1GRDTREND(1) Generic Mapping Tools GRDTREND(1)
2
3
4
6 grdtrend - Fit and/or remove a polynomial trend in a grid file
7
9 grdtrend grdfile -Nn_model[r] [ -Ddiff.grd ] [ -Ttrend.grd ] [ -V ] [
10 -Wweight.grd ]
11
13 grdtrend reads a 2-D grid file and fits a low-order polynomial trend to
14 these data by [optionally weighted] least-squares. The trend surface
15 is defined by:
16
17 m1 + m2*x + m3*y + m4*x*y + m5*x*x + m6*y*y + m7*x*x*x + m8*x*x*y +
18 m9*x*y*y + m10*y*y*y.
19
20 The user must specify -Nn_model, the number of model parameters to use;
21 thus, -N4 fits a bilinear trend, -N6 a quadratic surface, and so on.
22 Optionally, append r to the -N option to perform a robust fit. In this
23 case, the program will iteratively reweight the data based on a robust
24 scale estimate, in order to converge to a solution insensitive to out‐
25 liers. This may be handy when separating a "regional" field from a
26 "residual" which should have non-zero mean, such as a local mountain on
27 a regional surface.
28
29 If data file has values set to NaN, these will be ignored during fit‐
30 ting; if output files are written, these will also have NaN in the same
31 locations.
32
33 No space between the option flag and the associated arguments.
34
35 grdfile
36 The name of a 2-D binary grid file.
37
38 -N [r]n_model sets the number of model parameters to fit. Append r
39 for robust fit.
40
42 No space between the option flag and the associated arguments.
43
44 -D Write the difference (input data - trend) to the file diff.grd.
45
46 -T Write the fitted trend to the file trend.grd.
47
48 -V Selects verbose mode, which will send progress reports to stderr
49 [Default runs "silently"].
50
51 -W If weight.grd exists, it will be read and used to solve a
52 weighted least-squares problem. [Default: Ordinary least-
53 squares fit.] If the robust option has been selected, the
54 weights used in the robust fit will be written to weight.grd.
55
57 The domain of x and y will be shifted and scaled to [-1, 1] and the
58 basis functions are built from Legendre polynomials. These have a
59 numerical advantage in the form of the matrix which must be inverted
60 and allow more accurate solutions. NOTE: The model parameters listed
61 with -V are Legendre polynomial coefficients; they are not numerically
62 equivalent to the m#s in the equation described above. The description
63 above is to allow the user to match -N with the order of the polynomial
64 surface. See grdmath if you need to evaluate the trend using the
65 reported coefficients.
66
68 By default GMT writes out grid as single precision floats in a COARDS-
69 complaint netCDF file format. However, GMT is able to produce grid
70 files in many other commonly used grid file formats and also facili‐
71 tates so called "packing" of grids, writing out floating point data as
72 2- or 4-byte integers. To specify the precision, scale and offset, the
73 user should add the suffix =id[/scale/offset[/nan]], where id is a two-
74 letter identifier of the grid type and precision, and scale and offset
75 are optional scale factor and offset to be applied to all grid values,
76 and nan is the value used to indicate missing data. When reading
77 grids, the format is generally automatically recognized. If not, the
78 same suffix can be added to input grid file names. See grdreformat(1)
79 and Section 4.17 of the GMT Technical Reference and Cookbook for more
80 information.
81
82 When reading a netCDF file that contains multiple grids, GMT will read,
83 by default, the first 2-dimensional grid that can find in that file. To
84 coax GMT into reading another multi-dimensional variable in the grid
85 file, append ?varname to the file name, where varname is the name of
86 the variable. Note that you may need to escape the special meaning of ?
87 in your shell program by putting a backslash in front of it, or by
88 placing the filename and suffix between quotes or double quotes. The
89 ?varname suffix can also be used for output grids to specify a variable
90 name different from the default: "z". See grdreformat(1) and Section
91 4.18 of the GMT Technical Reference and Cookbook for more information,
92 particularly on how to read splices of 3-, 4-, or 5-dimensional grids.
93
95 To remove a planar trend from hawaii_topo.grd and write result in
96 hawaii_residual.grd:
97
98 grdtrend hawaii_topo.grd -N3 -Dhawaii_residual.grd
99
100 To do a robust fit of a bicubic surface to hawaii_topo.grd, writing the
101 result in hawaii_trend.grd and the weights used in hawaii_weight.grd,
102 and reporting the progress:
103
104 grdtrend hawaii_topo.grd -N10r -Thawaii_trend.grd -Whawaii_weight.grd
105 -V
106
108 GMT(1), grdfft(1), grdfilter(1)
109
110
111
112GMT 4.5.6 10 Mar 2011 GRDTREND(1)