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Weather Forecasting Services during Marine Operations in the Angra dos Reis Bay (RJ) 
Application of Delft3D in an Operational Forecasting System 
Delft3D Users Meeting 2014
INTRODUCTION 
•In support for marine operations in Angra dos Reis Bay, Tetra Tech performed forecasting services of meteoceanographic conditions; 
•Forecasts were obtained through a refined operational modeling system, coupling atmospheric and oceanic components; 
•Local measurements of atmospheric, hydrodynamic and wave parameters were used to validate the numerical modeling products prior to the start of operations; 
•During the marine operations period forecasting bulletins were provided with updating intervals of 12 hours.
STUDY LOCATION 
•The Ilha Grande Bay is located in the Southern coast of the state of Rio de Janeiro; 
•This region has great importance ecologically, for tourism and for the fishing industry, holding biological reserves and environmentally protected areas; 
•On the coast, besides the Central Nuclear Almirante Álvaro Alberto – CNAAA (Nuclear Central Almirante Álvaro Alberto), there are shipyard industries.
STUDY LOCATION
CIRCULATION PATTERNS 
•According to Signorini (1980) 
The circulation of the partially mixed estuarine system, formed by the Ilha Grande Bay (IGB) and Sepetiba Bay (SEPB), results from effects of tides, winds and density gradients. 
It can be observed the presence of a clockwise (west-east) flux around Ilha Grande. 
•The measured currents show a clockwise (54,6% to E) and a counter-clockwise flux (41,2% to W).
OPERATIONAL PROCEDURE 
•Bulletin updates were sent twice a day with forecasts for the following 72 hours of the environmental conditions predicted by the modeling system 
•An alert system was implemented in the bulletins, indicating when the forecasted environmental conditions were according to established thresholds for the execution of transport and lifting procedures. The threshold values were given by the contractor for each procedure as: 
Conditions for transport: 
•Wind speed ≤ 14 knots 
•Current speed ≤ 0.3 m/s 
•Wave peak period (Tp) ≤ 10 s 
•Significant wave height (Hs) ≤ 0.3 m 
Conditions for lifting: 
•Wind speed ≤ 10 knots 
•Wave peak period (Tp) ≤ 7 s 
•Significant wave height (Hs) ≤ 0.3 m
BULLETIN EXAMPLE (1)
BULLETIN EXAMPLE (2)
NUMERICAL MODELS 
•The operational procedure to generate the metocean forecasts in the Angra dos Reis Bay region was composed with three kinds of numerical models: 
Atmospheric model (WRF) 
Two wave models (WW3 and SWAN) 
Hydrodynamic model (Delft3D)
ATMOSPHERIC MODEL 
•WRF (Weather Reserch and Forecasting) 
NMM core (Nonhydrostatic Mesoscale Model), developed by north American centers NOAA and NCEP. 
Forced with global model data from the GFS (Global Forecasting System), with spatial resolution of 0.5° and 3- hour intervals. The GFS was developed and is maintained by NCEP, with online available outputs in the spatial and temporal resolution mentioned. 
The WRF-NMM model was setup with two nested grids. The coarser domain covered the Southeast region of Brazil, and the second grid was refined over the coastal area.
WAVE MODEL 
•Two third generation models were used: WAVEWATCH III (WW3) and SWAN (Simulating WAves Nearshore) 
•Output results from WW3 were used as boundary conditions for SWAN’s local grid, in a chain from smaller to higher resolution grids. 
•The high resolution atmospheric pressure and wind fields from WRF outputs were also used for forcing the high resolution SWAN grids.
HYDRODYNAMIC MODEL 
•Delft3D-FLOW Hydrodynamic Model was implemented in Angra dos Reis - Ilha Grande Bay; 
•Delft3D-FLOW ran in a Domain Decomposition scheme: 
The outside grid (lower resolution grid) had 126 x 68 grid cells and the high resolution grid had 104 x 86 grid cells 
Horizontal resolution ranging from 1 kilometer to 300 meters 
On the vertical axis 10 sigma layers have been used 
High resolution bathymetric data was imposed in the operations region
Hydrodynamic Forcing 
•Meteorological forcing: outputs from the atmospheric model WRF; 
•40 Riemann Boundaries (south, east and west) * 10 sigma layers HYCOM + TPXO composition 
Riemann Invariants enable Delft3D to capture the continental shelf dynamics and incorporate low frequency signs
Riemann Invariants 
25 Riemann Boundaries 
8 Riemann Boundaries 
7 Riemann Boundaries 
HYCOM (daily water level and currents) + TPXO 10 sigma layers
OPERATIONAL PROCEDURE FOR DELFT3D 
•WRF (wind and pressure) and HYCOM (currents and elevation) files are obtained from the FTP directory; 
•The forcing (.bct and meteo) files for Delft3D are generated; 
•The .mdf scenario is created; 
•The restart files are copied from the last run (from 12 hours later); 
•New scenario runs; 
•The output files are generated by Quickplot; 
•The output files are copied to the FTP. 
