Meteorological Forcing
Cocoa supports atmospheric forcing from wind fields and surface pressure data for storm surge and other weather-driven simulations. Forcing data is read from external files, interpolated onto the computational mesh, and applied at each timestep.
Overview
Meteorological forcing in Cocoa includes two components:
Wind stress: Surface drag from 10-meter wind velocity, computed via the Garratt (1977) bulk drag law
Atmospheric pressure gradient: Barotropic forcing from spatially varying surface pressure
Both components are read from the same input file(s) and share a common temporal interpolation framework. See Meteorological Forcing for the mathematical formulation.
Supported File Formats
Cocoa supports three meteorological file formats through the cocoa_meteo
library:
Format |
Config Value |
Domains |
Description |
|---|---|---|---|
CF-compliant NetCDF |
|
Single |
Standard climate/forecast NetCDF with configurable variable names |
OWI ASCII |
|
Multiple |
ADCIRC-compatible paired pressure/wind ASCII files |
OWI NetCDF |
|
Multiple |
NetCDF variant of OWI with support for moving (vortex-tracking) grids |
The synonyms cf and netcdf (for cf_netcdf) and owi (for
owi_ascii) are also accepted.
Configuration
Meteorological forcing is configured in the forcing.meteorological section
of the YAML configuration file.
Enabling Meteorological Forcing
To enable meteorological forcing, set enabled: true and specify the file
format and path(s):
forcing:
meteorological:
enabled: true
format: cf_netcdf
filename: "path/to/meteo_data.nc"
ramp:
enabled: true
duration: 1d
The ramp section controls the global spinup ramp applied to both tidal and
meteorological forcing. To use a different ramp for meteorological forcing,
add an optional ramp subsection under forcing.meteorological:
forcing:
ramp:
enabled: true
duration: 5d # Applied to tidal forcing
meteorological:
enabled: true
format: cf_netcdf
filename: "path/to/meteo_data.nc"
ramp: # Optional: overrides forcing.ramp for met
enabled: true
duration: 1d # Shorter met ramp
When the forcing.meteorological.ramp section is absent, the global ramp
is used for both tidal and meteorological forcing.
CF NetCDF Format
forcing:
meteorological:
enabled: true
format: cf_netcdf
filename: "path/to/meteo_data.nc"
Optional variable name overrides:
By default, Cocoa expects the following NetCDF variable names. Override them
under a nested variables map if your data uses different conventions:
Key |
Default |
Description |
|---|---|---|
|
|
Mean sea level pressure variable name |
|
|
Eastward 10-m wind component |
|
|
Northward 10-m wind component |
|
|
Time coordinate variable |
|
|
Longitude coordinate variable |
|
|
Latitude coordinate variable |
Example with custom variable names:
forcing:
meteorological:
enabled: true
format: cf_netcdf
filename: "era5_data.nc"
variables:
pressure: "sp"
wind_u: "u10"
wind_v: "v10"
time: "time"
lon: "longitude"
lat: "latitude"
OWI ASCII Format
OWI ASCII uses paired pressure and wind files per domain. This is the traditional ADCIRC meteorological forcing format.
Single domain:
forcing:
meteorological:
enabled: true
format: owi_ascii
filenames:
- pressure: "path/to/fort.221"
wind: "path/to/fort.222"
Multiple nested domains:
forcing:
meteorological:
enabled: true
format: owi_ascii
filenames:
- pressure: "path/to/basin.pre"
wind: "path/to/basin.wnd"
- pressure: "path/to/region.pre"
wind: "path/to/region.wnd"
Domain 0 (first entry) is the outer coarse grid. Subsequent entries are progressively finer inner grids. Where grids overlap, the innermost valid domain takes priority.
