Table 4.

The annual and seasonal mean precipitation and the corresponding climate tendencies in the northern Altai Mountains during 1966–2015.

	Station Name	Annual	Spring	Summer	Autumn	Winter
Mean Precipitation (mm)	Rubcovsk	336.70	56.15	127.79	91.26	61.49
	Zmeinogorsk	689.17	137.06	201.96	178.28	171.87
	Soloneshnoe	572.02	88.09	242.85	170.09	70.99
	Kyzyl-Ozek	733.56	111.38	282.94	238.22	101.03
	Yailu	879.96	117.44	374.85	299.44	88.22
	Mugur-Aksy	139.32	9.23	72.22	42.61	15.25
	Ust-Coksa	470.19	51.37	208.05	155.10	55.68
	Kara-Tyurek	574.46	81.63	235.77	191.71	65.36
	Kosh-Agach	118.35	7.36	61.81	37.23	11.96
Climate Tendency (mm/10 yr)	Rubcovsk	−5.20*	−4.15	2.24	−1.23	2.05
	Zmeinogorsk	−6.53*	−3.72	4.67	−7.22*	0.25
	Soloneshnoe	12.37**	2.81	11.88**	3.29	0.77
	Kyzyl-Ozek	−10.08**	−1.29	2.78	−11.66**	−2.49
	Yailu	3.77	3.72	6.13*	−6.47*	0.39
	Mugur-Aksy	−12.32**	0.22	−6.85*	−4.23	−1.02
	Ust-Coksa	2.19	1.15	−0.51	−0.12	1.68
	Kara-Tyurek	−2.75	−0.06	0.11	−1.11	−1.70
	Kosh-Agach	0.53	−0.34	1.57	−0.28	−0.43
	Average	−1.41	0.04	2.45	−3.47	−0.60

Note: * and ** indicate that the climate tendency is significant at the level of 0.05 and 0.01, respectively, by the Mann-Kendall test for the long-term trend.