Shoreline Change of the Northern Yellow River (Huanghe) Delta after the Latest Deltaic Course Shift in 1976 and Its Influence Factors
Xiaodong Zhang, Yexin Zhang, Ji Yang, Yawei Zhang, Zuosheng Yang
Abstract
Open-access reader
Xiaodong Zhang, Yexin Zhang, Ji Yang, Yawei Zhang, Zuosheng Yang
Abstract
Open-access reader
Zhang, X. D.; Zhang, Y. X.; Ji, Y.; Zhang, Y. W., and Yang, Z. S., 2016. Shoreline change of the northern Yellow River (Huanghe) Delta after the latest deltaic course shift in 1976 and its influence factors. 222 high-quality Landsat satellite images were used in this study to extract the instantaneous shoreline positions on 22 sections of the northern Yellow River delta. Based on the instantaneous water line position data, a new statistical method for studying annual shoreline change was proposed. The annual shoreline movement of the northern Yellow River delta after the latest deltaic course shift in 1976 was obtained. The results showed that the shoreline on northern Yellow River delta was mostly undergoing a retreat back process since 1976 due to the river course shift, relative sea level change, regional marine hydrodynamic forces and the local engineering constructions. The influence of the Yellow River deltaic course shift in 1976 on the shoreline change mainly occurred in the first 20 years in 1976–1996 after the course shift, and was mostly limited within 10 km range around the abandoned Diaokou river mouth. The coastal engineering constructions caused decrease of the erosion area by 61 km2, or 31% of the total erosion area. Most of the northern Yellow River delta was relatively insensitive to the relative sea level change except for the coast around sections S10 and S11; The annual shoreline movement due to the relative sea level change along most of the coast was only 1–3% of the actual annual shoreline movement; the total erosion area due to the relative sea level change was 9 km2, or 5% of the actual erosion area. The coast erosion in the northern Yellow River delta was mainly influenced by the regional marine hydrodynamic forces, which gradually increase from west to east, resulting in gradually eastward increase of annual shoreline movement and slope steepness of the coast.
OpenAlex reports 18 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Zhang, X. D.; Zhang, Y. X.; Ji, Y.; Zhang, Y. W., and Yang, Z. S., 2016. Shoreline change of the northern Yellow River (Huanghe) Delta after the latest deltaic course shift in 1976 and its influence factors. 222 high-quality Landsat satellite images were used in this study to extract the instantaneous shoreline positions on 22 sections of the northern Yellow River delta. Based on the instantaneous water line position data, a new statistical method for studying annual shoreline change was proposed. The annual shoreline movement of the northern Yellow River delta after the latest deltaic course shift in 1976 was obtained. The results showed that the shoreline on northern Yellow River delta was mostly undergoing a retreat back process since 1976 due to the river course shift, relative sea level change, regional marine hydrodynamic forces and the local engineering constructions. The influence of the Yellow River deltaic course shift in 1976 on the shoreline change mainly occurred in the first 20 years in 1976–1996 after the course shift, and was mostly limited within 10 km range around the abandoned Diaokou river mouth. The coastal engineering constructions caused decrease of the erosion area by 61 km2, or 31% of the total erosion area. Most of the northern Yellow River delta was relatively insensitive to the relative sea level change except for the coast around sections S10 and S11; The annual shoreline movement due to the relative sea level change along most of the coast was only 1–3% of the actual annual shoreline movement; the total erosion area due to the relative sea level change was 9 km2, or 5% of the actual erosion area. The coast erosion in the northern Yellow River delta was mainly influenced by the regional marine hydrodynamic forces, which gradually increase from west to east, resulting in gradually eastward increase of annual shoreline movement and slope steepness of the coast.
Key concepts: Shore, Delta, River delta, Geology, Erosion, Sea level, Oceanography, Coastal erosion