
wgt_volave_ccm
Calculates the volume average of a quantity from the CCM using weights.
Prototype
function wgt_volave_ccm ( q : numeric, wgtz : numeric, wgty [*] : numeric, wgtx [*] : numeric, opt : integer ) return_val : float or double
Arguments
qAn array of 3 or more dimensions containing the data to be averaged. The rightmost dimensions should correspond to "level" (lev), "latitude" (lat), and "longitude" (lon) when dealing with quantities on a sphere ([...,],lev,lat,lon), and "z", "y", and "x" otherwise ([...,],z,y,x).
wgtzAn array dimensioned the same size as q for the atmospheric component of the CCM. Typically, this will be the "delta-pressures" as calculated by NCL's dpres_hybrid_ccm function.
wgtyA scalar (typically 1.0) or 1-dimensional array of size "lat" (y) containing the weights.
wgtxA scalar (typically 1.0) or 1-dimensional array of size "lon" (x) containing the weights.
optIf opt = 0, the area average is calculated using available non-missing data. If opt = 1, then if any point in q is missing, the area average is not computed. In this case, it will be set to the missing value, which is indicated by q@_FillValue, or the default missing value if q@_FillValue is not set.
Return value
Returns a scalar if q is a two dimensional array. Otherwise, the output dimensionality is the same as the leftmost dimensions of the input q.
The return type is floating point if the input is floating point, and double if the input is of type double.
Description
This function computes the volume average of a quantity from the CCM using weights.
See Also
wgt_areaave, wgt_areaave2, wgt_arearmse, wgt_arearmse2, wgt_areasum2, wgt_runave, wgt_volave, wgt_volrmse, wgt_volrmse_ccm
Examples
Example 1
Let q(time, lev, lat, lon) be a global array with dimension sizes ktime = 120, nlev = 28, nlat = 64, mlon = 128 and wgtp(ktime, nlev, nlat, mlon) be an array containing the "delta-pressures" as computed by the NCL function dpres_hybrid_ccm. Let wgty(nlat) be a 1-dimensional array containing gaussian or cosine weights. Assume that no special weighting is applied in the longitude (x) direction. Then:
p0 = 100000.0 hyai = f->hyai hyai = f->hyai ps = f->PS wgty = f->gwt wgtx = 1.0 wgtp = dpres_hybrid_ccm(ps, p0, hyai, hybi) glAve = wgt_volave_ccm(q, wgtp, wgty, 1.0, 0) ; glAve(ktime) delete (wgtp)or
glAve = wgt_volave_ccm (q, dpres_hybrid_ccm(ps,p0,hyai,hybi), wgty, 1.0, 0)will calculate the volume (global) average for each time. glAve will be a 1-dimensional array with dimension (ktime = 120). If a missing value is encountered at any of the two rightmost dimensions, then the result will be set to q@_FillValue (opt = 0).
Example 2
nhAve = wgt_volave_ccm(q(:, :, 33:nlat - 1,:), wgtp(:, :, 33:nlat - 1, :), \ wgty(33:nlat), 1.0, 1)will calculate the volume (northern hemisphere) average for each time and level. Standard subscripting is used to subset the input global array. nhAve will be a 1-dimensional array with dimension (ktime = 120). If a missing value is encountered at any of the two rightmost dimension, it is ignored (equivalent to a weight of 0.0) and the average is calculated using available non-missing data (opt = 1).
Example 3
Same as above but q, wgtz and wgty must have named dimensions and coordinate variables.
shAve = wgt_volave_ccm(q(:, 5:7, {lat | -90:0}, :), wgtz(:, 5:7, {lat | -90:0}), \ wgty({lat | -90:0}), 1.0, 0)will calculate the volume (southern hemisphere) average for each time using levels = 5, 6, 7. Named subscripting and standard subscripting are used to subset the input global array. shAve will have dimension (ktime).