Statistical Uncertainty in Hydrometeorological Trend Analyses
Table 2
Summary of monotonic trend directions.
S number
CRD1
CRD2
SMR1
SMR2
SMR3
MK1
MK2
MK3
MK4
MK5
MK6
MK7
MK8
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].