Research Article

Long-Term Homogeneity and Trends of Hydroclimatic Variables in Upper Awash River Basin, Ethiopia

Table 8

Summary of Z statistics and Sen’s slope (Q) (mm/year) of the MK test for annual and seasonal rainfall of UASB.

StationAnnualKiremt (JJAS)Bega (ONDJ)Belg (FMAM)
Mk (zs)Sen’s (Q)Mk (zs)Sen’s (Q)Mk (zs)Sen’s (Q)Mk (zs)Sen’s (Q)

AA Bole−0.271−0.820.501.482.3792.31−1.325−3.16
AA T. Ambessa−0.470−2.321.1893.20.6790.58−2.124−5.16
Addis Alem−2.196−19.81−1.893−9.45−1.666−4.38−1.060−6.7
Akaki1.855−5.60−0.249−0.710.2850.24−1.213−2.479
Debre Zeit0.4800.820.9611.661.1000.586−0.867−1.459
Ghinch−2.747−12.38−1.248−5.25−0.178−0.275−2.515−6.033
Hombole−1.793−9.49−1.126−4.210.6380.703−1.512−3.82
Sebeta−1.200−4.06−1.784−19.01−0.875−1.659−0.779−4.819
Sendafa−0.526−1.160.0010.0020.9020.614−1.818−3.15
Teji−0.560−1.480.9512.12−0.527−0.18−1.835−3.81
Tulu Bolo−1.239−5.97−0.476−2.710.0540.007−0.585−1.057

Trend at α′ = 0.01 level. Trend at α′ = 0.05 level. Trend at α′ = 0.1 level.