GrADS Function: gr2stn

## gr2stn()

This function is a grid-to-station interpolator. It creates "station" data result by sampling a gridded data set and interpolating to a given location. That location may be provided by specifying a longitude and a latitude, or by providing a station expression.

### Syntax

`gr2stn(grid_expr, stn_expr, <-n>)`
or
`gr2stn(grid_expr, lon, lat, <-n>)`

where:

`grid_expr` is a GrADS expression that gives a grid result. The interpolation will be done on this data. The `grid_expr`may be a 2-D grid that varies in X and Y, or a 1-D grid that varies in Z or T.

`stn_expr` is a GrADS expression that gives a station data result. The interpolation will be done to the station locations, the station data values are not used.

`lon,lat` may be used instead of `stn_expr` to specify the location to which the gridded data will be interpolated (see Usage Note #3.)

(Version 2.0.a6 or later) The `-n` option was added to return the nearest neighbor to the station location instead of the bi-linear interpolation of the four surrounding grid points.

### Usage Notes

1. The result of the function is station data.
2. If `grid_expr` is a 2-D grid that varies in X and Y, then `stn_expr` should also be a 2-D expression that has multiple stations in the lat/lon domain. The result will be a station data set, with values interpolated from `grid_expr` to the station locations.
3. If `grid_expr` is a 1-D grid, then only Z or T can be the varying dimension. In this case, `stn_expr` should be an expression that has a single location, such as "temp(stid=kdca)". Alternatively, you may provide exact longitude and latitude values.
4. By default, the interpolation is done bi-linearly within the grid space. No weighting is done to account for real-world coordinate systems. If any of the four grid points around the station location are missing, the result will also be missing.
5. As of version 2.0.a6, the -n option may be used to return the nearest grid point value instead of the bi-linearly interpolated value.
6. See the section of the User's Guide on Arbitrary Cross Sections for more information on applications of `gr2stn`.

### Examples

1. To examine the difference between an analysis (ie, gridded data) and the original observations, one could:
     `d t.3-gr2stn(t.1,t.3)`

     where file 1 is gridded data, and file 3 is station data. The result would display as differences at the station locations.

2. If one wanted to display the difference calculated in Example 1 as a contour field, one can use the `oacres` function to do a quick analysis of the station values:
     `d oacres(t.1,t.3-gr2stn(t.1,t.3))`