
| Spatial Extent | North America |
| Spatial Resolution | 12 km |
| Time Period | 1996-2002 |
| Temporal Resolution | Hourly |
| Land Surface Models | MOSAIC, CLM, NOAH, Catchment |
| Atmospheric Model | NCEP's 12km Eta |
| Output Format | GRIB |
| Grid Characteristics |
|---|
| Note: |
| The rotation of the latitude/longitude grid is such that the intersection of the "prime meridian" and the "equator" has been located at the central latitude and longitude of the area represented. |
NLDAS-E and the Eta model use the semi-staggered Arakawa E grid (see visual below). Prognostic variables at mass (H) points are surface pressure, temperature, and specific humidity. Zonal and meridional wind components are carried at velocity (V) points. The E grid is mapped to a rotated latitude-longitude grid which is centered at 50N and 111W for the current operational Eta with 12 km resolution. Two rotations are involved. One moves the Greenwich meridian to 111 W, and the second shifts the equator to 50 N. Each row of the E grid lies along a line of constant rotated latitude; each column lies along a line of constant rotated longitude.
The 12km Eta grid representation in GRIB follows a 2-D grid format, whereby the grid is staggered row by row, wind and mass, and the same number of points (1211) are in each row. 606 (605) mass points exist on odd (even) rows, and vice versa for wind points.
Staggered, 2-D E-grid indexing
3 H V H V H V H (V)
J 2 V H V H V H V (H)
1 H V H V H V H (V) () points are "extra"
\ / \ / \ / \ / included in grid but not
1 2 3 4 used in integration
I
Data Representation Type 203 - Arakawa staggered E-grid on rotated
latitude/longitude grid

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LDAS
Web PageDeveloped and Maintained at NASA/GSFC | Matthew
Rodell: Matthew.Rodell@gsfc.nasa.gov Brian Cosgrove: Brian.Cosgrove@gsfc.nasa.gov | ![]() |