OWI NetCDF Format
OWI NetCDF stores all domains in a single NetCDF file using group-based organization. It additionally supports moving (vortex-tracking) grids where the grid coordinates change at each time step.
forcing:
meteorological:
enabled: true
format: owi_netcdf
filename: "path/to/meteo_owi.nc"
Drag Law
The wind drag law used to convert 10-m wind velocity to surface stress is
selected with forcing.meteorological.drag_law. The only accepted value is
garratt (the Garratt 1977 bulk drag law), which is also the default:
forcing:
meteorological:
enabled: true
format: cf_netcdf
filename: "data.nc"
drag_law: garratt # default; only accepted value
Scale Factors
Cocoa applies configurable scale factors to convert raw file values to SI units (Pa for pressure, m/s for wind):
Parameter |
Default |
Description |
|---|---|---|
|
|
Multiplier for pressure values. Default converts hectopascals (hPa) to pascals (Pa). |
|
|
Multiplier for wind velocity values. Default assumes m/s input. |
Example for a dataset with pressure in Pa and wind in knots:
forcing:
meteorological:
enabled: true
format: cf_netcdf
filename: "data.nc"
pressure_scale: 1.0 # Already in Pa
wind_scale: 0.514444 # Convert knots to m/s
File Format Details
CF-Compliant NetCDF
The CF NetCDF reader expects a regular rectangular grid with the following structure:
Required dimensions and variables:
dimensions:
time = UNLIMITED ;
lat = <NY> ;
lon = <NX> ;
variables:
double time(time) ;
time:units = "hours since 2026-01-01 00:00:00" ;
time:calendar = "standard" ;
double lat(lat) ;
double lon(lon) ;
float mslp(time, lat, lon) ; // Surface pressure
float wind_u(time, lat, lon) ; // Eastward 10-m wind
float wind_v(time, lat, lon) ; // Northward 10-m wind
The time variable must use CF-compliant units (e.g.,
"hours since ..."or"seconds since ...")Longitude and latitude are 1D coordinate arrays defining the grid
Global grids (360° longitude span) are detected automatically; the reader handles wrap-around
OWI ASCII
OWI ASCII files use a fixed-width format with one pressure file and one wind file per domain.
File header (line 1):
Oceanweather WIN/PRE Format YYYYMMDDHH YYYYMMDDHH
The header line contains a format identifier, the start time, and the end time.
Snapshot header (one per time step):
iLat= NNNiLong= NNNdx=D.DDDDdy=D.DDDDSWLat=LL.LLLLLSWLon=LLL.LLLLDT=YYYYMMDDHHNN
Field |
Position |
Description |
|---|---|---|
|
cols 5-8 |
Number of latitude points (NY) |
|
cols 15-18 |
Number of longitude points (NX) |
|
cols 22-27 |
Longitude grid spacing [degrees] |
|
cols 31-36 |
Latitude grid spacing [degrees] |
|
cols 43-50 |
Southwest corner latitude [degrees] |
|
cols 57-64 |
Southwest corner longitude [degrees] |
|
cols 68-79 |
Snapshot time (YYYYMMDDHHNN) |
Data records:
Following each snapshot header, NX * NY floating-point values are written
in free format. Pressure files contain one field per snapshot; wind files
contain two fields (eastward U, then northward V).
OWI NetCDF
OWI NetCDF files use NetCDF groups to organize multi-domain data:
root group:
dimensions:
time = UNLIMITED ;
variables:
double time(time) ;
group: domain_0 {
dimensions:
node = <NX*NY> ;
variables:
double longitude(time, node) ;
double latitude(time, node) ;
float pressure(time, node) ;
float wind_u(time, node) ;
float wind_v(time, node) ;
}
group: domain_1 {
...
}
The per-domain coordinate arrays (longitude, latitude) vary with time,
enabling vortex-tracking grids that follow a storm center. For stationary
grids, the coordinates are the same at each time step.
Combining Meteorological and Tidal Forcing
Meteorological forcing is commonly used alongside tidal forcing for storm surge simulations. Both forcing types operate independently and can be configured together:
forcing:
ramp:
enabled: true
duration: 2d
meteorological:
enabled: true
format: cf_netcdf
filename: "hurricane_met.nc"
tide:
potential:
enabled: true
type: astronomical
boundary:
enabled: true
constituents:
- name: M2
frequency: 1.405189028e-04
nodal_factor: 0.964
equilibrium_arg: 23.06
boundary_values:
- { amplitude: 0.50, phase: 340.0 }
The ramp function is applied independently to tidal and meteorological components. If the simulation starts from a pre-spun-up tidal state, a shorter meteorological ramp avoids unnecessary delay:
forcing:
ramp:
enabled: true
duration: 5d # Long tidal spinup
meteorological:
enabled: true
format: cf_netcdf
filename: "hurricane_met.nc"
ramp:
enabled: true
duration: 12h # Short met ramp
Wind Reduction
Cocoa supports two complementary wind reduction mechanisms that modify wind velocity over land before computing wind stress. These are particularly important for storm surge simulations where overland wind fields need to account for surface roughness and canopy sheltering.