A matlab script runs all the specified above twice a day.
MODEL EVALUATION 
•The model was calibrated and validated through the comparison of its results against measured data and tidal prediction 
•Tides (tidal prediction Angra dos Reis station) 
RMAE 20 
Index of Agreement 0,99
MODEL EVALUATION 
•Currents (ADCP) 
At this point there is a clockwise current with some inversions to counter clockwise 
The model represents this pattern coherently
Riemann Tide 
Index of agreement U comp. = 0,68 
Index of agreement V comp. = 0,64 
Index of agreement U comp. = 0,32 Index of agreement V comp. = 0,40
CONCLUSIONS 
•Delft3D system was successfully applied at the study area and proved to be a rugged tool, able to perform the coupling with HYCOM; 
•Without using HYCOM results the system was not able to represent the circulation pattern of the area; 
•The coupling between the numerical grids using domain decomposition technique solved properly the circulation dynamic  at the boundaries we used a lower resolution (outside the bay, where there are HYCOM results) and at the study area we used a higher resolution (2nd grid).
Eduardo Yassuda Eduardo.yassuda@tetratech.com Clarissa Brelinger De Luca Clarissa.deluca@tetratech.com Maria Fernanda Mendes Fiedler Fernanda.fiedler@tetratech.com TETRA TECH BRASIL Engenharia Costeira & Oceanografia Tel: +55 11 3095-5050 Rua Fidalga, 711 | São Paulo, SP 05432-070 | www.tetratech.com 
Contato:

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DSD-INT 2014 - Delft3D Users Meeting - Application of Delft3D in an Operational Forecasting System, Clarissa De Luca, Tetra Tech Brasil

  • 1. www.tetratech.com Weather Forecasting Services during Marine Operations in the Angra dos Reis Bay (RJ) Application of Delft3D in an Operational Forecasting System Delft3D Users Meeting 2014
  • 2. INTRODUCTION •In support for marine operations in Angra dos Reis Bay, Tetra Tech performed forecasting services of meteoceanographic conditions; •Forecasts were obtained through a refined operational modeling system, coupling atmospheric and oceanic components; •Local measurements of atmospheric, hydrodynamic and wave parameters were used to validate the numerical modeling products prior to the start of operations; •During the marine operations period forecasting bulletins were provided with updating intervals of 12 hours.
  • 3. STUDY LOCATION •The Ilha Grande Bay is located in the Southern coast of the state of Rio de Janeiro; •This region has great importance ecologically, for tourism and for the fishing industry, holding biological reserves and environmentally protected areas; •On the coast, besides the Central Nuclear Almirante Álvaro Alberto – CNAAA (Nuclear Central Almirante Álvaro Alberto), there are shipyard industries.
  • 5. CIRCULATION PATTERNS •According to Signorini (1980) The circulation of the partially mixed estuarine system, formed by the Ilha Grande Bay (IGB) and Sepetiba Bay (SEPB), results from effects of tides, winds and density gradients. It can be observed the presence of a clockwise (west-east) flux around Ilha Grande. •The measured currents show a clockwise (54,6% to E) and a counter-clockwise flux (41,2% to W).
