Resources Science ›› 2020, Vol. 42 ›› Issue (2): 346-357.doi: 10.18402/resci.2020.02.13
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WANG Guan1,2, CHEN Hanru3, WANG Ping1(), WANG Tianye1,2, YU Jingjie1,2, LIU Changming1, YANG Linsheng4
Received:
2019-10-10
Revised:
2019-12-15
Online:
2020-02-25
Published:
2020-04-25
Contact:
WANG Ping
E-mail:wangping@igsnrr.ac.cn
WANG Guan, CHEN Hanru, WANG Ping, WANG Tianye, YU Jingjie, LIU Changming, YANG Linsheng. Surface runoff changes and their causes in the Russian pan-Arctic Region[J].Resources Science, 2020, 42(2): 346-357.
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Table 1
Basic characteristics of the six main rivers in the Russian Arctic area[11]"
河流 | 站点名称 | 经度 | 纬度 | 年均径流量/(m3/s) | 流域面积/(103 km2) | 径流数据时间序列 |
---|---|---|---|---|---|---|
北德维纳河 | UST'-PINEGA | 41.92°E | 64.13°N | 3170 | 348 | 1930—2018年 |
伯朝拉河 | UST'-TSIL'MA | 52.28°E | 65.42°N | 3490 | 248 | 1932—2018年 |
鄂毕河 | SALEKHARD | 66.60°E | 66.63°N | 12700 | 2953 | 1930—2018年 |
叶尼塞河 | IGARKA | 86.48°E | 67.43°N | 18700 | 2440 | 1936—2018年 |
勒拿河 | KYUSYUR | 127.39°E | 70.68°N | 17200 | 2430 | 1935—2018年 |
科雷马河 | KOLYMSKOYE | 158.72°E | 68.73°N | 3300 | 526 | 1978—2018年 |
Table 2
Seasonal and annual average runoff trends of the six main rivers in the Russian Arctic area and coefficients of variation"
春 | 夏 | 秋 | 冬 | 年 | Cv | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
k (m3/s/a) | p | k (m3/s/a) | p | k (m3/s/a) | p | k (m3/s/a) | p | k (m3/s/a) | p | ||||||
北德维纳河 | 11.40 | 0.03* | -4.95 | 0.34 | 1.04 | 0.79 | 1.74 | 0.23 | 1.53 | 0.52 | 0.17 | ||||
伯朝拉河 | 16.80 | 0.03* | 1.23 | 0.90 | 5.28 | 0.16 | 3.40 | 0.00** | 7.27 | 0.01** | 0.15 | ||||
鄂毕河 | 38.51 | 0.00** | -1.84 | 0.93 | 8.63 | 0.45 | 18.32 | 0.00** | 15.37 | 0.06* | 0.15 | ||||
叶尼塞河 | 68.42 | 0.01** | -71.72 | 0.02* | 15.55 | 0.19 | 70.77 | 0.00** | 19.59 | 0.01** | 0.09 | ||||
勒拿河 | 76.47 | 0.00** | 11.13 | 0.68 | 38.70 | 0.02* | 27.14 | 0.00** | 38.41 | 0.06* | 0.13 | ||||
科雷马河 | 21.15 | 0.03* | -13.73 | 0.72 | 27.59 | 0.03* | 5.43 | 0.00** | 9.92 | 0.35 | 0.24 |
Table 3
Annual distribution of runoff of the six main rivers in the Russian Arctic area and coefficients of variation during 1930-1959, 1960-1989, and 1990-2018"
1930—1959年 | 1960—1989年 | 1990—2018年 | ||
---|---|---|---|---|
北德维纳河 | 春/% | 43.56 | 44.15 | 48.23 |
夏/% | 30.00 | 29.31 | 26.52 | |
秋/% | 18.53 | 17.78 | 16.74 | |
冬/% | 7.91 | 8.76 | 8.51 | |
伯朝拉河 | 春/% | 25.67 | 23.15 | 31.64 |
夏/% | 49.86 | 52.77 | 43.69 | |
秋/% | 19.30 | 18.34 | 18.66 | |
冬/% | 5.17 | 5.74 | 6.02 | |
鄂毕河 | 春/% | 14.02 | 14.37 | 17.94 |
夏/% | 56.60 | 56.40 | 51.81 | |
秋/% | 20.78 | 19.67 | 20.08 | |
冬/% | 8.60 | 9.56 | 10.17 | |
叶尼塞河 | 春/% | 18.30 | 20.24 | 23.25 |
夏/% | 56.60 | 52.07 | 47.11 | |
秋/% | 18.62 | 18.06 | 18.40 | |
冬/% | 6.48 | 9.63 | 11.24 | |
勒拿河 | 春/% | 3.74 | 5.03 | 8.89 |
夏/% | 70.44 | 70.64 | 63.63 | |
秋/% | 22.23 | 20.31 | 22.22 | |
冬/% | 3.60 | 4.02 | 5.26 | |
科雷马河 | 春/% | — | 3.99 | 8.40 |
夏/% | — | 76.53 | 67.01 | |
秋/% | — | 17.68 | 21.79 | |
冬/% | — | 1.80 | 2.80 |
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