Journal of Geographical Sciences ›› 2020, Vol. 30 ›› Issue (9): 1401-1418.doi: 10.1007/s11442-020-1789-5
• Research Articles • Previous Articles Next Articles
HOU Bingfei1,2(), JIANG Chao1,2, SUN Osbert Jianxin1,2,*(
)
Received:
2020-03-22
Accepted:
2020-06-08
Online:
2020-09-25
Published:
2020-11-25
Contact:
SUN Osbert Jianxin
E-mail:excailibur@163.com;sunjianx@bjfu.edu.cn
About author:
Hou Bingfei (1985–), PhD candidate, specialized in global change ecology. E-mail: Supported by:
HOU Bingfei, JIANG Chao, SUN Osbert Jianxin. Differential changes in precipitation and runoff discharge during 1958-2017 in the headwater region of Yellow River of China[J].Journal of Geographical Sciences, 2020, 30(9): 1401-1418.
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Figure 4
Abrupt changes in average annual runoff discharge for the period 1958-2017 with Mann-Kendall test at the Tangnaihai Hydrological Station of Qinghai province, China. The two parallel horizontal dash lines show confidence range of P = 0.05. UFk (solid line) and UBk (long dash line) are forward and backward time series of the dimensionless variable u in the Mann-Kendall abrupt change detection, respectively."
Figure 5
(a) Interannual variations in temperature during 1958-2017 (solid line) and evapotranspiration (dash line) in the Yellow River headwater region, (b) the Mann-Kendall abrupt change detection of temperature and (c) that of evapotranspiration, (b) and (c) show the 95% confidence range, and the UF (solid line) and UB (dash line) are forward and backward time series of the dimensionless variable u in the Mann-Kendall abrupt change detection, respectively."
Figure 6
(a) Interannual variations in precipitation during 1958-2017 (solid line) and the 5-year moving average of available data (dash line) in the Yellow River headwater region and (b) the Mann-Kendall abrupt change detection of precipitation. The two parallel horizontal lines in (b) show the 95% confidence range, and the UF (solid line) and UB (dash line) are forward and backward time series of the dimensionless variable u in the Mann-Kendall abrupt change detection, respectively."
Figure 7
Projections of (a) monthly SPI12 time series in the Yellow River headwater region from 1958 to 2017, (b) the Mann-Kendall abrupt change detection of SPI12, and (c) the decadal departure of SPI12 from long-term average. The two parallel horizontal lines in (b) show the 95% confidence range, and the UF (solid line) and UB (dash line) are forward and backward time series of the dimensionless variable u in the Mann-Kendall abrupt change detection, respectively."
Figure 8
Cyclic patterns of runoff discharge derived from Singular Spectrum Analysis at the Tangnaihai Hydrological Station of Qinghai province, China. (a) Reconstruction component 1 in runoff discharge derived from Singular Spectrum Analysis, showing the long-term for periods 1958-1988 (a1) and 1989-2017 (a2); (b) Reconstruction component 2 in runoff discharge derived from Singular Spectrum Analysis, showing a cyclic pattern of eight-year intervals for period 1958-1988 (b1) and a cyclic pattern of six-year intervals for period 1989-2017 (b2); (c) Reconstruction component 3 in runoff discharge derived from Singular Spectrum Analysis, showing a cyclic pattern of four-year intervals for period 1958-1988 (c1) and a cyclic pattern of three- to four-year interval for period 1989-2017 (c2)."
Figure 9
(a) Reconstruction component 1 in SPI12 derived from Singular Spectrum Analysis, for periods 1958-1988 (a1) and 1989-2017 (a2); (b) Reconstruction component 2 in SPI12 derived from Singular Spectrum Analysis, for periods 1958-1988 (b1) and 1989-2017 (b2) and (c) Reconstruction component 3 in SPI12 derived from Singular Spectrum Analysis for the period 1989-2017"
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