Both reductions are configured in the physics section and require
spatially-varying data from the mesh file. See
Wind Reduction for configuration details.
Directional Roughness Reduction
When surface_directional_roughness: mesh is specified, Cocoa applies
a direction-dependent wind reduction based on upwind land surface roughness.
This reproduces ADCIRC’s ApplyDirectionalWindReduction subroutine.
The algorithm:
Determines the wind direction at each node
Interpolates the land roughness length from the two nearest directional bins (12 bins at 30-degree spacing)
Computes the marine roughness from the current drag coefficient
Applies a reduction factor based on the roughness ratio
An overland flooding correction reduces the effective land roughness when
the total water depth exceeds twice the minimum depth threshold (h0),
accounting for the reduced influence of land surface features when they
are submerged.
Configuration:
physics:
surface_directional_roughness: mesh # Read from mesh file
The mesh file must contain the surface_directional_effective_roughness_length
variable with shape [num_nodes, 12]. See Mesh Preparation for
details on the mesh variable format.
Canopy Coefficient
When surface_canopy_coefficient: mesh is specified, wind velocity
components are multiplied by a per-node canopy sheltering factor before
stress computation. This represents wind attenuation under forest canopy.
Configuration:
physics:
surface_canopy_coefficient: mesh # Read from mesh file
The mesh file must contain the surface_canopy_coefficient variable with
shape [num_nodes] and values in the range [0, 1].
Processing Order
When meteorological forcing is active, the wind processing pipeline at each node follows this order:
Directional roughness (if enabled): Reduce wind based on upwind land roughness, using the drag coefficient computed from the pre-reduction wind speed
Canopy coefficient (if enabled): Multiply wind components by the canopy factor
Ramp: Scale wind by the meteorological ramp factor
Wind stress: Compute kinematic stress from the final (reduced, ramped) wind using the Garratt drag law
This ordering ensures that the directional roughness reduction uses the marine drag coefficient from the unreduced wind, the canopy reduction is applied as a simple multiplicative factor, and the ramp is applied last before stress computation.
Diagnostics
Cocoa tracks peak wind speed and minimum atmospheric pressure at each node over the course of the simulation. These peak values are written to the output file alongside the standard elevation and velocity fields, which is useful for post-processing storm surge maxima.
Complete Example
A storm surge simulation with OWI ASCII forcing on a regional mesh:
mesh:
filename: "gulf_mesh.nc"
projection:
type: "EquidistantCylindrical"
center: [-90.0, 25.0]
simulation:
start_time: 2026-08-01
end_time: 2026-08-10
time_step: 10s
initial_conditions:
water_level: 0.0
physics:
manning_n: mesh
tau0: mesh
cf_lower_limit: 0.001
smagorinsky_coefficient: 0.2
numeric:
solver: explicit
gwce_coefficients: [0.0, 1.0, 0.0]
forcing:
ramp:
enabled: true
duration: 2d
meteorological:
enabled: true
format: owi_ascii
filenames:
- pressure: "basin_scale.pre"
wind: "basin_scale.wnd"
- pressure: "inner_region.pre"
wind: "inner_region.wnd"
tide:
potential:
enabled: true
type: astronomical
boundary:
enabled: true
constituents:
- name: M2
frequency: 1.405189028e-04
nodal_factor: 0.964
equilibrium_arg: 23.06
boundary_values:
- { amplitude: 0.50, phase: 340.0 }
- { amplitude: 0.48, phase: 342.0 }
output:
filename: "surge_output.nc"
step_interval: 60
diagnostics:
screen_interval: 3600