Drivers of wind and water erosion for river sediments in a typical coarse sandy area in the middle reaches of the Yellow River

Warmer temperatures and the combined effects of wind and water erosion leads to serious soil loss. Identifying the contribution of different drivers to wind and water compound erosion can improve soil erosion management in the watershed. Accordingly, we calculated the erosion energy based on energy theory and applied the mutation test and trend analysis to explore environmental drivers, runoff, and sediment changes for the Kuyehe River Basin. Rainfall erosion energy, wind erosion energy, air temperature, NDVI, and land cover were selected as potential drivers to quantify the contribution of sediment change using a partial least squares regression model. The results indicated that rainfall erosion energy decreased, wind erosion energy increased and then decreased, temperature increased, and NDVI increased during the period 1990–2020. The relationship between runoff and sediment transport in the basin shifted from more water and more sediment to more water and less sediment, and the timing of the mutation was different for runoff and sediment, with the runoff mutation occurring in 1997 and the sediment mutation occurring during 2003–2004. After sediment mutations, wind, NDVI, and land cover of forests showed higher importance for sediment transport changes, while precipitation and temperature were less important. In addition, the importance of cropland, shrub and grassland, and other land cover types varied considerably between sub-basins. Over 70 % of the contribution to sediment change was due to land cover change, while the cumulative contribution of forest and NDVI was about 30 %. The study identified the key drivers of sediment transport changes in the basin and provided valuable insights for future studies of wind and water compound erosion at the basin scale.