| ADVxHEFF |
Lateral advective flux of grid cell mean sea-ice thickness (HEFF) in the +x direction through the 'u' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +ADVxHEFF(i_g,j) corresponds to +x fluxes through the 'u' face of the tracer cell at (i,j,k=0). Also, the model +x direction does not necessarily correspond to the geographical east-west direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-729527.6 to 295912.66 |
1 |
N/A |
| ADVxSNOW |
Lateral advective flux of grid cell mean snow thickness (HSNOW) in the +x direction through the 'u' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +ADVxSNOW(i_g,j) corresponds to +x fluxes through the 'u' face of the tracer cell at (i,j,k=0). Also, the model +x direction does not necessarily correspond to the geographical east-west direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-160005.03 to 73332.49 |
1 |
N/A |
| ADVyHEFF |
Lateral advective flux of grid cell mean sea-ice thickness (HEFF) in the +y direction through the 'v' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +ADVyHEFF(i,j_g) corresponds to +y fluxes through the 'v' face of the tracer cell at (i,j,k=0). Also, the model +y direction does not necessarily correspond to the geographical north-south direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-465630.6 to 524431.75 |
1 |
N/A |
| ADVySNOW |
Lateral advective flux of grid cell mean snow thickness (HSNOW) in the +y direction through the 'v' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +ADVySNOW(i,j_g) corresponds to +y fluxes through the 'v' face of the tracer cell at (i,j,k=0). Also, the model +y direction does not necessarily correspond to the geographical north-south direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-118862.89 to 124844.65 |
1 |
N/A |
| DFxEHEFF |
Lateral diffusive flux of grid cell mean sea-ice thickness (HEFF) in the +x direction through the 'u' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +DFxEHEFF(i_g,j) corresponds to +x fluxes through the 'u' face of the tracer cell at (i,j,k=0). Also, the model +x direction does not necessarily correspond to the geographical east-west direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-10574.459 to 15488.656 |
1 |
N/A |
| DFxESNOW |
Lateral diffusive flux of grid cell mean snow thickness (HSNOW) in the +x direction through the 'u' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +DFxESNOW(i_g,j) corresponds to +x fluxes through the 'u' face of the tracer cell at (i,j,k=0). Also, the model +x direction does not necessarily correspond to the geographical east-west direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-2493.87 to 2504.412 |
1 |
N/A |
| DFyEHEFF |
Lateral diffusive flux of grid cell mean sea-ice thickness (HEFF) in the +y direction through the 'v' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +DFyEHEFF(i,j_g) corresponds to +y fluxes through the 'v' face of the tracer cell at (i,j,k=0). Also, the model +y direction does not necessarily correspond to the geographical north-south direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-10149.449 to 14223.013 |
1 |
N/A |
| DFyESNOW |
Lateral diffusive flux of grid cell mean snow thickness (HSNOW) in the +y direction through the 'v' face of the tracer cell on the native model grid. Note: in the Arakawa-C grid, horizontal flux quantities are staggered relative to the tracer cells with indexing such that +DFyESNOW(i,j_g,k) corresponds to +y fluxes through the 'v' face of the tracer cell at (i,j,k=0). Also, the model +y direction does not necessarily correspond to the geographical north-south direction because the x and y axes of the model's curvilinear lat-lon-cap (llc) grid have arbitrary orientations which vary within and across tiles. |
m3 s-1 |
float |
9.96921E+36 |
-2940.1846 to 3237.8535 |
1 |
N/A |
| i |
In the Arakawa C-grid system, tracer (e.g., THETA) and 'v' variables (e.g., VVEL) have the same x coordinate on the model grid. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| i_g |
In the Arakawa C-grid system, 'u' (e.g., UVEL) and 'g' variables (e.g., XG) have the same x coordinate on the model grid. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| j |
In the Arakawa C-grid system, tracer (e.g., THETA) and 'u' variables (e.g., UVEL) have the same y coordinate on the model grid. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| j_g |
In the Arakawa C-grid system, 'v' (e.g., VVEL) and 'g' variables (e.g., XG) have the same y coordinate. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| tile |
The ECCO V4 horizontal model grid is divided into 13 tiles of 90x90 cells for convenience. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| time |
center time of averaging period |
hours since 1992-01-01T12:00:00 |
int |
N/A |
N/A |
1 |
N/A |
| time_bnds |
Start and end times of averaging period. |
N/A |
int |
N/A |
N/A |
1 |
N/A |
| XC |
nonuniform grid spacing |
degrees_east |
float |
N/A |
N/A |
1 |
N/A |
| XC_bnds |
Bounds array follows CF conventions. XC_bnds[i,j,0] = 'southwest' corner (j-1, i-1), XC_bnds[i,j,1] = 'southeast' corner (j-1, i+1), XC_bnds[i,j,2] = 'northeast' corner (j+1, i+1), XC_bnds[i,j,3] = 'northwest' corner (j+1, i-1). Note: 'southwest', 'southeast', northwest', and 'northeast' do not correspond to geographic orientation but are used for convenience to describe the computational grid. See MITgcm dcoumentation for details. |
N/A |
float |
N/A |
N/A |
1 |
N/A |
| XG |
Nonuniform grid spacing. Note: 'southwest' does not correspond to geographic orientation but is used for convenience to describe the computational grid. See MITgcm dcoumentation for details. |
degrees_east |
float |
N/A |
N/A |
1 |
N/A |
| YC |
nonuniform grid spacing |
degrees_north |
float |
N/A |
N/A |
1 |
N/A |
| YC_bnds |
Bounds array follows CF conventions. YC_bnds[i,j,0] = 'southwest' corner (j-1, i-1), YC_bnds[i,j,1] = 'southeast' corner (j-1, i+1), YC_bnds[i,j,2] = 'northeast' corner (j+1, i+1), YC_bnds[i,j,3] = 'northwest' corner (j+1, i-1). Note: 'southwest', 'southeast', northwest', and 'northeast' do not correspond to geographic orientation but are used for convenience to describe the computational grid. See MITgcm dcoumentation for details. |
N/A |
float |
N/A |
N/A |
1 |
N/A |
| YG |
Nonuniform grid spacing. Note: 'southwest' does not correspond to geographic orientation but is used for convenience to describe the computational grid. See MITgcm dcoumentation for details. |
degrees_north |
float |
N/A |
N/A |
1 |
N/A |