Coriolis Operators
Coriolis force operators for rotating-frame geophysical models on C-grids.
finitevolx.Coriolis2D
Bases: Module
Coriolis force operator for 2-D Arakawa C-grids.
Computes the Coriolis tendency for both velocity components:
du_cor[j, i+1/2] = +f_on_u[j, i+1/2] * v_on_u[j, i+1/2]
dv_cor[j+1/2, i] = -f_on_v[j+1/2, i] * u_on_v[j+1/2, i]
The Coriolis parameter f is interpolated from T-points to velocity points
using simple x/y averaging. The cross-face velocity averages are computed
with 4-point bilinear interpolation (same as :class:Interpolation2D).
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
grid
|
ArakawaCGrid2D
|
The underlying 2-D grid. |
required |
Examples:
>>> import jax.numpy as jnp
>>> from finitevolx import ArakawaCGrid2D, Coriolis2D
>>> grid = ArakawaCGrid2D.from_interior(8, 8, 1.0, 1.0)
>>> cor = Coriolis2D(grid=grid)
>>> u = jnp.zeros((grid.Ny, grid.Nx))
>>> v = jnp.ones((grid.Ny, grid.Nx))
>>> f = jnp.ones((grid.Ny, grid.Nx))
>>> du_cor, dv_cor = cor(u, v, f)
Source code in finitevolx/_src/operators/coriolis.py
__call__(u, v, f, mask=None)
Coriolis tendencies (du_cor, dv_cor).
du_cor[j, i+1/2] = +f_on_u * v_on_u dv_cor[j+1/2, i] = -f_on_v * u_on_v
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
u
|
Float[Array, 'Ny Nx']
|
x-velocity at U-points (east faces). |
required |
v
|
Float[Array, 'Ny Nx']
|
y-velocity at V-points (north faces). |
required |
f
|
Float[Array, 'Ny Nx']
|
Coriolis parameter at T-points. |
required |
mask
|
ArakawaCGridMask or None
|
Optional land/ocean mask. If provided, |
None
|
Returns:
| Type | Description |
|---|---|
tuple[Float[Array, 'Ny Nx'], Float[Array, 'Ny Nx']]
|
|
Source code in finitevolx/_src/operators/coriolis.py
finitevolx.Coriolis3D
Bases: Module
Coriolis force operator for 3-D Arakawa C-grids.
Applies the same horizontal Coriolis stencil as :class:Coriolis2D
independently at each z-level. The Coriolis parameter f is 2-D
(depth-independent) and broadcast over all z-levels.
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
grid
|
ArakawaCGrid3D
|
The underlying 3-D grid. |
required |
Examples:
>>> import jax.numpy as jnp
>>> from finitevolx import ArakawaCGrid3D, Coriolis3D
>>> grid = ArakawaCGrid3D.from_interior(6, 6, 4, 1.0, 1.0, 1.0)
>>> cor = Coriolis3D(grid=grid)
>>> u = jnp.zeros((grid.Nz, grid.Ny, grid.Nx))
>>> v = jnp.ones((grid.Nz, grid.Ny, grid.Nx))
>>> f = jnp.ones((grid.Ny, grid.Nx))
>>> du_cor, dv_cor = cor(u, v, f)
Source code in finitevolx/_src/operators/coriolis.py
124 125 126 127 128 129 130 131 132 133 134 135 136 137 138 139 140 141 142 143 144 145 146 147 148 149 150 151 152 153 154 155 156 157 158 159 160 161 162 163 164 165 166 167 168 169 170 171 172 173 174 175 176 177 178 179 180 181 182 183 184 185 186 187 188 189 190 191 192 193 194 195 196 197 198 199 | |
__call__(u, v, f, mask=None)
Coriolis tendencies over all z-levels.
du_cor[k, j, i+1/2] = +f_on_u[j, i+1/2] * v_on_u[k, j, i+1/2] dv_cor[k, j+1/2, i] = -f_on_v[j+1/2, i] * u_on_v[k, j+1/2, i]
Parameters:
| Name | Type | Description | Default |
|---|---|---|---|
u
|
Float[Array, 'Nz Ny Nx']
|
x-velocity at U-points. |
required |
v
|
Float[Array, 'Nz Ny Nx']
|
y-velocity at V-points. |
required |
f
|
Float[Array, 'Ny Nx']
|
Coriolis parameter at T-points (depth-independent). |
required |
mask
|
ArakawaCGridMask or None
|
Optional land/ocean mask. If provided, |
None
|
Returns:
| Type | Description |
|---|---|
tuple[Float[Array, 'Nz Ny Nx'], Float[Array, 'Nz Ny Nx']]
|
|