Considering the importance of data accuracy in climate studies, the standard normal homogeneity test (SNHT) and the Mann-Kendall (MK) trend test were applied to the data sets using XLSTAT software (Table 2). The SNHT test was developed by Alexanderson (1986) to detect a change in a series of rainfall data. The purpose of the MK test (Mann 1945; Kendall 1975; Gilbert 1987) is to statistically assess if there is a monotonic upward or downward trend of the variable of interest over time.
Results of homogeneity and trend test of selected stations
. | SNHT . | MK trend test . | . | |||
---|---|---|---|---|---|---|
Station . | p-value . | Risk of rejecting H0 (%) . | p-value . | Kendal's tau . | Risk of rejecting H0 (%) . | a . |
Abomoosa Island | 0.444 | 44.39 | 0.448 | −0.03 | 44.76 | 0.05 |
Bandar Abbas | 0.214 | 21.40 | 0.085 | −0.067 | 8.46 | 0.05 |
Jask | 0.201 | 20.09 | 0.310 | −0.041 | 30.95 | 0.05 |
Bandar Lengeh | 0.168 | 16.81 | 0.446 | −0.03 | 44.57 | 0.05 |
Kish Island | 0.159 | 15.9 | 0.206 | −0.05 | 20.63 | 0.05 |
Minab | 0.640 | 64.03 | 0.510 | −0.026 | 50.95 | 0.05 |
. | SNHT . | MK trend test . | . | |||
---|---|---|---|---|---|---|
Station . | p-value . | Risk of rejecting H0 (%) . | p-value . | Kendal's tau . | Risk of rejecting H0 (%) . | a . |
Abomoosa Island | 0.444 | 44.39 | 0.448 | −0.03 | 44.76 | 0.05 |
Bandar Abbas | 0.214 | 21.40 | 0.085 | −0.067 | 8.46 | 0.05 |
Jask | 0.201 | 20.09 | 0.310 | −0.041 | 30.95 | 0.05 |
Bandar Lengeh | 0.168 | 16.81 | 0.446 | −0.03 | 44.57 | 0.05 |
Kish Island | 0.159 | 15.9 | 0.206 | −0.05 | 20.63 | 0.05 |
Minab | 0.640 | 64.03 | 0.510 | −0.026 | 50.95 | 0.05 |