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TREND1D(1)		     Generic Mapping Tools		    TREND1D(1)

NAME
       trend1d - Fit a [weighted] [robust] polynomial [or Fourier] model for y
       = f(x) to xy[w] data.

SYNOPSIS
       trend1d -Fxymrw -N[f]n_model[r] [ xy[w]file ] [ -Ccondition_number ]  [
       -H[i][nrec]  ]  [  -I[confidence_level]	]  [ -V ] [ -W ] [ -:[i|o] ] [
       -b[i|o][s|S|d|D[ncol]|c[var1/...]] ] [ -f[i|o]colinfo ]

DESCRIPTION
       trend1d reads x,y [and w] values from the first two [three] columns  on
       standard	 input [or xy[w]file] and fits a regression model y = f(x) + e
       by [weighted] least squares.  The functional form of f(x) may be chosen
       as  polynomial  or Fourier, and the fit may be made robust by iterative
       reweighting of the data.	 The user may also search for  the  number  of
       terms in f(x) which significantly reduce the variance in y.

REQUIRED ARGUMENTS
       -F     Specify up to five letters from the set {x y m r w} in any order
	      to create columns of ASCII [or binary] output.  x = x, y = y,  m
	      = model f(x), r = residual y - m, w = weight used in fitting.

       -N     Specify  the  number  of terms in the model, n_model, whether to
	      fit a Fourier (-Nf) or polynomial [Default] model, and append  r
	      to do a robust fit.  E.g., a robust quadratic model is -N3r.

OPTIONS
       xy[w]file
	      ASCII  [or binary, see -b] file containing x,y [w] values in the
	      first 2 [3] columns.  If no file is specified, trend1d will read
	      from standard input.

       -C     Set  the	maximum	 allowed condition number for the matrix solu‐
	      tion.  trend1d fits a damped least squares model, retaining only
	      that  part of the eigenvalue spectrum such that the ratio of the
	      largest eigenvalue to the smallest  eigenvalue  is  condition_#.
	      [Default:	 condition_# = 1.0e06. ].

       -H     Input file(s) has header record(s).  If used, the default number
	      of header records is N_HEADER_RECS.  Use -Hi if only input  data
	      should  have  header  records  [Default  will  write  out header
	      records if the input data have  them].  Blank  lines  and	 lines
	      starting with # are always skipped.

       -I     Iteratively increase the number of model parameters, starting at
	      one, until n_model is reached or the reduction  in  variance  of
	      the model is not significant at the confidence_level level.  You
	      may set -I only, without an attached number; in  this  case  the
	      fit  will	 be iterative with a default confidence level of 0.51.
	      Or choose your own level between 0 and 1.	 See remarks section.

       -V     Selects verbose mode, which will send progress reports to stderr
	      [Default runs "silently"].

       -W     Weights  are  supplied  in  input column 3.  Do a weighted least
	      squares fit [or start with these weights when doing  the	itera‐
	      tive robust fit].	 [Default reads only the first 2 columns.]

       -:     Toggles  between	(longitude,latitude)  and (latitude,longitude)
	      input and/or output.  [Default is (longitude,latitude)].	Append
	      i	 to  select  input  only or o to select output only.  [Default
	      affects both].

       -bi    Selects binary input.  Append s for single precision [Default is
	      d	 (double)].   Uppercase	 S  or	D  will	 force	byte-swapping.
	      Optionally, append ncol, the number of columns  in  your	binary
	      input  file if it exceeds the columns needed by the program.  Or
	      append c	if  the	 input	file  is  netCDF.  Optionally,	append
	      var1/var2/...  to specify the variables to be read.  [Default is
	      2 (or 3 if -W is set) columns].

       -bo    Selects binary output.  Append s for single  precision  [Default
	      is  d  (double)].	  Uppercase  S	or D will force byte-swapping.
	      Optionally, append ncol, the number of desired columns  in  your
	      binary output file.  [Default is 1-5 columns as given by -F].

