4) h=1m Joint work with Geert Prinsen and Martijn Russcher
  • 12. Lumped concepts, known from SOBEK RR Coupled with D-Flow FM module (online/in timeloop) Only lumped or semi-distributed modelling, using concepts like Sacramento, HBV, Walrus, polder model with Capsim, HWRW Urban runoff model, SCS, .. Option 1: Lumped hydrology: domain coupling with RR DIMR DIMR-configuratie Lumped concepts Initialize Perform_ Timestep Finalize Set (varId) Get (varId) D-Flow FM (1D-2D-3D) timeloop Initialize Perform_ Timestep Finalize Set (varId) Get (varId)
  • 13. Option 1: Impact on-line coupling depends on lumped concept - RR-Sacramento: not depending on 1D water level - RR-Unpaved: there is impact of 1D water level - Test using constant water level 0.0 or on-line level from D-Flow FM (1D), approximately 1.0
  • 14. 12 November 2018 Whole simulation Detail – zoomed in Conclusion: It works! D-Flow FM - RR on-line coupled gives very similar results as SOBEK 1DFLOW - RR combination (but not identical) SOBEK-RR, no on-line coupling SOBEK, on-line 1D level D-Flow FM on-line coupled to RR Option 1: Comparison: Delft3D FM Suite and SOBEK 2 Suite
  • 15. Option 1: Lumped RR in practice: Westamstel 6 december 2018
  • 16. 1D surface water 2D surface water 2D unsaturated zone (soil moisture) 2D/3D groundwater Option 2: Fully distributed with MetaSWAP and MODFLOW Detailed coupling “LUMBRICUS” project
  • 17. 12 November 2018 Option 2: Fully distributed with MetaSWAP and MODFLOW
  • 18. From: the Lumbricus project Option 2: Fully distributed with MetaSWAP and MODFLOW
  • 19. Option 3 and 4: Coupling with wflow ▪ Distributed hydrology: vertical coupling with wflow ▪ Distributed hydrology: domain coupling with wflow wflow = An open source hydrological modelling framework Key strengths: ▪ Directly links to available (gridded) datasets ▪ Multiple hydrological concepts included ▪ Open Source – easy to work together / share knowledge ▪ Strongly linked to other products, modules, platforms and tools (e.g. MODFLOW (BMI), Delft-FEWS (wflow-adapter) and OpenDA (BMI)) 12 November 2018 Connectivity via: ▪ BMI ▪ NETCDF-CF ▪ Open standards
  • 20. Usage of the wflow framework wflow is used by Universities, Research Institutes, Consultants and Governments around the world 12 November 2018 wflow model available
  • 21. Example projects using wflow ▪ “RWSOS Rivieren” (forecasting Rhine / Meuse flows into The Netherlands) ▪ Indonesia (nation wide water availability) ▪ Sava Flood Forecasting System (forecasting) ▪ Ganga River Basin Model for strategic basin planning (IWRM)
  • 22. What is wflow? A hydrological modelling framework: ▪ Based on PCRaster / Python framework ▪ Fully distributed hydrological model ▪ Different hydrological concepts available ▪ HBV ▪ SBM ▪ FlexTopo (beta) ▪ W3RA ▪ PCRGLOB-WB ▪ Different modules available: ▪ Routing module ▪ (Simple) reservoirs module ▪ Crop growth module (LINTUL)
  • 23. Characteristics of the wflow model ▪ Grid based hydrological modelling 12 November 2018 Snowpack simulation in Albania Runoff simulation in France
  • 24. Goal: ▪ Better description of hydrological processes in Delft3D FM Suite ▪ Sharing code in a hydrological library ▪ Experiment with hydrological modelling on unstructured grids 12 November 2018 Option 3: Distributed hydrology: vertical coupling with wflow wflow wflow framework • Kinematic wave • Sub-surface flow • Reservoir module • … Delft3D FM Suite framework • Dynamic wave • 1D network • 2D grids • … Hydrological lib • Snowmelt • Interception • Evaporation • Infiltration • Percolation • …
  • 25. Goal: ▪ “From catchment to coast” models ▪ Simulate each process with the right model wflow D-Flow FM Option 4: Distributed hydrology: domain coupling with wflow
  • 26. More information Open Source Software portal: ▪ https://oss.deltares.nl/web/delft3dfm ▪ https://oss.deltares.nl/web/wflow Online technical documentation wflow: ▪ http://wflow.readthedocs.io/en/latest/ 12 November 2018