  • 6. OPERATIONAL PROCEDURE •Bulletin updates were sent twice a day with forecasts for the following 72 hours of the environmental conditions predicted by the modeling system •An alert system was implemented in the bulletins, indicating when the forecasted environmental conditions were according to established thresholds for the execution of transport and lifting procedures. The threshold values were given by the contractor for each procedure as: Conditions for transport: •Wind speed ≤ 14 knots •Current speed ≤ 0.3 m/s •Wave peak period (Tp) ≤ 10 s •Significant wave height (Hs) ≤ 0.3 m Conditions for lifting: •Wind speed ≤ 10 knots •Wave peak period (Tp) ≤ 7 s •Significant wave height (Hs) ≤ 0.3 m
  • 9. NUMERICAL MODELS •The operational procedure to generate the metocean forecasts in the Angra dos Reis Bay region was composed with three kinds of numerical models: Atmospheric model (WRF) Two wave models (WW3 and SWAN) Hydrodynamic model (Delft3D)
  • 10. ATMOSPHERIC MODEL •WRF (Weather Reserch and Forecasting) NMM core (Nonhydrostatic Mesoscale Model), developed by north American centers NOAA and NCEP. Forced with global model data from the GFS (Global Forecasting System), with spatial resolution of 0.5° and 3- hour intervals. The GFS was developed and is maintained by NCEP, with online available outputs in the spatial and temporal resolution mentioned. The WRF-NMM model was setup with two nested grids. The coarser domain covered the Southeast region of Brazil, and the second grid was refined over the coastal area.
  • 11.
  • 12. WAVE MODEL •Two third generation models were used: WAVEWATCH III (WW3) and SWAN (Simulating WAves Nearshore) •Output results from WW3 were used as boundary conditions for SWAN’s local grid, in a chain from smaller to higher resolution grids. •The high resolution atmospheric pressure and wind fields from WRF outputs were also used for forcing the high resolution SWAN grids.
  • 13.
  • 14. HYDRODYNAMIC MODEL •Delft3D-FLOW Hydrodynamic Model was implemented in Angra dos Reis - Ilha Grande Bay; •Delft3D-FLOW ran in a Domain Decomposition scheme: The outside grid (lower resolution grid) had 126 x 68 grid cells and the high resolution grid had 104 x 86 grid cells Horizontal resolution ranging from 1 kilometer to 300 meters On the vertical axis 10 sigma layers have been used High resolution bathymetric data was imposed in the operations region
  • 15.
  • 16. Hydrodynamic Forcing •Meteorological forcing: outputs from the atmospheric model WRF; •40 Riemann Boundaries (south, east and west) * 10 sigma layers HYCOM + TPXO composition Riemann Invariants enable Delft3D to capture the continental shelf dynamics and incorporate low frequency signs
  • 17. Riemann Invariants 25 Riemann Boundaries 8 Riemann Boundaries 7 Riemann Boundaries HYCOM (daily water level and currents) + TPXO 10 sigma layers
  • 18. OPERATIONAL PROCEDURE FOR DELFT3D •WRF (wind and pressure) and HYCOM (currents and elevation) files are obtained from the FTP directory; •The forcing (.bct and meteo) files for Delft3D are generated; •The .mdf scenario is created; •The restart files are copied from the last run (from 12 hours later); •New scenario runs; •The output files are generated by Quickplot; •The output files are copied to the FTP. A matlab script runs all the specified above twice a day.
  • 19. MODEL EVALUATION •The model was calibrated and validated through the comparison of its results against measured data and tidal prediction •Tides (tidal prediction Angra dos Reis station) RMAE 20 Index of Agreement 0,99
  • 20. MODEL EVALUATION •Currents (ADCP) At this point there is a clockwise current with some inversions to counter clockwise The model represents this pattern coherently
  • 21.
  • 22. Riemann Tide Index of agreement U comp. = 0,68 Index of agreement V comp. = 0,64 Index of agreement U comp. = 0,32 Index of agreement V comp. = 0,40
  • 23. CONCLUSIONS •Delft3D system was successfully applied at the study area and proved to be a rugged tool, able to perform the coupling with HYCOM; •Without using HYCOM results the system was not able to represent the circulation pattern of the area; •The coupling between the numerical grids using domain decomposition technique solved properly the circulation dynamic  at the boundaries we used a lower resolution (outside the bay, where there are HYCOM results) and at the study area we used a higher resolution (2nd grid).
  • 24. Eduardo Yassuda Eduardo.yassuda@tetratech.com Clarissa Brelinger De Luca Clarissa.deluca@tetratech.com Maria Fernanda Mendes Fiedler Fernanda.fiedler@tetratech.com TETRA TECH BRASIL Engenharia Costeira & Oceanografia Tel: +55 11 3095-5050 Rua Fidalga, 711 | São Paulo, SP 05432-070 | www.tetratech.com Contato: