Page 370 - Contributed Paper Session (CPS) - Volume 7
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CPS2133 Alexander Schnurr et al.
                                all data            < -1.8              [-1.8,0)             [0,1.8)              > 1.8

                  (3,2,1)        25.96%     10.17%     18.59%      23.22%     23.26%
                  (1,2,3)        53.91%     29.67%     58.59%      57.60%     26.57%
                  (2,1,3)         4.97%      2.54%       4.92%      5.37%     20.30%
                  (3,1,2)         5.51%     27.12%       7.12%      4.26%      2.95%
                  (2,3,1)         5.15%      4.24%       4.10%      6.46%     25.09%
                  (1,3,2)         4.50%     26.27%       6.68%      3.10%      1.48%


                        Table 1 : relative frequencies of the ordinal patterns in the winter data

                                               all data            < -3            [-3,-1)         [-1,1)               [1,3)              > 3
               (3,2,1)        25.76%    28.30%    20.85%    24.08%    26.04%    27.08%
               (1,2,3)        50.54%    20.00%    46.71%    52.33%    50.00%    29.17%
               (2,1,3)         6.06%     8.30%     8.20%     5.70%    7.91%    20.83%
               (3,1,2)         5.95%    15.00%     8.50%     6.24%    3.87%     0.00%
               (2,3,1)         5.78%    13.30%     5.62%     5.62%    8.50%    18.75%
               (1,3,2)         5.89%    15.00%    10.00%     6.03%    3.67%     4.17%

                     Table 2 : relative frequencies of the ordinal patterns in the all-year data

                   We  restrict  ourselves  here  to  the  interpretation  of  the  ordinal  pattern
               distributions of the winter data because they exhibit a better illustration of the
               effects we want to describe. Therefore, we focus on Table 1. First, we observe
               that there is a large difference between the relative frequencies of the two
               patterns  that  describe  a  monotone  behaviour  of  the  time  series,  more
               precisely, that the relative frequency of the pattern (1,2,3) is nearly twice the
               value of (3,2,1), while the values for the four remaining patterns are close to
               being  equal.  A  heuristic  explanation  considering  that  we  are  dealing  with
               discharge  data  might  be  that,  especially  in  the  winter  months,  if  we  have
               melting snow we might have a fast increase but a slow decrease. If we now
               look  at  the  distributions  of  the  patterns  in  the  different  intervals,  we  first
               observe that in the middle regions namely  [−1.8,0) and [0,1.8) we get a very
               similar distribution as in the entire data set. This is easy to explain because
               within these areas we find most of the data points as one can easily see in
               Figure 2.
                   However, in the extremes, meaning the values smaller than -1.8 and larger
               than 1.8 we obtain a different distribution. The first point to notice is that the
               frequencies of the patterns (3,2,1) and (1,2,3) are getting closer to each other,
               in particular in the case where the data values are larger than 1.8. In the last
               four  rows  we  get  the  interesting  phenomenon  that  the  almost  equal
               frequencies from before now change to two almost equally large values and
               two almost equally small values. In the case where the values are smaller than

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