Date: 29 January 2026
Attendees: @ezhilsabareesh8, @NoahDay, @sofarrell, @alberto
Chair & Minutes: @ezhilsabareesh8
1. ERA5 Forcing & Standalone WW3
- ERA5 used as primary wind input for standalone WW3.
- PR1 propagation scheme may be contributing to wave behaviour issues.
- Use ERA5 neutral wind speed, which corrects for atmospheric instabilities.
- Corrected ECMWF ERA5 dataset expected Q2 2026.
2. Wave–Current Interaction
- Currents influence wave energy balance and redistribute energy across frequency bands.
- Mean wave period biases may be caused by Doppler shifting from currents.
- MOM6 current representation quality requires assessment.
- Standalone WW3 should be tested with and without current forcing (e.g., ACCESS‑OM2 currents).
3. Excessive Low‑Frequency Dissipation
- Too much dissipation observed in low‑frequency bands, likely from strong refraction in swell regions.
- ST6 parameters, tuned for uncoupled WW3, may require retuning for coupled model.
4. Unresolved Obstacles Impacting Wave Biases
- Significant wave height (Hs) biases appear near small islands and unresolved bathymetric features.
- Dissipation parameterisation for unresolved obstacles should be explored.
5. Directional Spectra Evaluation
Directional spectra comparisons to be conducted with:
- WHACS dataset
CSIRO Data Access Portal - Southern Ocean Time Series (SOTS) directional spectra
- NDBC deep‑water buoys (offshore stations)
6. Wave–Ice Considerations
- Consider inclusion of ERA5 sea‑ice concentration in standalone WW3.
- Compare attenuation behaviour for solid vs broken ice regimes.
7. Mixing & MOM6 Diagnostics
Ezhil’s tests indicate that WW3 EFACTOR improves MLD performance in MOM6 over:
- KPP (no waves)
- ePBL
Add the following vertical mixing diagnostics to MCW KPP runs (with and without EFACTOR):
diff_cbt_t # vertical heat diffusivity
diff_cbt_s # vertical salt diffusivity
diff_cbt_back # background tracer diffusivity
diff_cbt_tides # tidal tracer diffusivity
8. Action Items
8.1 Wave Model Evaluation (Ezhil)
- Run standalone WW3 (ERA5 winds) and compare with:
- WHACS
- SOTS directional spectra
- NDBC offshore buoys
- Analyse PR1 propagation scheme.
- Test WW3 with/without currents.
- Investigate low‑frequency dissipation & refraction.
- Evaluate WW3 wind‑correction switches.
- Develop parameterisation for unresolved obstacles.
8.2 Data & Forcing (Ezhil)
- Use ERA5 neutral wind speeds.
- Assess feasibility of ERA5 sea‑ice concentration.
8.3 Wave–Ice Coupling (Noah)
- Compare broken vs solid ice attenuation regimes.
- Validate model against ice‑affected directional spectra.
- Compare attenuation with CICE wave forcing
- Evaluate fast‑ice vs broken‑ice behaviour
- Optimise breakup scheme