       -f     Special  formatting of input and/or output columns (time or geo‐
	      graphical data).	Specify i or o to  make	 this  apply  only  to
	      input  or	 output	 [Default  applies to both].  Give one or more
	      columns (or column ranges) separated by commas.  Append T (abso‐
	      lute  calendar time), t (relative time in chosen TIME_UNIT since
	      TIME_EPOCH), x (longitude), y (latitude), or f (floating	point)
	      to  each	column or column range item.  Shorthand -f[i|o]g means
	      -f[i|o]0x,1y (geographic coordinates).

ASCII FORMAT PRECISION
       The ASCII output formats of numerical data are controlled by parameters
       in  your	 .gmtdefaults4	file.	Longitude  and	latitude are formatted
       according to OUTPUT_DEGREE_FORMAT, whereas other values	are  formatted
       according  to D_FORMAT.	Be aware that the format in effect can lead to
       loss of precision in the output, which can  lead	 to  various  problems
       downstream.   If	 you find the output is not written with enough preci‐
       sion, consider switching to binary output (-bo if available) or specify
       more decimals using the D_FORMAT setting.

REMARKS
       If  a  Fourier  model  is selected, the domain of x will be shifted and
       scaled to [-pi, pi] and the basis functions used	 will  be  1,  cos(x),
       sin(x),	cos(2x), sin(2x), ...	If a polynomial model is selected, the
       domain of x will be shifted and scaled to [-1, 1] and the  basis	 func‐
       tions  will be Chebyshev polynomials.  These have a numerical advantage
       in the form of the matrix which must be inverted and allow  more	 accu‐
       rate  solutions.	  The Chebyshev polynomial of degree n has n+1 extrema
       in [-1, 1], at all of which its value is either -1  or  +1.   Therefore
       the magnitude of the polynomial model coefficients can be directly com‐
       pared.  NOTE: The stable model coefficients are Chebyshev coefficients.
       The  corresponding  polynomial  coefficients in a + bx + cxx + ...  are
       also given in Verbose mode but users must realize  that	they  are  NOT
       stable beyond degree 7 or 8. See Numerical Recipes for more discussion.
       For evaluating Chebyshev polynomials, see gmtmath.

       The -Nr (robust) and -I (iterative) options evaluate  the  significance
       of  the	improvement  in	 model	misfit	Chi-Squared by an F test.  The
       default confidence limit is set at 0.51; it can be changed with the  -I
       option.	 The  user  may	 be  surprised	to find that in most cases the
       reduction in variance achieved by increasing the number of terms	 in  a
       model  is  not  significant  at	a very high degree of confidence.  For
       example, with 120 degrees of freedom, Chi-Squared must decrease by  26%
       or  more to be significant at the 95% confidence level.	If you want to
       keep iterating  as  long	 as  Chi-Squared  is  decreasing,  set	confi‐
       dence_level to zero.

       A low confidence limit (such as the default value of 0.51) is needed to
       make the robust method work.  This  method  iteratively	reweights  the
       data  to	 reduce the influence of outliers.  The weight is based on the
       Median Absolute Deviation and a formula from Huber [1964], and  is  95%
       efficient  when the model residuals have an outlier-free normal distri‐
       bution.	This means that the influence  of  outliers  is	 reduced  only
       slightly	 at  each iteration; consequently the reduction in Chi-Squared
       is not very significant.	 If the procedure needs a  few	iterations  to
       successfully  attenuate	their  effect, the significance level of the F
       test must be kept low.

EXAMPLES
       To remove a linear trend from data.xy by ordinary least squares, use:

       trend1d data.xy -F xr -N 2 > detrended_data.xy

       To make the above linear trend robust with respect to outliers, use:

       trend1d data.xy -F xr -N 2r > detrended_data.xy

       To find out how many terms (up to 20, say) in a robust  Fourier	inter‐
       polant are significant in fitting data.xy, use:

       trend1d data.xy -Nf 20r -I -V

SEE ALSO
       GMT(1), gmtmath(1), grdtrend(1), trend2d(1)

REFERENCES
       Huber,  P.  J.,	1964,  Robust estimation of a location parameter, Ann.
       Math. Stat., 35, 73-101.

       Menke, W., 1989, Geophysical Data Analysis:  Discrete  Inverse  Theory,
       Revised Edition, Academic Press, San Diego.

GMT 4.5.14			  1 Nov 2015			    TREND1D(1)
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