Research Article

Statistical Uncertainty in Hydrometeorological Trend Analyses

Table 2

Summary of monotonic trend directions.

S numberCRD1CRD2SMR1SMR2SMR3MK1MK2MK3MK4MK5MK6MK7MK8

1□Y+□N+□Y+□N+□Y+□Y+□Y+□N+□Y+□Y+□Y+□Y+□Y+
2□N+□N+□Y+□Y+□Y+□N+□Y+□N+□N+□Y+□Y+□Y+□Y+
3□N+□Y+□N+□N+□Y+□N+□N+□N+□N+□N+□Y+▲Y+□Y+
4▲N+□Y+▲N+▲N+□Y+▲N+▲Y+▲Y+▲Y+▲Y+▲Y+▲Y+▲N+
5□N+□Y+□Y+□Y+□Y+□Y+□N+□N+□N+□Y+□N+□Y+□Y+
6□N–□N–□N−□Y−□Y−□N−□N−□Y−□N−□N−□Y−□N−□N−
7□N−□N−□Y−□Y−□Y−□Y−□Y−□N−□Y−□Y−□Y−□Y−□Y−
8□N+▲Y+▲Y+▲Y+▲N+□Y+□Y+□Y+□Y+□N+▲Y+▲Y+▲N+
9▼Y−□N−▼Y−▼N−□Y−▼N−□N−□Y−□N−□N−▼Y−▼Y−□N−
10□N−□Y−□Y−▼Y−□Y−▼Y−▼Y−□N−▼N−□N−□N−□N−□Y−
11□N+□N+□Y+□Y+□Y+□Y+□N+□N+□N+□Y+□Y+□Y+□Y−
12□Y−□Y−□Y−□Y−□N−□Y−□Y−□Y−□Y−□Y−□Y−□Y−□Y+
13□N+□N+□N+□N+□Y+□Y+□Y+□N+□Y+□N+□Y+□N+□Y+
14□Y−□N−□N−□N−□Y−□Y−□Y−□N−□Y−□N−□Y−□N−□Y−
15□N+□N+□N+□N+□Y+□N+□Y+□N+□Y+□N+□Y+□N+□Y−
16□N−□N−□Y−□Y−□Y−□N−□Y−□N−□Y−□Y−□Y−□Y−□Y−
17□N−▼N−▼Y−▼N−□Y−▼Y−□Y−□Y−□Y−□N−▼Y−▼Y−□N−
18□N+□N+□Y+□Y+□Y+□Y+□Y+□N+□Y+□Y+□Y+□Y+□Y+
19□Y+□N+□N+□N+□Y+□Y+□Y+□N+□Y+□N+□Y+□N+□N+
20□N+□N+□N+□N+□Y+□Y+□Y+□N+□N+□N+□N+□N+□N+
21□Y+□Y+□N+□N+□Y+□N+□Y+□N+□Y+□N+□N+□N+□N+
22□Y−□Y−□Y−□N−□Y−□Y−□N−□Y−□Y−□Y−□Y−□Y−□Y−
23□N+□N+□Y+□N+□Y+□N+□N+□Y+□N+□Y+□N+□Y+□Y+

Read the descriptive text under Section 4.1 for the interpretation of the results from this table. The results were based on values for CRD1 [12], CRD2 [see Appendix B], SMR1 [18], SMR2 [22], SMR3 [18], MK1 [30], MK2 [29], MK3 [15], MK4 [27], MK5 [45], MK6 [25], MK7 [24], and MK8 [46].