I have generated this two dimensional random field:
This is done following this page. In particular, I have selected t=23 as dataframe and I have changed some parameters.
As you can noticed, I have selected some random points (50 points).You can also see that there are a lot of zero, a common problem with rain.
At this point I would like to reconstruct the random filed by means of kriging.
As first step, I have, if I have understood correctly, to compute the semivariogram. In addition, I would like also to apply the Normal Score Transformation (NST) in order to have a normal distribution.
The station data, reported in the table bellow, are then transform in a normal distribution. This is done by applying the following procedure:
I have sorted all the data; then I have computed the ECDF; then I used the values of the ECDF to compute the corresponding in the normal distribution by applying the inverse of the normal ECDF but by using as input the ECDF of the empirical data.
These are the two resulting semivariograms computed with or without the NST:
without:
with NST
Now, I have some questions?
- Is what I have done correct so far?
- Why do all data seem correlated after applying the NST?
- Why do I have so many oscillations in the semivariogram without the NST?
The value of the random field at station locations are:
x y value
4 24 0.00
5 8 0.00
6 28 2.52
7 17 2.39
8 9 0.00
12 32 0.87
14 30 3.47
14 46 0.72
17 15 1.98
17 41 0.40
18 41 0.89
19 17 0.92
20 27 12.72
21 10 0.00
21 11 0.00
21 17 5.66
21 29 2.11
21 36 7.81
22 43 0.07
23 4 0.00
26 11 0.00
26 40 1.96
27 21 2.30
29 10 0.00
29 36 1.04
30 26 4.95
31 30 4.75
32 30 6.79
33 5 0.00
35 14 1.16
35 18 1.93
35 34 8.35
35 35 4.21
35 42 0.07
35 45 0.05
36 7 0.68
36 11 0.85
36 47 0.00
37 19 0.01
39 5 0.00
40 11 0.00
40 21 0.01
40 33 1.29
42 40 0.00
43 37 0.00
45 32 0.09
46 33 0.00
48 4 0.00
48 24 0.61
48 25 0.11


