Acta Geographica Sinica, Volume. 75, Issue 7, 1494(2020)
Fig. 3. Temporal changes of water and sediment conditions at Huayuankou station
Fig. 4. Annual average values of main-channel cross-sectional parameters in different reaches
Fig. 5. Temporal changes of relative main-channel cross-sectional parameters in different reaches
Fig. 6. Relationships between main-channel area and 4 a moving average water and sediment conditions in different reaches
Fig. 7. Relationships between main-channel width and 4 a moving average water and sediment conditions in different reaches
Fig. 8. Relationships between main-channel depth and 4 a moving average water and sediment conditions in different reaches
Fig. 9. Relationships between main-channel cross-sectional geomorphic coefficient and 4 a moving average water and sediment conditions in different reaches
Fig. 10. Comparison between computed and measured main-channel area in different reaches
Fig. 11. Comparison between computed and measured main-channel width in different reaches
Fig. 12. Comparison between computed and measured main-channel depth in different reaches
Fig. 13. Comparison between computed and measured main-channel cross-sectional geomorphic coefficient in different reaches
Fig. 14. Downstream changes of exponents
Fig. 15. Downstream changes of weights of previous water and sediment conditions to main-channel cross-sectional parameters
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Yanjun WANG, Baosheng WU, Deyu ZHONG.
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Received: May. 27, 2019
Accepted: --
Published Online: Jan. 27, 2021
The Author Email: WANG Yanjun (yanjun1113@126.com)