Spatiotemporal Variability in the Hydrometeorological Time-Series over Upper Indus River Basin of Pakistan

Table 4

Relative change (%) in annual and seasonal streamflow during the 2^nd period (1989–2014) with respect to the 1^st period (1963–1988) (bold, underline, and showed significant trend with Student’s t-test, F-test, and Mann–Whitney U test, respectively, at 95% confidence level).

Stream gauge	Annual	Winter	Spring	Summer	Autumn
Naran	−4	−6	−3	−10	24
Garhi Habibullah	5	17	19	−5	21
Muzaffarabad	−6	13	3	−16	6
Chinari	−3	6	0	−7	−5
Domel	−2	13	2	−8	0
Kohala	1	21	6	−8	8
Azad Pattan	8	37	12	0	13
Kotli	3	36	6	−10	10
Palote	−12	27	−27	−14	−17
Kharmong	1	7	7	−7	1
Yogo	8	4	19	6	19
Shigar	13	2	5	12	3
Kachura	21	18	24	19	26
Gilgit	20	14	43	16	26
Dainyor Br.	−19	8	5	−25	−6
Alam Br.	−6	12	21	−13	3
Bunji	10	12	35	5	15
Doyain	26	34	28	18	39
Shatial Br.	9	11	19	7	7
Karora	−14	19	−20	−28	14
Besham Qila	4	18	14	−1	13
Daggar	9	39	21	−6	2
Phulra	10	38	13	0	5
Kalam	1	9	20	−5	1
Chakdara	22	69	36	8	37
Chitral	8	5	15	6	12
Jhansi post	−23	−21	−35	−1	−30
Nowshera	−3	8	5	−9	1
Gurriala	−8	24	5	−18	−11
Khairabad	−12	−17	−18	−15	−19
Thal	−18	−24	−31	−1	−17
Chirah	−29	−11	−29	−35	−16
Chahan	−21	0	−18	−30	6
Dhok Pathan	−13	18	−3	−25	15
Massan	8	28	7	2	18