uv2vrF_Wrap
Computes the vorticity via spherical harmonics, given the u and v wind components on a fixed grid (retains metadata).
Prototype
load "$NCARG_ROOT/lib/ncarg/nclscripts/csm/contributed.ncl" function uv2vrF_Wrap ( u : numeric, v : numeric ) return_val [dimsizes(u)] : float or double
Arguments
uv
wind components (input, arrays with two or more dimensions, last two dimensions must be nlat x nlon)
- input values must be in ascending latitude order
- input array must be on a global grid
Return value
A double array is returned if u or v are double; a float array is returned otherwise. The returned array will be of dimension size dimsizes (u).
Description
Given wind components u and v, uv2vrF_Wrap computes the vorticity and returns it as an array with the same dimensions as u and v (values will be in ascending latitude order). uv2vrF_Wrap operates on a fixed grid. This function is identical to the built-in function uv2vrF, except it retains metadata.
This function does not handle missing values (defined by the _FillValue attribute). If any missing values are encountered in a particular 2D input grid, then all of the values in the corresponding output grids will be set to the default missing value appropriate to the type of the output.
Note: For the arrays whose last two dimensions are nlat x nlon, the rest of the dimensions (if any) are collectively referred to as N. If the input/output arrays are just two dimensions, then N can either be considered equal to 1 or nothing at all.
Arrays which have dimensions N x nlat x nlon should not include the cyclic (wraparound) points when invoking the procedures and functions which use spherical harmonics (Spherepack).
If the input arrays u and v are on a gaussian grid, uv2vrG_Wrap should be used.
Note: if the input arrays are not global or contain missing data, then it is recommended that uv2vr_cfd be used.
See Also
uv2vrG_Wrap uv2vrG, uv2vrf, uv2vrg, uv2vrdvf, vr2uvF_Wrap, uv2vr_cfd, uv2vrdvf, uv2vrdvg
Examples
Example 1
Compute the vorticity given u and v on a fixed grid. Also, compute the rotational wind components.
begin
nlat = 73 ; dimensions
mlon = 144
mlon1 = mlon+1
fbfile = "uv300.hs"
nrec = fbinnumrec(fbfile) ; total number of records in the file
ntim = nrec/2 ; number of time steps in dataset
uvmsg = 1e+36
do i = 0,nrec-1,2
month = 1 ; January
if (i .ge. 2) then
month = 7 ; July
end if
work = fbinrecread(fbfile,i ,(/nlat,mlon1/),"float")
u = work(:,0:mlon-1)
work = fbinrecread(fbfile,i+1,(/nlat,mlon1/),"float")
v = work(:,0:mlon-1)
vr = uv2vrF_Wrap (u,v) ; u,v ==> vorticity (rel)
uvr = vr2uvF_Wrap (vr) ; vr ==> rotational wind components
end do
end
Errors
If jer or ker is equal to:
1 : error in the specification of nlat
2 : error in the specification of nlon
4 : error in the specification of N (jer only)